There are over 300,000 contaminated groundwater sites in the U.S.

Preface.  If peak oil did indeed happen in 2018 as the EIA world production data shows, then let’s use the oil we still have, before it is rationed, to clean up the 126,000+ sites that threaten to pollute groundwater for thousands of years as this report from the National Research Council explains.  And while we’re at it, nuclear waste, which will pollute for hundreds of thousands of years. 

Pollution in the news:

Westenhaus B (2022) The environmental consequence of burning rubber. oilprice.com. Have you ever wondered what happens to the rubber tread that wears off a vehicle’s tires? On a planet with hundreds of millions of vehicles there has to be quite a lot somewhere. New modeling at the University of British Columbia Okanagan (UBCO) campus suggests an increasing amount of what are microplastics, the fragments from tires and roadways, are ending up in lakes and streams.The researchers found that more than 50 metric tons of tire and road wear particles are released into waterways annually in an area like the Okanagan valley of British Columbia. With1.5 billion tires  produced every year globally, thatl’s six million tonnes of tire and road wear particles plus chemical additives, contaminating fresh water.

Alice Friedemann  www.energyskeptic.com  Author of Life After Fossil Fuels: A Reality Check on Alternative Energy; When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Women in ecology  Podcasts: WGBH, Jore, Planet: Critical, Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, Kunstler 253 &278, Peak Prosperity,  Index of best energyskeptic posts

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NRC. 2013. Alternatives for Managing the Nation’s Complex Contaminated Groundwater Sites. National Research Council, National Academies Press.

contaminated water sites and costTABLE 2-6 Rough Estimate of the total number of currently known facilities or contaminated sites and estimated costs to complete

CONCLUSIONS AND RECOMMENDATIONS At least 126,000 sites across the country have been documented that have residual contamination at levels preventing them from reaching closure.

This number is likely to be an underestimate of the extent of contamination in the United States for a number of reasons. For some programs data are available only for contaminated facilities rather than individual sites, and the total does not include sites that likely exist but have not yet been identified, such as dry cleaners or small chemical-intensive businesses (e.g., electroplating, furniture refinishing). Information on cleanup costs incurred to date and estimates of future costs, as shown in Table 2-6, are highly uncertain. Despite this uncertainty, the estimated “cost to complete” of $110-$ 127 billion is likely an underestimate of future liabilities. Remaining sites include some of the most difficult to remediate sites, for which the effectiveness of planned remediation remains uncertain given their complex site conditions. Furthermore, many of the estimated costs do not fully consider the cost of long-term management of sites that will have contamination remaining in place at high levels for the foreseeable future.

Despite nearly 40 years of intensive efforts in the United States as well as in other industrialized countries worldwide, restoration of groundwater contaminated by releases of anthropogenic chemicals to a condition allowing for unlimited use and unrestricted exposure remains a significant technical and institutional challenge.

Recent estimates by the U.S. Environmental Protection Agency (EPA) indicate that expenditures for soil and groundwater cleanup at over 300,000 sites through 2033 may exceed $200 billion (not adjusted for inflation), and many of these sites have experienced groundwater impacts.

One dominant attribute of the nation’s efforts on subsurface remediation efforts has been lengthy delays between discovery of the problem and its resolution. Reasons for these extended timeframes are now well known: ineffective subsurface investigations, difficulties in characterizing the nature and extent of the problem in highly heterogeneous subsurface environments, remedial technologies that have not been capable of achieving restoration in many of these geologic settings, continued improvements in analytical detection limits leading to discovery of additional chemicals of concern, evolution of more stringent drinking water standards, and the realization that other exposure pathways, such as vapor intrusion, pose unacceptable health risks. A variety of administrative and policy factors also result in extensive delays, including, but not limited to, high regulatory personnel turnover, the difficulty in determining cost-effective remedies to meet cleanup goals, and allocation of responsibility at multiparty sites.

There is general agreement among practicing remediation professionals, however, that there is a substantial population of sites, where, due to inherent geologic complexities, restoration within the next 50 to 100 years is likely not achievable. Reaching agreement on which sites should be included in this category, and what should be done with such sites, however, has proven to be difficult.  A key decision in that Road Map is determining whether or not restoration of groundwater is “likely.

Summary

The nomenclature for the phases of site cleanup and cleanup progress are inconsistent between federal agencies, between the states and federal government, and in the private sector. Partly because of these inconsistencies, members of the public and other stakeholders can and have confused the concept of “site closure” with achieving unlimited use and unrestricted exposure goals for the site, such that no further monitoring or oversight is needed. In fact, many sites thought of as “closed” and considered as “successes” will require oversight and funding for decades and in some cases hundreds of years in order to be protective.

At hundreds of thousands of hazardous waste sites across the country, groundwater contamination remains in place at levels above cleanup goals. The most problematic sites are those with potentially persistent contaminants including chlorinated solvents recalcitrant to biodegradation, and with hydrogeologic conditions characterized by large spatial heterogeneity or the presence of fractures. While there have been success stories over the past 30 years, the majority of hazardous waste sites that have been closed were relatively simple compared to the remaining caseload.

At least 126,000 sites across the country have been documented that have residual contamination at levels preventing them from reaching closure. This number is likely to be an underestimate of the extent of contamination in the United States

Significant limitations with currently available remedial technologies persist that make achievement of Maximum Contaminant Levels (MCL) throughout the aquifer unlikely at most complex groundwater sites in a time frame of 50-100 years. Furthermore, future improvements in these technologies are likely to be incremental, such that long-term monitoring and stewardship at sites with groundwater contamination should be expected.

IMPLICATIONS OF CONTAMINATION REMAINING IN PLACE

Chapter 5 discusses the potential technical, legal, economic, and other practical implications of the finding that groundwater at complex sites is unlikely to attain unlimited use and unrestricted exposure levels for many decades.  First, the failure of hydraulic or physical containment systems, as well as the failure of institutional controls, could create new exposures. Second, toxicity information is regularly updated, which can alter drinking water standards, and contaminants that were previously unregulated may become so. In addition, pathways of exposure that were not previously considered can be found to be important, such as the vapor intrusion pathway. Third, treating contaminated groundwater for drinking water purposes is costly and, for some contaminants, technically challenging. Finally, leaving contamination in the subsurface may expose the landowner, property manager, or original disposer to complications that would not exist in the absence of the contamination, such as natural resource damages, trespass, and changes in land values. Thus, the risks and the technical, economic, and legal complications associated with residual contamination need to be compared to the time, cost, and feasibility involved in removing contamination outright.

New toxicological understanding and revisions to dose-response relationships will continue to be developed for existing chemicals, such as trichloroethene and tetrachloroethene, and for new chemicals of concern, such as perchlorate and perfluorinated chemicals. The implications of such evolving understanding include identification of new or revised ARARs (either more or less restrictive than existing ones), potentially leading to a determination that the existing remedy at some hazardous waste sites is no longer protective of human health and the environment.

Introduction

Since the 1970s, hundreds of billions of dollars have been invested by federal, state, and local government agencies as well as responsible parties to mitigate the human health and ecological risks posed by chemicals released to the subsurface environment. Many of the contaminants common to these hazardous waste sites, such as metals and volatile organic compounds, are known or suspected to cause cancer or adverse neurological, reproductive, or developmental conditions.

Over the past 30 years, some progress in meeting mitigation and remediation goals at hazardous waste sites has been achieved. For example, of the 1,723 sites ever listed on the National Priorities List (NPL), which are considered by the U.S. Environmental Protection Agency (EPA) to present the most significant risks, 360 have been permanently removed from the list because EPA deemed that no further response was needed to protect human health or the environment (EPA, 2012).

Seventy percent of the 3,747 hazardous waste sites regulated under the Resource Conservation and Recovery Act (RCRA) corrective action program have achieved “control of human exposure to contamination,” and 686 have been designated as “corrective action completed”. The Underground Storage Tank (UST) program also reports successes, including closure of over 1.7 million USTs since the program was initiated in 1984. The cumulative cost associated with these national efforts underscores the importance of pollution prevention and serves as a powerful incentive to reduce the discharge or release of 13 hazardous substances to the environment, particularly when a groundwater resource is threatened. Although some of the success stories described above were challenging in terms of contaminants present and underlying hydrogeology, the majority of sites that have been closed were relatively simple (e.g., shallow, localized petroleum contamination from USTs) compared to the remaining caseload.

Indeed, hundreds of thousands of sites across both state and federal programs are thought to still have contamination remaining in place at levels above those allowing for unlimited land and groundwater use and unrestricted exposure (see Chapter 2).  According to its most recent assessment, EPA estimates that more than $209 billion dollars (in constant 2004 dollars) will be needed over the next 30 years to mitigate hazards at between 235,000 to 355,000 sites (EPA, 2004). This cost estimate, however, does not include continued expenditures at sites where remediation is already in progress, or where remediation has transitioned to long-term management.

It is widely agreed that long-term management will be needed at many sites for the foreseeable future, particularly for the more complex sites that have recalcitrant contaminants, large amounts of contamination, and/or subsurface conditions known to be difficult to remediate (e.g., low-permeability strata, fractured media, deep contamination).

According to the most recent annual report to Congress, the Department of Defense (DoD) currently has almost 26,000 active sites under its Installation Restoration Program where soil and groundwater remediation is either planned or under way. Of these, approximately 13,000 sites are the responsibility of the Army, the sponsor of this report. The estimated cost to complete cleanup at all DoD sites is approximately $12.8 billion. (Note that these estimates do not include sites containing unexploded ordnance.)

Complex Contaminated Sites

Although progress has been made in remediating many hazardous waste sites, there remains a sizeable population of complex sites, where restoration is likely not achievable in the next 50-100 years. Although there is no formal definition of complexity, most remediation professionals agree that attributes include a really extensive groundwater contamination, heterogeneous geology, large releases and/or source zones, multiple and/or recalcitrant contaminants, heterogeneous contaminant distribution in the subsurface, and long time frames since releases occurred.

Complexity is also directly tied to the contaminants present at hazardous waste sites, which can vary widely and include organics, metals, explosives, and radionuclides. Some of the most challenging to remediate are dense nonaqueous phase liquids (DNAPLs), including chlorinated solvents.

Each of the NRC studies has, in one form or another, recognized that in almost all cases, complete restoration of contaminated groundwater is difficult, and in a substantial fraction of contaminated sites, not likely to be achieved in less than 100 years.

Trichloroethene (TCE) and tetrachloroethene are particularly challenging to restore because of their complex contaminant distribution in the subsurface.

Three classes of contaminants that have proven very difficult to treat once released to the subsurface: metals, radionuclides, and DNAPLs, such as chlorinated solvents. The report concluded that “removing all sources of groundwater contamination, particularly DNAPLs, will be technically impracticable at many Department of Energy sites, and long-term containment systems will be necessary for these sites.”

An example of the array of challenges faced by the DoD is provided by the Anniston Army Depot, where groundwater is contaminated with chlorinated solvents (as much as 27 million pounds of TCE and inorganic compounds. TCE and other contaminants are thought to be migrating vertically and horizontally from the source areas, affecting groundwater downgradient of the base including the potable water supply to the City of Anniston, Alabama. The interim Record of Decision called for a groundwater extraction and treatment system, which has resulted in the removal of TCE in extracted water to levels below drinking water standards. Because the treatment system is not significantly reducing the extent or mobility of the groundwater contaminants in the subsurface, the current interim remedy is considered “not protective.” Therefore, additional efforts have been made to remove greater quantities of TCE from the subsurface, and no end is in sight. Modeling studies suggest that the time to reach the TCE MCL in the groundwater beneath the source areas ranges from 1,200 to 10,000 years, and that partial source removal will shorten those times to 830–7,900 years.

The Department of Defense

The DoD environmental remediation program, measured by the number of facilities, is the largest such program in the United States, and perhaps the world.

The Installation Restoration Program (IRP), which addresses toxic and radioactive wastes as well as building demolition and debris removal, is responsible for 3,486 installations containing over 29,000 contaminated sites

The Military Munitions Response Program, which focuses on unexploded ordnance and discarded military munitions, is beyond the scope of this report and is not discussed further here, although its future expenses are greater than those anticipated for the IRP.

The CERCLA program was established to address hazardous substances at abandoned or uncontrolled hazardous waste sites. Through the CERCLA program, the EPA has developed the National Priorities List (NPL).  There are 1,723 facilities that have been on the NPL.

As of June 2012, 359 of the 1,723 facilities have been “deleted” from the NPL, which means the EPA has determined that no further response is required to protect human health or the environment; 1,364 remain on the NPL.

Statistics from EPA (2004) illustrate the typical complexity of hazardous waste sites at facilities on the NPL. Volatile organic compounds (VOCs) are present at 78 percent of NPL facilities, metals at 77 percent, and semivolatile organic compounds (SVOCs) at 71 percent. All three contaminant groups are found at 52 percent of NPL facilities, and two of the groups at 76 percent of facilities

RCRA Corrective Action Program Among other objectives, the Resource Conservation and Recovery Act (RCRA) governs the management of hazardous wastes at operating facilities that handle or handled hazardous waste.

Although tens of thousands of waste handlers are potentially subject to RCRA, currently EPA has authority to impose corrective action on 3,747 RCRA hazardous waste facilities in the United States

Underground Storage Tank Program In 1984, Congress recognized the unique and widespread problem posed by leaking underground storage tanks by adding Subtitle I to RCRA.

UST contaminants are typically light nonaqueous phase liquids (LNAPLs) such as petroleum hydrocarbons and fuel additives.

Responsibility for the UST program has been delegated to the states (or even local oversight agencies such as a county or a water utility with basin management programs), which set specific cleanup standards and approve specific corrective action plans and the application of particular technologies at sites. This is true even for petroleum-only USTs on military bases, a few of which have hundreds of such tanks.

At the end of 2011, there were 590,104 active tanks in the UST program

Currently, there are 87,983 leaking tanks that have contaminated surrounding soil and groundwater, the so-called “backlog.” The backlog number represents the cumulative number of confirmed releases (501,723) minus the cumulative number of completed cleanups (413,740).

Department of Energy

The DOE faces the task of cleaning up the legacy of environmental contamination from activities to develop nuclear weapons during World War II and the Cold War. Contaminants include short-lived and long-lived radioactive wastes, toxic substances such as chlorinated solvents, “mixed wastes” that include both toxic substances and radionuclides, and, at a handful of facilities, unexploded ordnance. Much like the military, a given DOE facility or installation will tend to have multiple sites where contaminants may have been spilled, disposed of, or abandoned that can be variously regulated by CERCLA, RCRA, or the UST program. T

The DOE Environmental Management program, established in 1989 to address several decades of nuclear weapons production, “is the largest in the world, originally involving two million acres at 107 sites in 35 states and some of the most dangerous materials known to man”.

Given that major DOE sites tend to be more challenging than typical DoD sites, it is not surprising that the scope of future remediation is substantial. Furthermore, because many DOE sites date back 50 years, contaminants have diffused into the subsurface matrix, considerably complicating remediation.

More recent reports suggest that about 7,000 individual release sites out of 10,645 historical release sites have been “completed,” which means at least that a remedy is in place, leaving approximately 3,650 sites remaining. In 2004, DOE estimated that almost all installations would require long-term stewardship

As of April 1995, over 3,000 contaminated sites on 700 facilities, distributed among 17 non-DoD and non-DOE federal agencies, were potentially in need of remediation. The Department of Interior (DOI), Department of Agriculture (USDA), and National Aeronautics and Space Administration (NASA) together account for about 70 percent of the civilian federal facilities reported to EPA as potentially needing remediation (EPA, 2004). EPA estimates that many more sites have not yet been reported, including an estimated 8,000 to 31,000 abandoned mine sites, most of which are on federal lands, although the fraction of these that are impacting groundwater quality is not reported. The Government Accountability Office (GAO) (2008) determined that there were at least 33,000 abandoned hardrock mine sites in the 12 western states and Alaska that had degraded the environment by contaminating surface water and groundwater or leaving arsenic-contaminated tailings piles.

State Sites

A broad spectrum of sites is managed by states, local jurisdictions, and private parties, and thus are not part of the CERCLA, RCRA, or UST programs. These types of sites can vary in size and complexity, ranging from sites similar to those at facilities listed on the NPL to small sites with low levels of contamination.

States typically define Brownfields sites as industrial or commercial facilities that are abandoned or underutilized due to environmental contamination or fear of contamination. EPA (2004) postulated that only 10 to 15 percent of the estimated one-half to one million Brownfields sites have been identified.

As of 2000, 23,000 state sites had been identified as needing further attention that had not yet been targeted for remediation (EPA, 2004). The same study estimated that 127,000 additional sites would be identified by 2030. Dry Cleaner Sites Active and particularly former dry cleaner sites present a unique problem in hazardous waste management because of their ubiquitous nature in urban settings, the carcinogenic contaminants used in the dry cleaning process (primarily the chlorinated solvent PCE, although other solvents have been used), and the potential for the contamination to reach receptors via the drinking water and indoor air (vapor intrusion) exposure pathways. Depending on the size and extent of contamination, dry cleaner sites may be remediated under one or more state or federal programs such as RCRA, CERCLA, or state mandated or voluntary programs discussed previously, and thus the total estimates of dry cleaner sites are not listed separately in

In 2004, there were an estimated 30,000 commercial, 325 industrial, and 100 coin-operated active dry cleaners in the United States (EPA, 2004). Despite their smaller numbers, industrial dry cleaners produce the majority of the estimated gallons of hazardous waste from these facilities (EPA, 2004). As of 2010, the number of dry cleaners has grown, with an estimated 36,000 active dry cleaner facilities in the United States—of which about 75 percent (27,000 dry cleaners) have soil and groundwater contamination (SCRD, 2010b). In addition to active sites, dry cleaners that have moved or gone out of business—i.e., inactive sites—also have the potential for contamination. Unfortunately, significant uncertainty surrounds estimates of the number of inactive dry cleaner sites and the extent of contamination at these sites. Complicating factors include the fact that (1) older dry cleaners used solvents less efficiently than younger dry cleaners thus enhancing the amount of potential contamination and (2) dry cleaners that have moved or were in business for long amounts of time tend to employ different cleaning methods throughout their lifetime. EPA (2004) documented at least 9,000 inactive dry cleaner sites, although this number does not include data on dry cleaners that closed prior to 1960. There are no data on how many of these documented inactive dry cleaner sites may have been remediated over the years. EPA estimated that there could be as many as 90,000 inactive dry cleaner sites in the United States.

Department of Defense The Installation Restoration Program reports that it has spent approximately $31 billion through FY 2010, and estimates for “cost to complete” exceed $12 billion

Implementation costs for the CERCLA program are difficult to obtain because most remedies are implemented by private, nongovernmental PRPs and generally there is no requirement for these PRPs to report actual implementation costs.

EPA (2004) estimated that the cost for addressing the 456 facilities that have not begun remedial action is $16-$23 billion.

A more recent report from the GAO (2009) suggests that individual site remediation costs have increased over time (in constant dollars) because a higher percentage of the remaining NPL facilities are larger and more complex (i.e., “megasites”) than those addressed in the past. Additionally, GAO (2009) found that the percentage of NPL facilities without responsible parties to fund cleanups may be increasing. When no PRP can be identified, the cost for Superfund remediation is shared by the states and the Superfund Trust Fund. The Superfund Trust Fund has enjoyed a relatively stable budget—e.g., $1.25 billion, $1.27 billion, and $1.27 billion for FY 2009, 2010, and 2011, 8 respectively—although recent budget proposals seek to reduce these levels. States contribute as much as 50 percent of the construction and operation costs for certain CERCLA actions in their state. After ten years of remedial actions at such NPL facilities, states become fully responsible for continuing long-term remedial actions.

In 2004, EPA estimated that remediation of the remaining RCRA sites will cost between $31 billion and $58 billion, or an average of $11.4 million per facility

Underground Storage Tank Program

There is limited information available to determine costs already incurred in the UST program. EPA (2004) estimated that the cost to close all leaking UST (LUST) sites could reach $12-$19 billion or an average of $125,000 to remediate each release site (this includes site investigations, feasibility studies, and treatment/disposal of soil and groundwater). Based on this estimate of $125,000 per site, the Committee calculated that remediating the 87,983 backlogged releases would require $11 billion. The presence of the recalcitrant former fuel additive methyl tert-butyl ether (MTBE) and its daughter product and co-additive tert-butyl alcohol could increase the cost per site. Most UST cleanup costs are paid by property owners, state and local governments, and special trust funds based on dedicated taxes, such as fuel taxes. Department of Energy

The Department’s FY 2011 report to Congress, which shows that DOE’s anticipated cost to complete remediation of soil and groundwater contamination ranges from $17.3 to $20.9 billion. The program is dominated by a small number of mega-facilities, including Hanford (WA), Idaho National Labs, Savannah River (SC), Los Alamos National Labs (NM), and the Nevada Test Site. Given that the cost to complete soil and groundwater remediation at these five facilities alone ranges from $16.4 to $19.9 billion (DOE, 2011), the Committee believes that the DOE’s anticipated cost-to-complete figure is likely an underestimate of the Agency’s financial burden; the number does not include newly discovered releases or the cost of long-term management at all sites where waste remains in the subsurface. Data on long-term stewardship costs, including the expense of operating and maintaining engineering controls, enforcing institutional controls, and monitoring, are not consolidated but are likely to be substantial and ongoing.

Stewardship costs for just the five facilities managed by the National Nuclear Security Administration (Lawrence Livermore National Laboratory, CA, Livermore’s Site 300, Pantex, TX, Sandia National Laboratories, NM, and the Kansas City Plant, MO) total about $45 million per year (DOE, 2012c).

Other Federal Sites EPA (2004) reports that there is a $15-$22 billion estimated cost to address at least 3,000 contaminated areas on 700 civilian federal facilities, based on estimates from various reports from DOI, USDA, and NASA. States EPA (2004) estimated that states and private parties together have spent about $1 billion per year on remediation, addressing about 5,000 sites annually under mandatory and voluntary state programs. If remediation were continued at this rate, 150,000 sites would be completed over 30 years, at a cost of approximately $30 billion (or $20,000 per site). IMPACTS TO

DRINKING WATER SUPPLIES

The Committee sought information both on the number of hazardous waste sites that impact a drinking water aquifer—that is, pose a substantial near-term risk to public water supply systems that use groundwater as a source. Unfortunately, program-specific information on water supply impacts was generally not available. Therefore, the Committee also sought other evidence related to the effects of hazardous waste disposal on the nation’s drinking water aquifers.

Despite the existence of several NPL and DoD facilities that are known sources of contamination to public or domestic wells (e.g., the San Fernando and San Gabriel basins in Los Angeles County), there is little aggregated information about the number of CERCLA, RCRA, DoD, DOE, UST, or other sites that directly impact drinking water supply systems. None of the programs reviewed in this chapter specifically compiles information on the number of sites currently adversely affecting a drinking water aquifer. However, the Committee was able to obtain information relevant to the groundwater impacts from some programs, i.e. the DoD. The Army informed the Committee that public water supplies are threatened at 18 Army installations

Also, private drinking water wells are known to be affected at 23 installations. A preliminary assessment in 1997 showed that 29 Army installations may possibly overlie one or more sole source aquifers. Some of the best known are Camp Lejeune Marine Corps Base (NC), Otis Air National Guard Base (MA), and the Bethpage Naval Weapons Industrial Reserve Plant (NY).

CERCLA. Each individual remedial investigation/feasibility study (RI/FS) and Record of Decision (ROD) should state whether a drinking water aquifer is affected, although this information has not been compiled. Canter and Sabatini (1994) reviewed the RODs for 450 facilities on the NPL. Their investigation revealed that 49 of the RODs (11 percent) indicated that contamination of public water supply systems had occurred. “A significant number” of RODs also noted potential threats to public supply wells. Additionally, the authors note that undeveloped aquifers have also been contaminated, which prevents or limits the unrestricted use (i.e., without treatment) of these resources as a future water supply.

The EPA also compiles information about remedies implemented within Superfund. EPA (2007) reported that out of 1,072 facilities that have a groundwater remedy, 106 specifically have a water supply remedy, by which we inferred direct treatment of the water to allow potable use or switching to an alternative water supply. This suggests that 10 percent of NPL facilities adversely affect or significantly threaten drinking water supply systems.

RCRA. Of the 1,968 highest priority RCRA Corrective Action facilities, EPA (2008) reported that there is “unacceptable migration of contaminated groundwater” at 77 facilities. Also, 17,042 drinking water aquifers have a RCRA facility within five miles, but without additional information, it is impossible to know if these facilities are actually affecting the water sources.

UST. In 2000, 35 states reported USTs as the number one threat to groundwater quality (and thus indirectly to drinking water). However, more specific information on the number of leaking USTs currently impacting a drinking water aquifer is not available. Other Evidence That Hazardous Waste Sites Affect Water Supplies The U.S. Geological Survey (USGS) has compiled large data sets over the past 20 years regarding the prevalence of VOCs in waters derived from domestic (private) and public wells. VOCs include solvents, trihalomethanes (some of which are solvents [e.g., chloroform], but may also arise from chlorination of drinking water), refrigerants, organic synthesis compounds (e.g., vinyl chloride), gasoline hydrocarbons, fumigants, and gasoline oxygenates. Because many (but not all) of these compounds may arise from hazardous waste sites, the USGS studies provide further insight into the extent to which anthropogenic activities contaminate groundwater supplies

Zogorski et al. (2006) summarized the presence of VOCs in groundwater, private domestic wells, and public supply wells from sampling sites throughout the United States. Using a threshold level of 0.2 µg/L—much lower than current EPA drinking water standards for individual VOCs (see Table 3-1)—14 percent of domestic wells and 26 percent of public wells had one or more VOCs present. The detection frequencies of individual VOCs in domestic wells were two to ten times higher when a threshold of 0.02 µg/L was used (see Figures 2-2 and 2-3). In public supply wells, PCE was detected above the 0.2 µg/L threshold in 5.3 percent of the samples and TCE in 4.3 percent of the samples. The total percentage of public supply wells with either PCE or TCE (or both) above the 0.2 µg/L threshold is 7.3

Chloroform Methyl tert-butyl ether (MTBE) Perchloroethene (PCE) 1,1,1-Trichloroethane (TCA) Dichlorodifluoromethane (CFC-12) Toluene Chloromethane Trichloroethene (TCE) Dibromochloropropane (DBCP) Methylene chloride Trichlorofluoromethane (CFC-11) Bromodichloromethane 1,2-Dichloropropane Dibromochloromethane 1,2,3-Trichloropropane

FIGURE 2-2 Detection frequencies in domestic well samples for 15 most frequently detected VOCs at levels of 0.2 and 0.02 mg/L. SOURCE: Zogorski et al. (2006) with illustration provided by USGS National Water Quality Assessment program. Figure 2-2 Chloroform Methyl tert-butyl ether (MTBE) Perchloroethene (PCE) Bromoform Dibromochloromethane Trichloroethene (TCE) Bromodichloromethane 1,1,1-Trichloroethane (TCA) 1,1-Dichloroethane (1,1-DCA) Dichlorodifluoromethane (CFC-12) cis-1,2-Dichloroethene (cis-1,2-DCE) 1,1-Dichloroethene (1,1-DCE) Trichlorofluoromethane (CFC-11) trans-1,2-Dichloroethene (trans-1,2-DCE) Toluene

FIGURE 2-3 The 15 most frequently detected VOCs in public supply wells. SOURCE: Zogorski et al. (2006) with illustration provided by USGS National Wa ter Quality Assessment program.Figure

Further analysis of domestic wells by DeSimone et al. (2009) showed that organic contaminants were detected in 60 percent of 2,100 sampled wells. Wells were sampled in 48 states in parts of 30 regionally extensive aquifers used for water supply. Aquifers were randomly selected for sampling and there was no prior knowledge of contamination.

Of 30 regionally extensive aquifers used for water supply. Aquifers were randomly selected for sampling and there was no prior knowledge of contamination.

Toccalino and Hopple (2010) and Toccalino et al. (2010) focused on 932 public supply wells across the United States. The public wells sampled in this study represent less than 1 percent of all groundwater that feeds the nation’s public water systems. The samples, however, were widely distributed nationally and were randomly selected to represent typical aquifer conditions. Overall, 60 percent of public wells contained one or more VOCs at a concentration of = 0.02 µg/L, and 35 percent of public wells contained one or more VOCs at a concentration of = 0.2 µg/L.

 

Overall detection frequencies for individual compounds included 23 percent for PCE, 15 percent for TCE, 14 percent for MTBE, and 12 percent for 1,1,1-TCA (see Figure 2-5). PCE and TCE exceeded the MCL in approximately 1 percent of the public wells sampled.

 

PERCENT FIGURE 2-4 VOCs (in black) and pesticides (in white) detected in more than 1 percent of domestic wells at a level of 0.02 µg/L.

 

FIGURE 2-5 VOCs and pesticides with detection frequencies of 1 percent or greater at assessment levels of 0.02 µg/L in public wells in samples collected from 1993–2007. SOURCE: Toccalino and Hopple (2010) and Toccalino et al. (2010)

 

Overall, the USGS studies show that there is widespread, very low level contamination of private and public wells by VOCs, with a reasonable estimate being 60 to 65% of public wells having detectable VOCs. According to the data sets of Toccalino and Hopple (2010) and Toccalino et al. (2010), approximately 1% of sampled public wells have levels of VOCs above MCLs. Thus, water from these wells requires additional treatment to remove the contaminants before it is provided as drinking water to the public. EPA (2009b) compiled over 309,000 groundwater measurements of PCE and TCE from raw water samples at over 46,000 groundwater-derived public water supplies in 45 states. Compared to the USGS data, this report gives a lower percentage of water supplies being contaminated: TCE concentration exceeded its MCL in 0.34 percent of the raw water samples from groundwater-derived drinking water supply systems. There are other potential sources of VOCs in groundwater beyond hazardous waste sites. For example, chloroform is a solvent but also a disinfection byproduct, so groundwater sources impacted by chlorinated water (e.g., via aquifer storage/recharge, leaking sewer pipes) would be expected to show chloroform detections. Another correlation seen in the USGS data is that domestic and public wells in urban areas are more likely to have VOC detections that those in rural areas. This finding is not unexpected given the much higher level of industrial practices in urban areas that can result in releases of these chemicals to the subsurface. Another way to estimate the number of public water supplies affected by contaminated groundwater is to consider the number of water supply systems that specifically seek to remove organic contaminants. The EPA Community Water System Survey (EPA, 2002) reports that 2.3 to 2.6 percent of systems relying solely on groundwater have “organic contaminant removal” as a treatment goal. For systems that use both surface water and groundwater, 10.3 to 10.5 percent have this as a treatment goal.

 

In summary, it appears that the following conclusions about the contamination of private and public groundwater systems can be drawn: (1) there is VOC contamination of many private and public wells (upwards of 65%) in the U.S., but at levels well below MCLs; the origin of this contamination is uncertain and the proportion caused by releases from hazardous waste sites is unknown; (2) approximately one in 10 NPL facilities is impacting or significantly threatening a drinking water supply system relying on groundwater, requiring wellhead treatment or the use of alternative water sources; and (3) public wells are more susceptible to contamination than private wells, due their higher likelihood of being in urban areas and their higher pumping rates and hydraulic capture zones.

 

All of these issues suggest that there can be no generalizations about the condition of sites referred to as “closed,” particularly assumptions that they are “clean,” meaning available for unlimited use and unrestricted exposure. Indeed, the experience of the Committee in researching “closed sites” suggests that many of them contain contaminant levels above those allowing for unlimited use and unrestricted exposure, even in those situations where there is “no further action” required.

 

Furthermore, it is clear that states are not tracking their caseload at the level of detail needed to ensure that risks are being controlled subsequent to “site closure.” Thus, reports of cleanup success should be viewed with caution.

 

CONCLUSIONS AND RECOMMENDATIONS

 

The Committee’s rough estimate of the number of sites remaining to be addressed and their associated future costs is presented in Table 2-6, which lists the latest available information on the number of facilities (for CERCLA and RCRA) and contaminated sites (for the other programs) that have not yet reached closure, and the estimated costs to remediate the remaining sites.

 

 

water/contaminated

 

TABLE 2-6 Rough Estimate of the total number of currently known facilities or contaminated sites that have Not reached closure and estimated costs to complete

 

 

At least 126,000 sites across the country have been documented that have residual contamination at levels preventing them from reaching closure. This number is likely to be an underestimate of the extent of contamination in the United States for a number of reasons. First, for some programs data are available only for contaminated facilities rather than individual sites; for example, RCRA officials declined to provide an average number of solid waste management units per facility, noting that it ranged from 1 to “scores.” CERCLA facilities frequently contain more than one individual release site. The total does not include DoD sites that have reached remedy in place or response complete, although some such sites may indeed contain residual contamination. Finally, the total does not include sites that likely exist but have not yet been identified, such as dry cleaners or small chemical-intensive businesses (e.g., electroplating, furniture refinishing).

 

 

Information on cleanup costs incurred to date and estimates of future costs, as shown in Table 2-6, are highly uncertain. Despite this uncertainty, the estimated “cost to complete” of $110-$ 127 billion is likely an underestimate of future liabilities. Remaining sites include some of the most difficult to remediate sites, for which the effectiveness of planned remediation remains uncertain given their complex site conditions. Furthermore, many of the estimated costs (e.g., the CERCLA figure) do not fully consider the cost of long-term management of sites that will have contamination remaining in place at high levels for the foreseeable future.

 

Remedial Objectives, Remedy Selection, and Site Closure

The issue of setting remedial objectives touches upon every aspect and phase of soil and groundwater cleanup, but none perhaps as important as defining the conditions for “site closure.” Whether a site can be “closed” depends largely on whether remediation has met its stated objectives, usually stated as “remedial action objectives.” Such determinations can be very difficult to make when objectives are stated in such ill-defined terms as removal of mass “to the maximum extent practicable.” More importantly, there are debates at hazardous waste sites across the country about whether or not to alter long-standing cleanup objectives when they are unobtainable in a reasonable time frame. For example, the state of California is closing a large number of petroleum underground storage tank sites that are deemed to present a low threat to the public, despite the affected groundwater not meeting cleanup. In other words, some residual contamination remains in the subsurface, but this residual contamination is deemed not to pose unacceptable future risks to human health and the environment. Other states have pursued similar pragmatic approaches to low-risk sites where the residual contaminants are known to biodegrade over time, as is the case for most petroleum-based chemicals of concern (e.g., benzene, naphthalene). Many of these efforts appear to be in response to the slow pace of cleanup of contaminated groundwater; the inability of many technologies to meet drinking water-based cleanup goals in a reasonable period of time, particularly at sites with dense nonaqueous phase liquids (DNAPLs) and complicated hydrogeology like fractured rock; and the limited resources available to fund site remediation.

There is considerable variability in how EPA and the states consider groundwater as a potential source of drinking water. EPA has defined groundwater as not capable of being used as a source of drinking water if (1) the available quantity is too low (e.g., less than 150 gallons per day can be extracted), (2) the groundwater quality is unacceptable (e.g., greater than 10,000 ppm total dissolved solids, TDS), (3) background levels of metals or radioactivity are too high, or (4) the groundwater is already contaminated by manmade chemicals (EPA, 1986, cited in EPA, 2009a). California, on the other hand, establishes the TDS criteria at less than 3,000 ppm to define a “potential” source of drinking water. And in Florida, cleanup target levels for groundwater of low yield and/or poor quality can be ten times higher than the drinking water standard (see Florida Administrative Code Chapter 62-520 Ground Water Classes, Standards, and Exemptions). Some states designate all groundwater as a current or future source of drinking water (GAO, 2011).

The Limits of Aquifer Restoration

As shown in many previous reports (EPA, 2003; NRC, 1994, 1997, 2003, 2005), at complex groundwater contamination sites (particularly those with low solubility or strongly adsorbed contaminants), conventional and alternative remediation technologies have not been capable of reducing contaminant concentrations (particularly in the source area) to drinking water standards quickly.

 

 

Posted in Chemicals, Hazardous Waste, National Academies of Sciences, Water Pollution | Tagged , , , | 1 Comment

Book review of Fruits of Eden: David Fairchild & Americas Plant Hunters

Preface. Botanist David Fairchild is one of the reasons the average grocery store has 39,500 items. Before he came along, most people ate just a few kinds of food day in day out (though that was partly due to a lack of refrigeration).

I have longed to eat a mangosteen ever since I read this book, Fairchild’s favorite fruit, with mango a close second. But no luck so far.

What wonderful and often adventurous work Fairchild and other botanists had traveling all over the world in search of new crops American farmers could grow. Grains that could grow in colder climates were sought out.

Since 80 to 90% of future generations will be farmers after fossil fuels are gone, who will be growing food organically since fertilizer and pesticides are made from natural gas and oil, it would be wise for them to plant as many varieties of crops as possible not only for gourmet meals, but biodiversity, pest control, and a higher quality of life.

As usual, what follows are Kindle notes, this isn’t a proper book review.

Alice Friedemann   www.energyskeptic.com  author of  “Life After Fossil Fuels: A Reality Check on Alternative Energy”, 2021, Springer; “When Trucks Stop Running: Energy and the Future of Transportation”, 2015, Springer; Barriers to Making Algal Biofuels, and “Crunch! Whole Grain Artisan Chips and Crackers”. Podcasts: Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity , XX2 report

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Amanda Harris.  2015. Fruits of Eden: David Fairchild and Americas Plant Hunters. University Press of Florida.   

At the end of the 19th century, most food in America was bland and brown. The typical family ate pretty much the same dishes every day. Their standard fare included beefsteaks smothered in onions, ham with rank-smelling cabbage, or maybe mushy macaroni coated in cheese. Since refrigeration didn’t exist, ingredients were limited to crops raised in the backyard or on a nearby farm. Corn and wheat, cows and pigs dominated American agriculture and American kitchens.

Fairchild transformed American meals by introducing foods from other countries. His campaign began as a New Year’s Resolution for 1897 and continued for more than 30 years, despite difficult periods of xenophobia at home and international warfare abroad. After he persuaded the United States Department of Agriculture to sponsor his project, he sent other smart, curious botanists to Asia, Africa, South America, and Europe to find new foods and plants. They explored remote jungles, desert oases, and mountain valleys and shipped their discoveries to government gardeners for testing across America. Collectively, the plant explorers introduced more than 58,000 items.

Many of their discoveries have been used as breeding material to improve existing plants, and others have become staples of the American table like mangoes, avocados, soybeans, figs, dates, and Meyer lemons.

Fairchild arrived in the nation’s capital on July 25, 1889, four months after the inauguration of Benjamin Harrison, a Republican from Indiana. The United States totaled 38, although four new ones— North Dakota, Washington, South Dakota, and Montana—would be added in November 1889. The country’s population was a little more than 50 million. Farming was an enormously important segment of the economy: the market value of agricultural products was more than $500 million (more than $12.5 billion in current dollars). Young scientists working to improve agriculture were as valuable to the nation as rocket scientists would be 75 years later.

Despite the national importance of farming, the U.S. Department of Agriculture had become a cabinet-level agency—one of seven—only a few months earlier. For decades, presidents had considered creating a separate office to help farmers, but many legislators, especially southerners, vehemently opposed granting the federal government any official role in the family farm, a fiercely independent American institution.  Congress had finally established the office in 1862 only because the southern states had seceded, leaving northern senators and representatives free to approve the legislation without opposition.

After the Civil War ended, his uncle Thomas Barbour Bryan built Graceland Cemetery, a significant urban development that was the city’s first landscaped burial ground. He hired his nephew, Bryan Lathrop, to manage the cemetery, a job he apparently did well. Creating Graceland would probably have remained the family’s biggest accomplishment if not for the Great Chicago Fire of Sunday, October 8, 1871, a day that created one of the biggest real estate investment opportunities in American history. The fire triggered a chain of events that transformed urban architecture and, in the process, produced the personal fortune that bankrolled America’s first plant expeditions.

After Fairchild arrived in Naples he immediately recognized how unexciting American meals had been. “No sooner had I landed in Italy that I began to get a perspective on the limited number of foods which the fare in my home and in American boarding houses had brought to my palate,” he wrote later. His education began in a small restaurant where he usually ate lunch. There he sampled his first foreign food: a dried fig, a wickedly sweet morsel for a young man raised on boiled vegetables. He tried vermicelli with a sauce of tomatoes, a fruit whose possibly poisonous qualities were still being debated in America. He enjoyed Italian pasta so much—it was chewy and flavorful, not the mushy kind made with soft American wheat—that he collected 52 shapes and mailed them to friends in Washington.

As he rushed away from Corsica Fairchild stole a few cuttings from citron trees along a road and hid them under his coat. Unequipped with material to protect the branches from drying out on the long voyage between Italy and America, he jammed the sticks into raw potatoes, packaged the lot and mailed them. The potatoes provided enough moisture to nourish the cuttings, which survived the trip to Washington. Officials sent the twigs to California, where they launched a profitable business.

At the end of 1895, Fairchild went to Java. The ship landed on the west coast of Sumatra at the village of Padang, a collection of low buildings strung along the waterfront and backed by thick jungle. Fairchild was finally in the South Seas, on the verge of seeing the world he had dreamed about in Kansas. He never forgot the thrill of his first visit. “The memory of that first tropical night on shore and of the noise of the myriads of insects and the smell of the vegetation and the sensation of being close to wild jungles and wild people sometimes comes back to me even though millions of later experiences have left their traces on my brain.”  

The Visitors’ Laboratory at the botanical garden in Buitenzorg, a city now called Bogor, was, like the Zoological States in Naples, an unusual spot where botanists from around the world worked together. This spirit of shared scientific inquiry among researchers of all nationalities and all specialties stayed with Fairchild for the rest of his life.

“The institution was to discover and bring to light a knowledge of the plant life of the tropical world,” Fairchild wrote later. “Not for the uses of Holland and Netherlands India alone, but for the whole world of plants—a world which knows no national boundaries, a world which constitutes a vast, magnificent realm of living stuff destined to be of interest to the human race for all time.”  

Most remarkable were the unfamiliar, even bizarre tropical fruits. It was in Java, in the summer of 1896, that David Fairchild began his lifelong love affair with one food: the mangosteen. Four years later he launched a lifelong but ultimately unsuccessful push to cultivate them in America. His enthusiasm mirrored the fascination of Queen Victoria, who in 1855 allegedly promised to pay 100 pounds to the first person to bring her a single mangosteen.

After this Fairchild went to Sumatra, and after landing  toured the public market in a settlement called Pandang. It was a noisy, crowded place that offered a cornucopia of strange cultivated fruits and vegetables. Fairchild was immediately intrigued. The visit “showed me how many new and interesting food plants there were if only we had an established place where they could be sent,” he wrote.

Fairchild’s wealthy supporter, Lathrop, proposed that these strange, foreign plants be sent to America to see which ones take root, produce fruit, and make money for farmers and merchants. At the time, only about 2% of the world’s edible plants were cultivated in America, and the typical farmer grew only about twenty of them. Lathrop wanted Americans to open their mouths to new foods.

“He began to lay before me his idea of what a botanist could do if he were given the opportunity to travel and collect the native vegetables, fruits, drug plants, grains and all the other types of useful plants as yet unknown in America,” Fairchild wrote later. It was a long evening of lively debate, and in the end, Lathrop won. Fairchild agreed to join his project. He would abandon his cloistered studies in Java and take up the mission of foreign plant introduction. As the clock approached midnight, David Fairchild promised Barbour Lathrop that he would spend his life searching the globe for new foods. “Without Barbour Lathrop to goad him into an entirely different life work,” Douglas wrote later, “to pay his salary and his expenses on their long wanderings, David Fairchild might have become a quiet, little-known if distinguished plant pathologist and entomologist, a scientist-scholar whose life might have been lived almost entirely within the walls of some laboratory.

“The greatest service which can be rendered any country is to add a useful plant to its culture,” Jefferson wrote in 1800, a remark that later American plant explorers frequently quoted with pride. Jefferson had followed his own advice: he once smuggled grains of rice from Italy to Virginia in his coat pocket even though Italian officials could have executed him if he had been caught.

When Fairchild and Lathrop began the adventures that would change America’s eating habits, they looked like improbable companions. Lathrop was tall, slim, and always well dressed; in bearing he resembled the military men he admired. He carried a cane and wore a hat wherever he went. Fairchild, in contrast, was gawky and uncertain and rarely wore clothes appropriate to the occasion, whatever it was. Lathrop was demanding and critical; Fairchild was constantly frazzled. In the beginning Lathrop, who had flashing dark blue eyes and expressive bushy eyebrows, called Fairchild “my investment,” with a little bit of a sneer. Fairchild, fully aware of the contrast, felt inadequate. “Somehow I could not do anything quite to suit him,” he admitted. Fairchild was so socially awkward that he agreed to one condition of working with Lathrop: he promised not to get married while he was exploring for plants.

Their expedition began immediately with a leisurely cruise to Singapore and Siam. A few days later when he and Lathrop attended a young couple’s wedding dinner. It was a special occasion because the Crown Prince of Siam also attended the feast. Fairchild found the food unfamiliar and the formal etiquette bizarre. “During the 13-course dinner, every dish was strange to us except the rice,” he wrote later. “Each course was noiselessly placed on the table by a servant deferentially crawling on his knees. Not a person stood or walked erect while the prince and his guests were at the table. At the close of the long meal, the wives appeared and even those of royal birth all hitched themselves across the floor like a child who has not yet learned to creep.” As witnesses to the wedding ceremony, Fairchild and Lathrop were obliged by local custom to trickle perfumed water down the bride and groom’s necks as the couple knelt together with their foreheads touching. “If the others poured as much water from the jeweled conch shell as I did,” he wrote later, “the poor bride and groom must have been well soaked.

The two had a clear plan. First of all, they were only interested in new foods and other useful plants, nothing ornamental or impractical. Also, they needed trained botanists to do the hunting so the government wouldn’t be inundated with worthless material. Next, they wanted experiment gardens prepared to test the foreign plants. Finally, Swingle and Fairchild proposed, the whole operation could be funded by quietly diverting $20,000 (equal to about $500,000 today) from another line in the agriculture department’s budget. It was an audacious scheme from two junior botanists. But by then Fairchild had grown more confident.

Fairchild and Swingle were apprehensive when they entered their new boss’s office at the end of August 1897 even though they had arranged for a senior department employee to go with them to give their idea more credibility. “Secretary Wilson was a tall, gaunt man with a gray beard and deep-set eyes,” Fairchild remembered. “He sat listening to us with his eyes half closed and, at intervals, made use of the nearby spittoon. … I waited breathlessly for his verdict.

Wilson named it “the section of foreign seed and plant introduction”. No modern government had employed its own team of full-time plant explorers. In England and France, large private companies had sponsored many foreign plant expeditions to increase their profits by selling rare plants, usually showy ornamentals. These private firms were fiercely competitive and proprietary about their discoveries, but the U.S. government would be eager to share its findings with the public and let farmers make money.

Lathrop suddenly arrived in person as Fairchild was engaged in his valuable but sedentary work. Wasting no time, Lathrop tempted him with the offer of another exciting trip to faraway lands, one that would be longer and more interesting than their six-month cruise through the South Seas. When Fairchild protested that he had just started his new job, Lathrop argued that he was too inexperienced to supervise international plant collectors. If the government’s scheme were to succeed, Lathrop insisted, Fairchild couldn’t depend on strangers to send the material he wanted. He needed to visit the places himself and make important contacts with botanists, gardeners, and government officials

The two-year trip Lathrop had promised turned into a five-year odyssey. It was a remarkable adventure of luxury travel experiences, punctuated by meetings with prominent horticulturalists—few were lowly enough to be called gardeners—and casual, dreamlike botanizing sessions on remote islands.

His visit to Maine in the summer of 1898 was brief. Because Lathrop was paying the bills, traveling was always conducted on his terms: expensive, comfortable, quick, and not always in a straight line. The zigzagging began immediately after the two men left Maine for California where Fairchild met Luther Burbank, America’s first celebrity nurseryman. Burbank had caused great excitement in horticultural circles by inventing startling new varieties of fruits, vegetables, and flowers in these years before scientists understood the science of plant breeding

Trinidad, Jamaica, and Barbados received a little more attention. In Kingston, Fairchild first tasted chayote, a mild-flavored squash that he later tried hard to persuade Americans to appreciate. Fairchild collected 16 varieties of yams and four kinds of sweet potatoes, nutritious stables in the Caribbean diet.

Throughout South America, Fairchild hunted for plants the easiest way possible: he bought them in local markets and took cuttings from plants in botanical gardens. At this point in his travels everything was so new and Fairchild’s interests were so broad that he randomly collected samples of almost everything that was unfamiliar.

He shipped large batches to Washington, often without providing information or advice for the people who were supposed to test the plants. By July 1899 the department had received more than 200 samples of Latin American beans, peppers, squashes, melons, peas, apples, and other fruits and vegetables. Fairchild’s most successful discovery during the first part of the expedition was an alfalfa from Lima, Peru, that eventually flourished as a forage plant in Arizona known as the “Hairy Peruvian”.

In Chile he bought a bushel of avocado seeds that wound up in California; they produced one of the earliest varieties grown there. Many foods Fairchild collected failed; he admitted that a large percentage of the plants he shipped were lost before they got a chance to grow in America.

The men were constantly exposed to illness. When they arrived in Panama in February 1899, a few years after yellow fever had forced French engineers to abort construction of the canal there, Panama was considered the most dangerous place in South America. Death was so common that all hospital patients were fitted for coffins when they were admitted for treatment.

These secret shipments included broccoli, then virtually unknown in America. In Venice Fairchild also discovered zucchini—identified as “vegetable marrow”—for sale in a market.

Before he arrived in Egypt he said he knew the word sesame only as Ali Baba’s famous password; afterward he understood it to be a source of valuable cooking oil. He also collected chickpeas, okra, strawberry spinach, and more hot peppers.

Lathrop encouraged Fairchild to buy as much cotton as possible. He shipped six bushels of seeds of three varieties, material that eventually boosted the lucrative cotton industries in Arizona and California.

Banda was an important source of nutmeg, an especially handsome plant. “There are few fruit trees more beautiful than nutmeg trees with their glossy leaves and pear-shaped, straw-colored fruits,” he recalled. “As the fruits ripen, they crack open and show the brilliant crimson mace which covers the seed or nutmeg with a thin, waxy covering. The vivid color of the fruit and the deep green foliage make the trees among the most dramatic and colorful of the tropical plant world.” Fairchild, who rarely passed up an opportunity to stroll alone among trees, spent hours wandering through nutmeg groves.

In May 1900, Fairchild visited Scandinavia to collect examples of tough-weather fruits and fodder plants.

the Chinese treated Fairchild well and he had time to introduce himself to John M. Swan, a doctor at a missionary hospital in Canton who helped him collect dozens of peaches, plums, persimmons, and other fruits. Swan also told him how to find the seeds that produce tung oil, the glossy material used to waterproof the exterior of Chinese junks.

Fairchild was able to visit rural areas outside Canton and wander among the small vegetable plots there. “These truck gardens of a city of 2,000,000 people did not contain a single vegetable with which we are familiar in America.

He watched Chinese farmers control pests the old-fashioned way: they picked off each insect on every plant by hand.

By the time Fairchild finished this two-month detour to the Persian Gulf he had collected 224 date palm offshoots or suckers, each weighing about thirty pounds.

After he arranged to send almost four tons of trees to Washington, Fairchild retraced his route and joined Lathrop in Japan in the summer of 1902. They lived comfortably at the Imperial Hotel in Tokyo where Lathrop relaxed and Fairchild searched for plants. He bought fruits and vegetables at public markets and discovered zoysia, a plant that eventually became a popular ground cover in America. At Lathrop’s insistence he also bought bamboo plants, a purchase that triggered Fairchild’s long love affair with this huge grass.

Japanese flowering cherry trees remained one of Fairchild’s passions.

During his travels with Lathrop, Fairchild constantly hunted for varieties of one particular food, the mango. It was his second favorite fruit after the mangosteen, which, despite its name, is not related.

It was Elbridge Gale’s determination and defiance of conventional, wrong-headed wisdom that inspired Fairchild to search for mangos all over the world. During the four years he spent traveling alone and with Lathrop, Fairchild sent 24 varieties from six countries, each supposedly tastier or hardier than the other.

Hansen, who emigrated from Denmark when he was seven years old, was a young plant breeder who worked in the northern plains, the region that Wilson was trying hardest to help. Hansen had done some traveling before Wilson hired him in spring 1897, having visited Russia and seven other countries for four months in 1894 while he was a student at Iowa State College and Wilson ran the plant experiment station there. Hansen also had another, more important qualification for the job. Unlike many other horticulturalists at the time, he was a plant breeder who understood that it was botanically impossible to acclimate plants to tolerate severe conditions; only cross breeding with proven hardy varieties could produce tough plants. Because Hansen possessed this scientific sophistication, Wilson trusted him to know what to look for in the field.

Hansen was thirty-one in 1897 when Wilson convinced him that the future of American agriculture depended on his returning to Russia to find material that could be introduced in the Dakotas, then a dry, unproductive region where few crops grew. The mission was haphazard and dangerous. Wilson paid him $3,000, a generous salary equal to about $78,000 in current dollars.  Shortly after Hansen arrived in Uzbek province in Turkistan in November 1897, a field of alfalfa with small blue flowers attracted his attention. He believed the plant would survive in South Dakota, where temperatures range from 50 degrees below zero to 114 degrees above, to provide year-round feed for livestock, as well as produce nitrogen to enrich the soil. Before he could recommend the plant to Secretary Wilson, however, he needed to figure out how far north the blue alfalfa grew.

On Christmas 1897 he reached Kopal in southwestern Siberia, a town on the same latitude as South Dakota, where the blue Turkistan alfalfa was still growing. Confident it could thrive on the northern plains, he sent thousands of seeds to Washington. (Years later he returned and discovered a hardier type, an alfalfa with tiny yellow flowers, and brought that one to America, too. As a lasting tribute to Hansen’s work, South Dakota State University selected blue and yellow as its school colors.)

At first the parcels trickled in from Russia; soon, however, hundreds of packages arrived in a deluge. One day in February 1898, twelve tons of seeds of a fodder plant called smooth brome grass from the Volga River district turned up. Fairchild struggled to keep the shipments straight and check for dangerous insects or diseases that might have accompanied the material. The department had organized a system of public and private experiment gardens to test the material, so Fairchild arranged the seeds into 5,000 small packages and shipped them around the country. The enormous workload made him miserable. Fairchild, who hated clerical tasks, soon decided that he would rather be exploring himself. Again he was unhappy. “Hansen felt that he had been sent out to collect, and he collected everything and collected it in quantity,” Fairchild recalled. Later in an unpublished essay his criticism was harsher: “Hansen’s collections took on the character of a nightmare.” Nonetheless, Hansen had Secretary Wilson’s support, and Wilson sent him on two more trips to Russia. Fairchild, who may have been jealous of Hansen’s close relationship with his boss, accused Plant Explorer Number One of keeping bad records, overspending, and—perhaps an explorer’s biggest sin—passing off plants he bought in a market as material he found in the wild.

The department’s second staff explorer, who was hired in July 1898, earned Fairchild’s great respect. He was Mark Alfred Carleton, Fairchild’s classmate at Kansas State Agricultural College, who had become a cereal specialist for the department after graduation. Carleton’s great passion was to improve the grains cultivated in America’s wheat belt. Born in Ohio and raised on a farm in Kansas, Carleton spent his childhood and youth watching his neighbors labor constantly to harvest good wheat. Most wheat cultivated in America at this time was a red or white winter variety with soft kernels high in starch and low in protein. America’s earliest settlers had planted it east of the Mississippi River and ground it into flour to make bread and pastry.

As pioneers moved west early in the nineteenth century, they brought seeds of these soft wheats with them, unaware that the varieties couldn’t handle the different growing conditions west of the Mississippi. Midwestern winters are too cold and summers are too hot and dry for most soft wheats. In the prairie fields of Kansas, Carleton learned, they were especially vulnerable to rust, a fungus that shrivels the grain and rots the straw.

Carleton had also learned, however, that not all farmers in Kansas had this problem. The exceptions were Mennonites who had arrived from Russia in 1873. America was the most recent home for these Protestants, who had wandered through Europe for generations. The sect had originally lived in West Prussia, but many members moved to southern Russia about 1770 when Catherine the Great convinced them to settle remote sections of her country in exchange for one hundred years of special privileges, including exemption from military service. The Mennonites were skilled farmers who thrived in the Crimea by developing through trial and error hard wheat varieties that could handle the tough climate there.

In the mid-1800s, as Catherine’s century of protection drew to an end, the Russian government warned the Mennonites that they would soon face conscription despite their pacifist convictions. Many in the community fled Russia and sought religious freedom in the New World.

After exploring for six months, Carleton returned to Washington with several types of wheat, including the hardest of all—durum, often known as macaroni wheat.

While midwestern farmers were pleased with Carleton’s seeds, midwestern millers were not. They didn’t want the trouble and expense of updating their machinery to process harder grains. “Durum, the hardest of hard wheats, met at once with the most violent opposition, chiefly from millers, but also from all grain men,” Carleton wrote later. “Various epithets, such as ‘bastard’ and ‘goose,’ were applied to the wheat without restriction.

Carleton’s promotional campaign worked. Within a few years, large grain processors relented and modified their mills to grind hard wheat into flour. Carleton’s trip cost the U.S. government about $10,000 (about $250,000 today); by 1905 the new crop was worth $10 million a year (more than $250 million today)—a 1,000 percent increase. America had so much durum wheat that the country exported 6 million bushels a year. By 2011 production rose to about 50 million bushels a year. Because of Mark Carleton, American farmers had more than enough wheat, freeing experts at the end of the nineteenth century to worry about something other than widespread famine.

Americans consumed rice primarily as a pudding, not—like most people in the world—as part of a meal’s main course. Americans demanded kernels with a clean, smooth texture. Farmers in Louisiana and Texas grew mostly long-grain varieties originally imported from Honduras, but the kernel’s length made the rice fragile. When the outer coating was polished to whiten the grains, the only kind most Americans would eat, the rice often shattered. To make the product pretty and smooth enough to attract shoppers, processors coated it with paraffin wax. Of course, this beauty came with a price; buffing removed rice’s nutrients and wax removed its taste.

America’s rice-eating habits appalled Fairchild. “Rice is the greatest food staple in the world, more people living on it than on any other, and yet Americans know so little about it that they are actually throwing away the best part of the grains of rice and are eating only the tasteless, starchy, proteinless remainder,” he wrote in a magazine article. He mocked Americans for demanding rice as shiny as “glass beads.” “A pudding of stewed, sweetened rice, dusted with cinnamon is about as unappetizing to a fastidious Japanese as a sugar-coated beefsteak filled with raisins would be to an American,” Fairchild wrote.

Those glass beads were unhealthy as well. In 1908, a decade after Knapp’s trip, scientists determined that a diet of polished white rice could cause beriberi, a discovery that forced rice growers to enrich the grains with the nutrients removed by milling.

Fairchild had taken hundreds during his travels, and as he chatted with Grosvenor, he described one unforgettable scene he had captured. In May 1901 he had gone to North Africa to find date palms. When he landed in Tunis, he noticed an astonishing spectacle: strolling through town were young women wearing yards of brilliantly colored silk and tall pointed hats. Each woman weighed about 300 pounds. “I simply could not turn my eyes away from them,” Fairchild wrote later, “and frequently turned my Kodak toward them too, although they did not like it.”  

Davidia involucrata is the most interesting and most beautiful of all trees which grow in the north temperate regions

That spring Meyer set off for Manchuria, his first long trip inside Asia. It was a remote but promising destination because Manchuria’s growing conditions were similar to those of the northern United States, the section of the country that Secretary Wilson wanted most to help. Problems plagued the trip from the beginning, however. Officials wouldn’t let Meyer travel freely because Russian and Japanese soldiers were still skirmishing in the region, a bitter after-effect of the Russo-Japanese War that had ended only seven months earlier. Notorious outlaws called the Hun-hutzes (Red Beards) also menaced the area. Despite these obstacles, Meyer, confident he would be safe, was determined to make the trip. He knew he could be physically intimidating, especially when he wore a heavy sheepskin coat, big boots, and a bearskin hat to survive temperatures that dropped to 30 degrees below zero Fahrenheit. With a revolver and a Bowie knife in his belt, Meyer was prepared to defend himself. He relished the adventure

He spent only three months in Manchuria, including side trips to northern Korea and Siberia. It was still a rough expedition: he covered 1,800 miles from Liaoyang to Vladivostock almost entirely on foot, averaging twenty miles a day for ninety days. He wore out three pairs of boots in three months. On the way he saw beautiful peonies growing wild and collected many specimens of useful plants, including one that eventually became enormously important to America: the soybean.

Meyer, recognizing that it was a mainstay of the Chinese diet, sent samples to Fairchild: he collected seeds, whole plants, even beans prepared as tofu, which he called cheese. During his travels Meyer shipped more than one hundred varieties—including ones that launched America’s vast soybean oil industry.

Meyer told de Vries that he had wanted to walk across Manchuria to Harbin, but the trip would have been too dangerous, so he took a train. Tigers, panthers, bears, and wolves lurked nearby, but Meyer said he was more afraid of humans than wild animals.

On March 31, 1908, as he was heading to Peking toward the end of his first expedition, Meyer stopped briefly in the small village of Fengtai. In a doorway he noticed something new. It was a small tree bearing about a dozen unusual fruits that looked like a cross between a lemon and an orange. Villagers told him that the strange plant was valuable; rich Chinese paid as much as ten dollars for each tree because it produced fruit all year. “The idea is to have as many fruits as possible on the smallest possible plant,” Meyer explained later. He sliced a thin branch off the tree with his Bowie knife and packed it carefully in damp moss. Meyer delivered it two months later to Fairchild. He gave the cutting an unexciting label—“Plant Introduction No. 23028”—and sent it to the department’s garden in Chico, California, to see if it would grow and, what was more important, produce fruit in America. The experiment lasted seven years, but eventually Fairchild was able to report that the cutting was a success. “Meyer’s dwarf lemon from Peking was producing a high yield,” he said. “It had begun to attract attention as a possible commercial lemon, even though its fruit flesh had an orange tint.

Six weeks after he spotted the lemon, Meyer boarded a ship in Shanghai for San Francisco. He carried twenty tons of trees, cuttings, seeds, and dried herbarium material as well as, almost as an afterthought, two rare monkeys for the National Zoo. “They cause me as much trouble as babies,” Meyer complained when he arrived in California in June 1908.

Roosevelt, who was battling with Congress over the need for tough conservation laws, wanted a firsthand account of the devastation of Wutaishan. The burly plant explorer, seated in a leather armchair in a large room decorated with moose heads and bearskin rugs, described deforestation in China to the president of the United States. “The Chinese peasants have no regard for the wild vegetation and they cut down and grub out every wild wood plant in their perpetual search for fuel,” Meyer explained

Four months later, in the leaflet he sent to Congress as his annual State of the Union message, Roosevelt quoted Meyer by name and included his photographs to illustrate the price America could pay if the nation didn’t protect its trees. Meyer’s pictures, Roosevelt told lawmakers, “show in vivid fashion the appalling desolation, taking the shape of barren mountains and gravel and sand-covered plains, which immediately follows and depends upon the deforestation of the mountains.

While Wilson was sidelined in the hospital, Paul and Homer Brett, a U.S. consul in Muscat, set off into the interior of the Arabian Peninsula to buy date palms. They traveled sixty miles through the desert under the sultan of Oman’s protection in a caravan of eleven of the sultan’s best camels, Wilson told his father. They were ambushed twice, yet they escaped unharmed each time. The assignment was not easy. The Popenoe brothers, who both had fair skin, light hair, and bright blue eyes, must have stood out dramatically in the Mideast. “As we passed through the bazaars [in Basra], merchants would spit on the ground and significantly draw their fingers across their throats,” Paul wrote later. “In Baghdad we were chased for a mile by a crowd throwing stones, and in one of the seaports of Persia a native suddenly took a shot at us with his rifle, which fortunately missed.” Despite the risks, they did not disappoint their father. The brothers bought 9,000 date palm offshoots in Baghdad and Basra and another 6,000 in Algeria and arranged to have the huge lot—each healthy offshoot stood about three feet tall and weighed thirty pounds—shipped across the Atlantic Ocean. The trees survived the voyage because Wilson Popenoe gave his portable typewriter to the ship’s captain in exchange for enough fresh water to keep the palms alive. During the last leg of the journey from Galveston, Texas, to California, the offshoots filled seventeen refrigerated railroad cars, a load so remarkable that newspapers reported the shipment in detail. Paul Popenoe’s separate journey home took long enough for him to write three hundred pages about date palms.

The trip’s primary purpose was to finish an assignment that Frank Meyer had started before he died: save the American chestnut tree. At the beginning of the 20th century, America’s native chestnuts thrived along the Eastern Seaboard. An estimated four billion trees—many as tall as 100 feet—covered about a quarter of the region’s forests. Chestnut wood was hard and straight and vital to serve the nation’s growing needs for railroad ties and telephone poles. But in 1904 a scientist at the Bronx Zoo in New York City noticed a canker or fungus spreading on the trees’ bark. Three years later the same disease was evident on chestnut trees growing across the street in the New York Botanical Garden. It was the beginning of the most significant invasion of a foreign plant disease in American history.

Fairchild’s last official day on the agriculture department’s staff was June 30, 1935. As of that date the office he established had introduced 111,857 varieties of seeds and plants to America.

 “Many of the immigrants have their little day or hour and are never again heard from,” he wrote in the 1928 Yearbook of Agriculture. “Others sink out of sight for a time and later achieve great prominence.” He could have added that a few were out-and-out flops and others were impractical curiosities that Fairchild showed off to his friends and relatives. Yet many of David Fairchild’s plant immigrants were great successes of incalculable value. Mark Carleton’s durum wheat and Frank Meyer’s soybeans completely transformed American agriculture in the twentieth century. And by the beginning of the twenty-first century, Walter Swingle’s dates and figs and Wilson Popenoe’s avocados had become staples of the American diet. Meyer’s lemon was a food lovers’ delight. Many other introductions served the important but less visible role of providing essential breeding material to make existing plants hardier or more productive.

When David Fairchild left Washington in 1924, after giving up a job that kept him at a desk for most of 20 years, his weariness suddenly vanished. Overnight, it seems, he acquired enormous energy and enthusiasm that propelled him into a constant series of adventures that filled the rest of his life. “As the fieldmen used to say, DF had it made,” Ryerson said later. His first project took him back to the tropics. While he waited for Allison Armour to outfit his ship for the scientific expedition, Fairchild helped his friends William Morton Wheeler and Thomas Barbour, an entomologist and a zoologist associated with Harvard University, set up a new scientific research center on an island in Panama’s rain forest. Initially called the Barro Colorado Island Biological Laboratory (and now known as the Smithsonian Tropical Research Institute), the facility was modeled after the botanical institutes Fairchild loved in Naples and Java.

In September 1924, David and Marian Fairchild—and sometimes their children and friends—began exploring for plants, often under Allison Armour’s sponsorship. They drove an old American car through Algeria and Morocco, visiting gardens, ancient cities, and souks. They especially enjoyed Mogador, then a drowsy little town on the sea that was home of the rare argan nut trees. Marian Fairchild showed off her firm feminist convictions by driving their Dodge sedan through Fez. “Marian takes every opportunity to run the car around through the narrow streets just to show that she is not in any way under her husband’s thumb,” Fairchild told Grosvenor on April 4, 1925.

Sumatra and nearby islands were full of fascinating, mysterious plants. In April 1926, Fairchild finally took Marian to Java, fulfilling a promise he had made when they married more than twenty years earlier. Soon after they arrived, they visited a penal colony off the coast of Java where they encountered an imprisoned headhunter. He “had failed to get as many heads as his sweetheart demanded before she would marry him,” Fairchild explained, “because the government stopped him and sent him here after his last murder.” He had only five; she wanted six.

The kepel, whose proper name is Stelechocarpus burahol, is related to the cherimoya and the pawpaw, both fruits Fairchild had promoted in America. Local guides told the Fairchilds that sultans had planted the trees and ordered their lovers to eat kepel fruit because it made their bodily fluids smell like violets. They also warned outsiders that stealing the fruit would bring bad luck. Fairchild immediately went to the open market in Djokjakarta to buy some for America. (Kepel was the 67,491st seed or plant to arrive in Washington from the ends of the earth. In 2012 the plant was growing at The Kampong in Coconut Grove.) At the age of 57, in a beautiful, rundown spot far away from home, Fairchild had discovered one of the world’s most romantic fruits.

Between trips he joined Marjory Douglas on Ernest F. Coe’s early campaign to save the Florida Everglades by becoming the first president of the Tropical Everglades Park Association and writing articles about the natural glories of the swamp. “The Everglades of South Florida have a strange and to me appealing beauty,” he said during a speech on February 28, 1929. “Their charm partakes of the charm of the Pacific Islands.” With the authority of a global traveler, he insisted that the Everglades’ natural beauty was unmatched anywhere in the world.

Fairchild’s many books and articles brought attention to his accomplishments and led to the establishment of the Fairchild Tropical Botanic Garden in Coral Gables by Colonel Robert H. Montgomery, yet another wealthy philanthropist who loved nature—he collected trees, large ones—and was charmed by David Fairchild.

The project began by accident. One day in 1936 Montgomery, an accountant and business executive with a home in Florida, was playing bridge with Stanton Griffis, a New York investor and businessman. Griffis said he wanted some land near Miami, so Montgomery obligingly bought twenty-five acres for him. But Griffis backed out of the deal, leaving Montgomery with land he didn’t need. The situation gave Montgomery the opportunity to create a garden of palms. This palmetum soon expanded into the 83-acre site that is now the Fairchild Tropical Garden. The garden officially opened on March 23, 1938. Griffis became one of its first lifetime members. Montgomery and Fairchild’s love of palm trees led to Fairchild’s last big seagoing adventure.

Fairchild bought hundreds of mangosteens in the market at Penang and sent the seeds to Wilson Popenoe, who was setting up the Lancetilla Agricultural Experiment Station in Tela, Honduras.

Popenoe planted the seeds and waited. Mangosteens are difficult plants to grow for they need the right soil and climate and, most significantly, more time than commercial growers want to give them, especially in America. However, by 1944 the orchard had produced thirty tons of David Fairchild’s favorite fruit.

By the middle of 1954, Fairchild’s own health had deteriorated. He died at home in Coconut Grove on the afternoon of August 6, 1954. He was 85.  

Posted in Agriculture, Farming & Ranching | Tagged , , , , | Comments Off on Book review of Fruits of Eden: David Fairchild & Americas Plant Hunters

A Century from Now Concrete Will be Nothing But Rubble

FL Keys Old Hwy (4)Photo: road abandoned since 1984 in the Florida Keys

Preface. Much of the material that follows is based on Robert Courland’s 2011 book Concrete Planet, which explains why concrete is an essential part of our infrastructure. And it’s all falling apart.

After water, concrete is the most widely-used substance in the world. Producing cement, a key component of concrete, is responsible for about 8% of global carbon dioxide (CO2) emissions because of the dependency of the high heat generated by coal. There are no electric, hydrogen, or other possible fuels besides fossil fuels, best explained in Chapter 9 of Life After Fossil Fuels: A Reality Check on Alternative Energy .

Related posts:

Expressways & Interstates are only designed to last for 20 years

Alice Friedemann  www.energyskeptic.com Women in ecology  author of 2021 Life After Fossil Fuels: A Reality Check on Alternative Energy best price here; 2015 When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Podcasts: Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity

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Courland writes that some of our infrastructure may last even less than a century.  For example, in the ocean, concrete shows signs of decay within 50 years according to Marie Jackson at Lawrence Berkeley National Laboratory (Yang 2013).

The problem is the iron and steel rebar reinforcement inside of concrete.  Cracks in cement can be fixed, but when air, moisture, and chemicals seep into reinforced concrete, the rebar rusts, expanding in diameter up to seven-fold, which destroys the surrounding concrete.

Roads are by far the most vulnerable, with cracks developing and water entering to rust the rebar and expand it up to 7-fold. It cracks from freeze/thaw cycles, vibration, heavy trucks, and salt to melt snow. Also vulnerable are bridges, airport runways, canals, parking lots / garages and sidewalks. Many roads have a life expectancy of 20 years or less.

Buildings are vulnerable too (Boydell 2021, Lacasse 2020)

Buildings in coastal areas are especially susceptible as the chloride in salt water accelerates rusting. Rising sea levels will raise the water table and make it saltier, affecting building foundations, while salt-spray will spread further on stronger winds.

At the same time, the concrete is affected by carbonation, a process where carbon dioxide from the air reacts with the cement to form a different chemical element, calcium carbonate. This lowers the pH of the concrete, making the steel even more prone to corrosion. Since the 1950s, global CO₂ levels have increased from about 300 parts per million in the atmosphere to well over 400. More CO₂ means more carbonation.

The tragic recent collapse of an apartment building in Miami in the US may be an early warning of this process gaining speed.

Buildings have always been less vulnerable because of their protective external cladding.  But they were designed to operate within a certain climate, and global warming is likely to increase the range of hot and cold temperatures, rain, snow, wind, ground water levels, floods, chemical deposition on metals from the atmosphere, and more solar and UV radiation. These will cause the building envelope to deteriorate more rapidly, and warmer temperatures allow wood chomping termite populations to explode.  And like roads, allow water to seep into the concrete and expand the rebar below, greatly shortening their expected lifespan.

Heat expands metals, so buildings with steel frames will suffer, and soil subsidence is expected to increase with warmer temperatures and greater rainfall.

Uh-oh, nuclear reactors are vulnerable too. This will eventually destroy nuclear reactors, spent nuclear fuel pools, and nearby waste containers (in 2009 the only contender for a nuclear waste disposal site after 40 years and $10 Billion of studies is Yucca Mountain, but it was put off limits by Energy Secretary Steven Chu in order to get Henry Reid elected).

All rocks weather, and natural disasters can crack and expose the steel rebar to corrosion, shortening its lifespan, so in the end, concrete structures are temporary: coal and natural gas power plants, buildings, homes, and skyscrapers;  dams, levees, water mains, barges, sewage and water treatment plants and pipes, schools, subways, corn and grain silos, shipping wharves and piers, tunnels, shopping malls, swimming pools, and so on will waste away.

What to do: Replacing these structures as energy declines will be far more difficult than maintaining them properly, so hopefully this will be a top priority when our throwaway society is no longer possible.  In a world that’s shrinking from declining energy resources, topsoil, aquifers, and minerals, it’s time to construct buildings that last and maintain the ones we have.

Fixing instead of rebuilding will also reduce CO2, since cement takes a lot of energy to produce, around 450 grams of coal per 900 grams of cement produced, up to 8% of global carbon dioxide emissions per year.

Courland says that engineers and architects have known about concrete’s short lifespan for a long time, yet either refuse to admit it or don’t think it matters.  The main theme of Courland’s book is that it does matter:

1)  The lifespan of concrete is not only shorter than masonry, it “is probably less than that of wood…We have built a disposable world using a short-lived material, the manufacture of which generates millions of tons of greenhouse gases.”

2)  “Even more troubling is that all this steel-reinforced concrete that we use for building our roads, buildings, bridges, sewer pipes, and sidewalks is ultimately expendable, so we will have to keep rebuilding them every couple of generations, adding more pollution and expense for our descendants to bear.  Most of the concrete structures built at the beginning of the 20th century have begun falling apart, and most will be, or already have been, demolished”.

3) The world we have built over the last century is decaying at an alarming rate. Our infrastructure is especially terrible:

  • One in four bridges are either structurally deficient or structurally obsolete
  • The service life of most reinforced concrete highway bridges is 50 years, and their average age is 42 years….
  • Besides our crumbling highway system, the reinforced concrete used for our water conduits, sewer pipes, water-treatment plants, and pumping stations is also disintegrating.  The chemicals and bacteria in sewage make it almost as corrosive as seawater, reducing the life span of the reinforced concrete used in these systems to 50 years of less.”

Perhaps the American Society of Civil Engineers (ASCE) would agree. Below is their 2017 report card for America’s infrastructure which all has a lot of concrete: Aviation (D), Bridges (C+), Dams (D), Drinking water (D), Energy (D+), Hazardous Waste (D+), Inland Waterways (D), Levees (D), Ports (C+), Public Parks (D+), Roads (D), Schools (D+), Waste Water (D+).  It will cost over $3 trillion to fix this.

Alan Weisman’s in his book, “The World Without Us”, writes of places abandoned by people, such as Chernobyl.  It doesn’t take long for vegetation to crack and take over buildings, roads, and other concrete structures.  For example, consider what knotweed can do:

Knotweed can pierce tarmac and crack concrete foundations, causing serious damage to infrastructure, and grow up to a meter per month. In winter the underground rhizome survives and can grow as much as 14 meters long and 3 meters deep. The rhizome can even survive burial by volcanic lava and send up rock-piercing shoots when the surface cools. “A plant like that will laugh at concrete foundations,” says Mike Clough of Japanese Knotweed Solutions in Manchester, UK (Pain).

Improving Concrete

There is a program to make better concrete at the National Institute of Standards & Technology Engineering Laboratory. One programs is researching how to prevent concrete from cracking in a program called REACT: Reducing Early-Age Cracking Today.  In 2007, the National Infrastructure Improvement Act, to establish a National Commission on the Infrastructure of the United States, passed in the Senate but failed in the House.

Researchers are now experimenting with root vegetables and recycled plastic in concrete to see whether this can make it stronger—and more sustainable.   Cement needs to be combined with water so it adheres to sand and crushed rock and binds them together. However, not all cement particles become hydrated during the process. Most of them remain essentially sitting there doing nothing which is a waste. If this hydration mechanism could be amplified, its strength will increase significantly and we can use less cement. At last, the carrots: incorporating sheets made from vegetable waste was able to improve cement hydration by acting as reservoirs that allowed water to reach more cement particles and thus improve its binding ability.  After hydration ends, some of these carrot nanosheets remain in the cement and make its structure very strong. But don’t hold your breath, this was done in the laboratory, and postcarbon society will be so simplified that nanosheets will not be possible.  But perhaps research on plastic will be more successful, and there is certainly plent of that around (Ceurstemont 2021).

Engineers are working on making better concrete.   The fixes below will extend lifespan one time:

  1. Using bacteria that emit limestone to self-heal concrete by mixing tiny capsules of these bacteria within concrete that multiply when a crack breaks the capsule open.  The bacteria also use up oxygen that would have corroded the steel bars.  Whether this can be done or not is not clear since concrete is a very hostile place for bacteria due to high alkalinity, and as the concrete cures, it’s likely to crush many of the microcapsules.
  2. Filling the concrete with polymer microcapsules that break open and turn into a water-resistant solid when exposed to sunlight, filling in the crack.
  3. Add spores of bacteria that can last for 50 years and food for them so that when concrete cracks, they form a glue to fix it.  This is a one-time-only fix though.
  4. Coat rebar to protect it from rust.  This special rebar takes 20 years longer to rust.

It is hard to make concrete last

Concrete tends to be made from local gravel, stone, and sand since these are very heavy and so expensive to move any distance.  So the best recipe will likely vary a bit from place to place.Steel also varies in what alloys were used, how strong and corrodable it is, and asphaltic concrete will vary depending on the crude oil source of the bitumen.  It’s often mentioned that Roman concrete lasted because of the use of volcanic ash, perhaps the Romans just lucked out with good local materials.  And Rome didn’t have to deal with the freeze-thaw cycle, rust from steel rebar, heavy trucks, and other modern insults.  Dealing with all these local materials makes it hard to come up with a one-formula fits all solution to long-lasting concrete.

According to David Fridley at Lawrence Berkeley National Laboratory: Even though Roman concrete was superior to what he have now, we use concrete for far more applications now than the romans did, many of which require rebar.  “Concrete has very high compressive strength, so it is the best material for foundations, arches, domes, etc. for which weight is the major concern. However, concrete has very poor tensile strength, so applications that require resistance to bending (such as a beam) requires the addition of rebar, as the tensile strength of steel is quite high (but compressive strength low). The Romans didn’t use their concrete for such applications. Rebar inevitably corrodes, leading to expansion (tensile stressing), cracks, spalling, and ultimately, failure.  According to an article in Nature Geoscience last fall (http://www.nature.com/ngeo/journal/v9/n12/full/ngeo2840.html), carbonation of cement is substantial, with the impact of increasing the acidity of the concrete, and thus susceptibility of the rebar to corrosion. There’s not a rebarred concrete structure today that could last a millennium.

Peak Energy and Concrete

This reminds me of the verses from the Talking Heads Nothing But Flowers out of my head:

There was a factory
Now there are mountains and rivers
There was a shopping mall
Now it’s all covered with flowers
The highways and cars
Were sacrificed for agriculture
Once there were parking lots
Now it’s a peaceful oasis
This was a Pizza Hut
Now it’s all covered with daisies
And as things fell apart
Nobody paid much attention

Why waste our remaining energy  to make concrete? At this point it seems crazy to build projects with short-term concrete we KNOW will only last for decades.  Once we stop repairing our concrete (and cement) structures, they will quickly fall apart.

Why try to rebuild our infrastructure and create vastly more greenhouse gases?

Our descendants won’t be driving much.  They’ll probably wish we had converted most of the roads to farmland, which will take centuries even after the cement is gone for the soil to recover — why not start now?  Stop maintaining roads in the national forests, rural areas, and wherever else it makes sense –let them return to gravel, jackhammer and remove the rubble while we still have the energy to do so.

De-paving and de-damming would also restore streams, fisheries, wetlands, and ecosystems for future generations.

Future generations eventually won’t have the energy to maintain, repair, or rebuild very many concrete structures in a wood energy based civilization.  Courland says it takes one cord (4 x 4 x 8 feet) of wood to make 1 cubic yard of lime.

Those of you downstream from large dams might be interested to know that Courland says they are still “undergoing the curing process, thus forestalling corrosion. It will be interesting for our descendants to discover whether the tremendous weight of these dams will continue to put off the rebar’s corrosion expansion”.

Failing dams are a double tragedy, since electricity from hydro-power will be especially valuable as one of the few (reliable) energy sources in the future.

Peter Taylor, in “Long-life Concrete: how long will my concrete last?” closes his paper with: “The need for long-lasting pavement systems is growing as budgets decrease,traffic increases,and sustainability becomes more important. Increasing complexity of concrete mixtures and the demands being placed on them means that business as usual is no longer acceptable”

After oil decline, there will be absurd amounts of concrete rubble — what the hell are people in the future going to do with 300 billion tons of concrete? Build sheep fences? Since peak oil occured in November of 2018, I suggest we have contests to figure out what to do with all the rubble, especially since the energy to make new concrete won’t exist.

References

Boydell R (2021) Most buildings were designed for an earlier climate – here’s what will happen as global warming accelerates. The Conversation.

Ceurstemont S (2021) Carrot cement: How root vegetables and ash could make concrete more sustainable. The EU Research & Innovation Magazine

Lacasse MA et al (2020) Durability and Climate Change—Implications for Service Life Prediction and the Maintainability of Buildings. Buildings.

Pain, Stephanie. 3 July 2014. How to kill knotweed: Let slip the bugs of war. NewScientist.

Yang S (2013) To improve today’s concrete, do as the Romans did. U.C. Berkeley

Posted in Concrete, Infrastructure & Collapse, Manufacturing & Industrial Heat, Peak Sand, Roads | Tagged , , , , , , , , , , , | 3 Comments

Microchip fabrication plants need electricity 24 x 7 for four months

Preface. Computer chip fabrication plants need to run continuously for months to accomplish the thousands of steps needed to make microchips. A half-hour power outage at Samsung’s Pyeongtaek chip plant caused losses of over $43 million dollars (Reuters 2019). Intermittent power will kill microprocessors when there’s no natural gas or other fossils, which today function as energy storage.

Just about anything electronic has microprocessors: televisions, VCRs, DVD players, microwaves, toasters, ovens, stoves, clothes washers, stereo systems, computers, hand-held game devices, thermostats, video game systems, alarm clocks, bread machines, dishwashers, central heating systems, washing machines, burglar alarm system, remote control TV, electric kettles, home lighting systems, refrigerators with digital temperature control, cars, boats, planes, trucks, heavy machinery, gasoline pumps, credit card processing units, traffic control devices, elevators, computer servers, most high tech medical devices, digital kiosks, security systems, surveillance systems, doors with automatic entry, thermal imaging equipment.

This is unfortunate for the Preservation of Knowledge, since so many books and journals are online only.

Continue reading →

Posted in Microchips and computers | Tagged , , , , , | 27 Comments

The orbiting solar power fantasy

Preface. This 2020 article “Solar Power Beamed Down To Earth From Space Moves Forward” will leave you all warm, fuzzy, and unworried about the future. The Scientists Will Come Up With Something. 

But that’s because you know little to nothing about orbital solar power.  It’s hard to be a bullshit detector without knowing something a topic, but you can still notice missing information.  How much will all this stuff weigh?  How much will it cost to launch into space?  How often will maintenance flights need to be made? And if the Air Force and Northrup Grumman are building this solar contraption, it might occur to you that this is more likely to be a weapon than an orbital solar power solution.

A genuine orbiting solar power generator meant to provide electricity could turn into a weapon if the computer hiccuped and allowed the down link beam to drift off target by a few degrees, slewing the beam across the countryside and barbecuing whatever was in its path with a few gigawatts of microwave radiation.  

2026  The Controversial Space Mirrors Designed to Boost Solar Power   Several scientists oppose the move over concerns that light beams could “flash blind” pilots, hamper astronomical research, and interfere with circadian rhythms, which could hinder plant growth, human sleep, and hormone release in humans and other animals. Others said the abnormal light could negatively affect the migration of nocturnal species, seasonal cycles in plants, and the rhythms of marine phytoplankton that underpin ocean food webs. International scientific societies representing around 2,500 researchers from over 30 countries have written letters to the FCC voicing their concerns. They requested that the agency conduct a full environmental review and set limits on satellite reflectivity and cumulative night sky brightness.

Alice Friedemann   www.energyskeptic.com  author of  “Life After Fossil Fuels: A Reality Check on Alternative Energy”, 2021, Springer; “When Trucks Stop Running: Energy and the Future of Transportation”, 2015, Springer; Barriers to Making Algal Biofuels, and “Crunch! Whole Grain Artisan Chips and Crackers”. Podcasts: Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity , XX2 report

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In theory, orbiting solar arrays could make electricity, convert it to microwaves and then beam that energy to a ground antenna where it would be converted back to electricity. But to make 10 trillion watts of power would require about 660 space solar power arrays, each about the size of Manhattan, in orbit about 22,000 miles above the Earth (Hoffert et al 2002).

So how are you going to get these gigantic solar power satellites into space?  Normile (2001)  estimates that it would take 1,000 space shuttle payloads to deliver the necessary material, an order of magnitude more than the number of missions needed to construct the international space station.  The average space shuttle mission cost $450 million (NASA 2020). Without breakthroughs in launching technology, space solar power “would be impractical and uneconomical for the generation of terrestrial base load power due to the high cost and mass of the components and construction.”

Nor can we be sure that there will be breakthrough advances in a number of technologies according to Richard Schwartz, an electrical engineer and dean of engineering at Purdue University in West Lafayette, Indiana (NRC 2001).

And we can’t run wires from Earth’s surface to an orbiting satellite, so the solar energy would have to be converted into electric energy on obard to power a microwave transmitter or laser emitter, and focus its beam toward a collector on Earth.  

And can you imagine how often astronauts would have to go into space to fix and maintain hundreds of these objects, how much fossil energy that would take at a time when fossil energy is declining?

And astronauts will have to up there to replace the solar panels, because space is hostile and the solar panels will suffer about eight times as much damage and degradation as they do on earth.

These truly gigantic orbital arrays could be hit by space junk and create even more space junk, taking out other satellites or orbital solar stations and their microwave emissions would probably interfere with the functioning of other satellites.

Meanwhile, shell out even more money for the enormous receiving stations on the ground.

Power beaming from geostationary orbit by microwaves  requires very large ‘optical aperture’ sizes, including a 1-km diameter transmitting antenna in outer space, and a 10 km diameter receiving rectenna on earth, for a microwave beam at 2.45 GHz. These sizes can be somewhat decreased by using shorter wavelengths, although they have increased atmospheric absorption and even potential beam blockage by rain or water droplets. Because of the thinned array curse, it is not possible to make a narrower beam by combining the beams of several smaller satellites. The large size of the transmitting and receiving antennas means that the minimum practical power level for an SPS will necessarily be high; small SPS systems will be possible, but uneconomic (Wiki 2020).

To give an idea of the scale of the problem, assuming a solar panel mass of 20 kg per kilowatt (without considering the mass of the supporting structure, antenna, or any significant mass reduction of any focusing mirrors) a 4 GW power station would weigh about 80,000 metric tons, all of which would, in current circumstances, be launched from the Earth. Very lightweight designs could likely achieve 1 kg/kW, meaning 4,000 metric tons for the solar panels for the same 4 GW capacity station. This would be the equivalent of between 40 and 150 heavy-lift launch vehicle (HLLV) launches to send the material to low earth orbit, where it would likely be converted into subassembly solar arrays, which then could use high-efficiency ion-engine style rockets to (slowly) reach GEO (Geostationary orbit).

The cost to build orbital solar is, well, out of this world.

With an estimated serial launch cost for shuttle-based HLLVs of $500 million to $800 million, and launch costs for alternative HLLVs at $78 million, total launch costs would range between $11 billion (low cost HLLV, low weight panels) and $320 billion (‘expensive’ HLLV, heavier panels).To these costs must be added the environmental impact of heavy space launch emissions, if such costs are to be used in comparison to earth-based energy production. For comparison, the direct cost of a new coal or nuclear power plant ranges from $3 billion to $6 billion per GW (not including the full cost to the environment from CO2 emissions or storage of spent nuclear fuel, respectively); another example is the Apollo missions to the Moon cost a grand total of $24 billion (1970s’ dollars), taking inflation into account, would cost $140 billion today, more expensive than the construction of the International Space Station.

SBSP costs might be reduced if a means of putting the materials into orbit were developed that did not rely on rockets. Some possible technologies include ground launch systems such as Star Tram, mass drivers or launch loops, which would launch using electrical power, or the geosynchronous orbit space elevator. However, these require technology that is yet to be developed. Project Orion (nuclear propulsion) is a low cost launch option which could be implemented without major technological advances, but would result in the release of Nuclear fallout.

Patterson (2003) wrote “It’s hard to calculate the cost per pound of deliver to the geosynchronous orbit (GSO), but Futron Corporation is paid by the companies that actually launch satellites to make estimates (www.futron.com). In 2003, Futron estimated GSO launch vehicles cost per pound at $17,000 (Western) and $7,000 (non-Western). In 2000, the costs were around $12,000 per pound. Low Earth Orbit, (LEO) is much cheaper. At $7,000 per pound, it would cost $42 billion to launch a 3,055-ton satellite into geosynchronous orbit, and another $4.2 billion for every refueling run. These costs are for UNMANNED objects.”

References

Hoffert MI, Caldeira K, Benford G, et al (2002) Advanced Technology Paths to Global Climate Stability: Energy for a Greenhouse Planet. Science 298: 981-987.

NASA (2017) Space Shuttle and International Space Station. National Aeronautics and Space Administration.

Normile D (2001) SPACE SOLAR POWER. Japan Looks for Bright Answers to Energy Needs. Science 294: 1273

NRC (2001) Laying the Foundation for Space Solar Power: An Assessment of NASA’s Space Solar Power Investment Strategy. Washington, DC:
The National Academies Press. https://doi.org/10.17226/10202.

Patterson R (14 Jan 2003) Energyresources message 28631

Wiki (2020) Space-based solar power. https://en.wikipedia.org/wiki/Space-based_solar_power

Posted in Far Out, Orbiting Solar | Tagged , , | 2 Comments

Population explosion to destroy 11% of remaining ecosystems and biodiversity

Preface. According to a recent paper in Nature Sustainability (Williams et al 2020), we are on the verge of destroying 11% of earth’s remaining ecosystems by 2050 to grow more food. We already are using 75% of Earth’s land. What a species! Reminds me of the ecology phrase “Are Humans Smarter than Yeast?”

But I have several criticisms of this research.

Proposed remedies include increasing crop yields, but we are at peak food, so that isn’t going to happen. We are also at peak pesticides, as we are running out of new toxic chemicals and pests adapt within five years on average. The second idea is to have homo sapiens stop eating meat and adopt a plant-based diet.  As long as meat is available and affordable, that simply won’t happen.  The third way is to cut food waste or loss.  That would require all of us to live in dire poverty given human nature, and then we’d all chop away at the remaining wild lands to grow more food. And finally, the 4th solution would be to export food to the nations that are going to destroy the most creatures and forests.  Which in turn would lead to expanding populations in these regions. Malthus was right about food being the only limitation on population. And it would be difficult to export food when there are 83 million more mouths to feed every year globally. 

This research article doesn’t even mention family planning and birth control as a solution.

Or point out the huge increase in greenhouse gases that would be emitted. From “Life After Fossil Fuels: A Reality Check on Alternative Energy”:  The idea that biofuels generate less CO2 than gasoline stems from the fact that biofuels are derived from plants that absorb carbon dioxide.  But land typically supports plant growth regardless of whether it’s being used to grow corn or not. Corn grown for ethanol for use in gasoline has a net benefit of storing around three tons of carbon dioxide per hectare.  But if the land had not been used for ethanol, we’d be better off.  If reforested, then 7.5-12 tons of CO2 would be stored per hectare.  A corn ethanol field, formerly a forest, will emit 12 to 35 tons of CO2 per hectare a year for 30 years (NRC 2014).  By contrast, a wetland stores 81-216 tons of carbon per acre (TCF 2020). In sum, corn doesn’t sequester carbon, but recycles it at best, releasing CO2 when made into ethanol, and absorbing CO2 in the next corn crop. Every year when land is tilled or cleared to grow crops, greenhouse gases are emitted from the soil. A carbon storehouse, soil stores 4.5 times more carbon than vegetation (Lal 2004).  Agriculture emits 30% of all global greenhouse gas emissions.

Alice Friedemann  www.energyskeptic.com Women in ecology  author of 2021 Life After Fossil Fuels: A Reality Check on Alternative Energy best price here; 2015 When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Podcasts: Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity

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Williams DR, Clark M, Buchanan GM, et al (2020) Proactive conservation to prevent habitat losses to agricultural expansion. Nature Sustainability.

If current trends continue, land clearing for agriculture will eat away at the habitats of nearly 90% of land animals by 2050. Humans have already appropriated over 75% of Earth’s lands for farms, ranches, cities and other endeavors, leaving just 11.6 of the planet’s 57.3 million square miles of land to house the wealth of global biodiversity (Watson et al. 2016).  Humans are likely to convert 1.3 million square miles of the remaining 11.6 million square miles of ecosystems to agriculture by 2050. Williams et al (2020) estimate that the conversion to cropland will further shrink the habitats of more than 17,000 species of land vertebrates, mainly in sub-Saharan Africa as well as South and Southeast Asia.

References

Watson JEM, Shanahan DF, Di Marco M, et al (2016) Catastrophic Declines in Wilderness Areas Undermine Global Environment Targets. Current Biology 26: 2929-2934.

Posted in Chemicals, Deforestation, Food production, Overpopulation | Tagged , , | 4 Comments

Negative energy return of solar PV in Northern Europe

Preface.  I once yanked this paper after huge blow back, almost as bad as nuclear proponents, but in the past few years, I have no reason to doubt Ferroni and Hopkirks methods, boundaries, or conclusions, so I’m putting this post back. If you automatically dismiss this paper because of Raugei’s rebuttal, then you need to read Ferroni et al’s rebuttal of Raugei:  Further considerations to: Energy Return on Energy Invested (ERoEI) for photovoltaic solar systems in regions of moderate insolation

An ERoEI of less than 1 means there is a net energy loss. In this paper Ferroni and Hopkirk found the EROEI of Solar PV to be negative, just .82 (+/-) 15%) in countries north of the Swiss Alps.

The problem with EROEI is that there is endless arguing over the boundaries.  For example, Prieto and Hall’s 2013 book, “Spain’s Photovoltaic Revolution-The Energy Return on Investment” had energy data for over 20 activities outside the production process of the modules, typically NOT included in EROEI studies. But these steps are necessary, or the solar PV installation won’t happen, and Pedro Prieto built several large installations and was in charge of the finances, so he knew everything required — the road built to access the site, the new transmission lines, the security fence and system and more that EROI studies typically don’t include.  

This paper goes beyond Prieto and Hall’s boundaries because they deliberately left out labor and other costs to mollify solar proponents. It didn’t do any good, they tried to get Springer to not publish their book. But this paper includes labor, the costs of the energy required to integrate and buffer intermittent PV-electricity in the grid (i.e. storage via pumped hydro, batteries, natural gas or coal backup plants), and the energy embodied in faulty equipment.  If Prieto & Hall had included these then their paper would have found a negative EROI, as Prieto wrote here. Also important is that Prieto and Hall’s EROI of 2.6 : 1 in sunny Spain is still far less than the EROI of 10 to 14 many scientists believe necessary to maintain our current civilization.

Another important finding of this paper is that based on recycling rates of PV in Germany, solar panel lifespan is closer to 17 or 18 years than 25.  And that doesn’t count the solar panels that are abandoned or tossed in the trash. But the paper doesn’t use the 17-18 year lifespan and sticks with a 25-year lifespan or the EROEI would be considerably less than the 0.82 (negative EROEI) calculated. If the real lifespan is 17 years, then the calculations of all solar PV papers need to be reduced by 43%, because solar PV EROI research assumes a lifespan of 30 years.

Other items of interest:

  1. The capacity factor during the winter period is only about 3% (or more recently in Germany during January 2015, only 2%)
  2. In the winter PV is producing at peak power for only 1.7 hours per day on average, and in the summer only 3.3 hours daily
  3. the consumption of material resources using the photovoltaic technology is at least 64 times that of nuclear energy
  4. The production of PV modules requires a process consisting of approximately 200 steps [and as I have written in many of my posts on EROI – every step takes energy and lowers the energy return on investment ]
  5. Many potentially hazardous chemicals are used during the production of solar modules. To be mentioned here is, for instance, nitrogen trifluoride (NF3), (Arnold et al., 2013), a gas used for the cleaning of the remaining silicon-containing contaminants in process chambers. According to the IPCC (Intergovernmental Panel on Climate Change) this gas has a global warming potential of approximately 16,600 times that of CO2.

In order to keep civilization running, transportation comes first, because you need to deliver tens of thousands of parts to solar PV farms, wind turbine factories, and biorefineries and transport the final contraption after assembly to its living quarters.

You’ll also need specialized trucks to build and maintain the millions of miles of transmission and distribution lines of the electric grid.  And as I make a case for in my book “When trucks stop running”, trucks can’t be electrified because batteries have a terribly low energy density, about 40 times less than oil kg for kg, and so batteries will always be too heavy when scaled up to a truck that weighs 80,000 pounds fully loaded.

So in the end, the EROEI of solar PV doesn’t matter, and EROEI distracts from the fact that civilization will end unless a drop-in fuel for diesel engines, which can only burn diesel #2, is made in massive quantities with an EROI above 10.

And with world peak oil in 2018, time is running out.

Related posts:

Alice Friedemann  www.energyskeptic.com  Author of Life After Fossil Fuels: A Reality Check on Alternative Energy; When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Women in ecology  Podcasts: WGBH, Financial Sense, Jore, Planet: Critical, Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, Kunstler 253 &278, Peak Prosperity,  Index of best energyskeptic posts

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Ferroni F, Hopkirk RJ (2016) Energy Return on Energy Invested (ERoEI) for photovoltaic solar systems in regions of moderate insolation. Energy Policy 94: 336–344

Many people believe renewable energy sources to be capable of substituting fossil or nuclear energy. However there exist very few scientifically sound studies, which apply due diligence to substantiating this impression. In the present paper, the case of photovoltaic power sources in regions of moderate insolation is analyzed critically by using the concept of Energy Return on Energy Invested (ERoEI, also called EROI). But the methodology for calculating the ERoEI differs greatly from author-to-author. The main differences between solar PV Systems are between the current ERoEI and what is called the extended ERoEI (ERoEI EXT). The current methodology recommended by the International Energy Agency is not strictly applicable for comparing photovoltaic (PV) power generation with other systems. The main reasons are due to the fact that on one hand, solar electricity is very material-intensive, labor-intensive and capital-intensive and on the other hand the solar radiation exhibits a rather low power density.

Publications in increasing numbers have started to raise doubts as to whether the commonly promoted, renewable energy sources can replace fossil fuels, providing abundant and affordable energy. Trainer (2014) stated: “Many reports have claimed to show that it is possible and up to now the academic literature has not questioned the faith. Therefore, it is not surprising that all Green agencies as well as the progressive political movements have endorsed the belief that the replacement of fossil fuels with renewables is feasible”.

However, experience from more than 20 years of real operation of renewable power plants such as photovoltaic installations and the deficient scientific quality and validity of many studies, specifically aimed at demonstrating the effective sustainability of renewable energy sources, indicate precisely the contrary.

A meta-analysis by Dale and Benson (2013) has been concerned with the global photovoltaic (PV) industry’s energy balance and is aimed at discovering whether or not the global industry is a net energy producer. It contains reviews of cumulative energy demand (CED) from 28 published reports, each concerning a different PV installation using one of the currently available technologies. The majority use either single- crystal or multi-crystalline silicon solar panels, which together effectively comprise around 90% of the market. The huge scatter in the reported CEDs is itself a strong indication that the authors of the 28 publications studied were not following the same criteria in determining the boundaries of the PV system: in setting the criteria for the calculation of the values of the embodied energy of the various materials, in the calculation of the energy invested for the necessary labor, in the calculation of the energy invested for obtaining and servicing the required capital and, in defining the conversion factors for the system’s inputs and outputs consistently in terms of coherent energy and monetary units.

In fact, the CEDs show a range, from maximum of 2000 kW he/m² of module area down to a minimum of 300 kW he/m² with a median value of 585 kW he/m². For such cases, a meta- analysis would require an additional investigation to explain the system boundary conditions leading to the more extreme values.

Pickard (2014) expresses concerns similar to those of Trainer. He examines: “the open question of whether mankind, having run through its dowry of fossil fuels, will be able to maintain its advanced global society. Given our present knowledge base, no definite answer can be reached”. His conclusion is: “it appears that mankind may be facing an obligatory change to renewable fuel sources, without having done due diligence to learn whether, as envisioned, those renewable sources can possibly suffice”.

We wish at this point to emphasize the significance of the factor ERoEI (often abbreviated elsewhere to EROI), which lies at the heart of the present paper. Arithmetically, it is most simply expressed as a ratio – the quotient obtained by dividing the total energy returned (or energy output) from a system by the total energy invested (the energy input or the system’s CED). If the quotient is larger than one, then the system can be considered to be an energy source and if the quotient is lower than one, then the same system must be considered to be an energy sink. Clearly, the difference between the total energy returned and the total energy invested is equal in absolute units to the net energy produced during system lifetime. The words “TOTAL” and “NET” are critical here.

In this paper the ERoEI analysis is applied to systems including the PV installations located in regions of modest insolation in Europe, in particular in Switzerland and Germany. The energy returned and the energy invested will be treated separately. Sufficient data records are now available for the regions of interest, from which the electrical (i.e. secondary) energy returned can be derived.

The energy invested, on the other hand, is based on the actual industrial situation for the production of silicon-based PV modules, for their transport, their installation, their maintenance and their financing. Due to the elevated costs and local environmental restrictions in Europe, PV module/panel manufacture takes place primarily in China.

Let us consider first the energy returned as the specific electrical energy produced, per unit of PV-panel surface (annually, in kW he/m2 yr and over plant lifetime, in kW he/m2).

Energy returned per unit of photovoltaic panel surface

There are two ways of approaching the calculation of yearly average and lifetime levels of electrical energy production.

The first starts with the yearly total of global horizontal irradiation, used currently as an indicator for the insolation levels at a site. The average value for Switzerland of this primary (thermal) energy (Haeberlin, 2010) lies between 1000 and 1400 kW ht/m2 yr. However, measurements with a pyranometer, from which these values are derived do not take into consideration the reduction of irradiation and hence of solar cell performance due to the presence, in the course of real operation, of accumulations of dust, fungus and bird droppings, due to surface damage, ageing and wear and finally due to atmospheric phenomena like snow, frost and condensing humidity.

We use therefore the published statistical data for thermal collectors actually in operation as an indicator for the insolation. Such data are measured as a function of the surface given in square meters. The data are available in the Swiss annual energy statistics (Swiss Federal Office of Energy, 2015) prepared and published in German and French by the Swiss Federal Office of Energy (Bundesamt für Energie) and show an average value of 400 kW ht/m2 yr (suffix “t” means “thermal”) for the last 10 years.

This is an indication of the rather low effective level of the insolation in Switzerland. It is to be noted that further to the North, in Germany, the value is about 5% lower than this.

The uptake from the incoming solar radiation is converted into electrical energy by the photovoltaic effect. The conversion process is subject to the Shockley-Queisser Limit, which indicates for the silicon technology a maximum theoretical energy conversion efficiency of 31%. Since the maximum measured efficiency under standard test conditions (vertical irradiation and temperature below 25 °C) is lower, at approximately 20%, the yearly energy return derived by this first method in the form of electricity generated, amounts to only 80 kW he/m2 yr.

An alternative route to obtaining the energy return starts with the published statistical data of the PV installations themselves. The values measured are the electrical energy flow after conversion in the inverter from direct to alternating low voltage current and the indication of the kWp peak rating of the installed PV system. In this case, applying the module surface per installed peak kWp, it is possible to calculate the electricity production per square meter of the module. According to the official Swiss energy statistics (Swiss Federal Office of Energy, 2015), an average for the last 10 years of 106 kW he/m2 yr is obtained for relatively new modules.

At this stage, we need to de fine the operational lifetime of a PV installation. This requires an assumption. Currently, vendors of PV installations quote a lifetime of 30 years, but the warranty for the material is normally limited to 5 years and all damaging events, such as damage due to incorrect installation or maintenance, hail, snow and storm, etc. lie outside the scope of responsibility of the vendor. Modules, which have failed during transport, installation or operating are collected for disposal by the European Association PV CYCLE (PV CYCLE – Operational Status Report – Europe, 2015), which is published on a monthly basis. Over the whole of Europe 13239 tonnes of failed or exhausted modules had been collected by the end of December 2015.

We must concentrate here on the history in Germany, where the records are most complete. Table 1, below, shows the peak power of PV systems installed and the weight of the modules at a range of dates starting in 1985. It is necessary to compare these figures with the mass of module material from Germany treated so far (by the end of 2015). This was 7637 tonnes. A module of 1 m2 weighs 16 kg and 1 kWp peak rating needs 9 m2 and consequently, scaling this up, a 1 MWp module will weigh approximately 144 tonnes.

The source of the values of installed capacity has been Report IEA-PVPS T1-18: 2009 “Trends in Photovoltaic Application.” This is a survey report concerning selected IEA countries between 2002 and 2008.

If the system lifetime were 30, or 25 years the quantity of dismantled modules (Table 1) should be practically zero, since by the year 1985 or 1990 (30 or 25 years ago) practically no PV systems had been installed. Now, at the end of 2015, modules corresponding to some 53 MWp , the peak power capacity installed by 1998, a time between 17 and 18 years ago, have already been dismantled. Therefore, the average lifetime could be said to be nearer to 17 than to 30 years, due to the fact that the quantity of treated material by the end of 2015 (7637 tonnes) corresponds to the capacity installed by 1998. In more recent years the quantity of new installations has increased very sharply and quality of installation design and building may be improving, or may have improved, but an extended lifetime remains to be demonstrated.

Table 1. Installed PV module capacities and weights between 1985 and 1998 in Germany  

Years ago End of year Installed capacity MWp Weight of installed modules (tonnes)
30 1985 0.5 72
25 1990 2.0 288
20 1995 17.7 2549
19 1996 27.8 4003
18 1997 41.8 6019
17 1998 53.8 7747

There are also other, external factors, which can reduce PV module lifetime, for instance the site, the weather and indeed climatic conditions. These aspects do not appear to have been treated in the scientific literature in connection with photovoltaic energy usage. The thermal cycling effects of passing clouds, the alternating night and day air temperatures varying strongly with season, the corrosion effects of humidity and the surface loading due to snow, ice and hailstones impacts should be studied and accounted for.

Furthermore, the performance during operation of PV installations has not been problem- free. For instance, in the “Quality Monitor, 2013” of the TUV Rheinland, it is stated that 30% of the modules installed in Germany have serious deficiencies. A further review published in the January 2013 issue of the magazine PHOTON states that about 70% have minor defects. It is clear that these faults influence lifetimes, downtimes and efficiencies of PV installations. Considering that many installations are not maintenance-friendly, it can be expected that such figures will continue to be seen. For the remainder of the present study a lifetime of 25 years is assumed, realizing that this too, based on the above data, tends to be optimistic.

Experience has shown that, on average, efficiency and hence performance degradations of around 1% per year of operation must be expected (Jordan and Kurtz, 2012).

In addition, module failures have been found to cause operational downtime of some 5% per year (Jahn et al., 2005).

Please note that this does not include electric grid losses.

The total energy returned over plant lifetime is 88.1 times 25, or 2203 kW he/m2. The analysis continues now, using this, the higher and more optimistic of the two values derived earlier.   

The photovoltaic technology is material, labor and capital intensive.  For general information on the photovoltaic technology we refer to the “White Paper – Towards a Just and Sustainable Solar Energy Industry”– (Silicon Valley Toxics Coalition, 2009).

In Sections 3.1, 3.2 and 3.3 of this Chapter we shall evaluate separately the characteristics, relevant for the comparison of the energy invested in PV plants with that necessary for other energy sources. This is important, as it enables us to understand the relative position in the energy mix of PV energy imposed by the limited power density of the incoming radiation, by the level of efficiency of its conversion to electricity and by the intermittent and frequently non-deliverable nature of the power output. Since most data offered by the solar energy industry refer to the installed peak power and not to the potential deliverable electrical energy, it is necessary to convert the power-based data to electrical energy relationships

The average weight of a photovoltaic module is 16 kg/m2 and the weight of the support system, inverter and the balance of the system is at least 25 kg/m2 (Myrans, 2009), whereby the weight of concrete is not included. Also, most chemicals used, such as acids/ bases, etchants, elemental gases, dopants, photolithographic chemicals etc. are not included, since quantities are small. But, we must add hydrochloric acid (HCl): the production of the solar-grade silicon for one square meter of panel area requires 3.5 kg of concentrated hydrochloric acid. Summarizing now, we have a total weight of used materials per square meter of PV module panel area of: 16 kg (module) + 25 kg (balance of plant) + 3.5 kg (significant chemicals) = 44.5 kg/m2

Since the total lifetime energy return is 2203 kW he/m²,we obtain a material flow of 20.2 g per kW he (principally steel, aluminum and copper). To compare this number with the corresponding numbers for other low CO2- emission power sources, we use the values for a nuclear power plant adapted from the “Environmental Product Declaration of Electricity from Sizewell B Nuclear Power Station (EDF Energy, 2009) for a modern power plant rated at 1500 MWe and with a design lifetime of 60 years.

The resulting material flow (principally steel) amounts to 0.31 g per kW he for a load factor of at least 85%. Thus the consumption of material resources using the photovoltaic technology is at least 64 times that of nuclear energy. This will also have a great influence on the energy invested during transport, which is not included in the usual type of energy balance analysis.

The data used in this section have been published by the solar or nuclear industries and may be biased. Important however, is that the differences in the energy balances be known in their orders of magnitude rather than in great detail.

Methodology for the calculation of the energy invested

The suppliers involved in the renewable energies industry advertise their capability to create many new jobs. The European Photovoltaic Industry Association (EPIA-Job creation, 2012) gives the value of 10 for the direct and indirect jobs needed for installation, operation and decommissioning per MWp installed. This refers to the peak power of a PV- system.

Job creation in respect to the energy produced is 94.4 jobs. Comparison with an estimate for the job creation by nuclear power plants is significant. Our study finds 13 jobs created per MW installed for the site construction, operation, maintenance, and decommissioning of a nuclear power plant. The human resources involved in the photovoltaic industry are thus revealed to be rather high – the PV technology is more than 7 times (or 94.44/13) more labor intensive than other energy sources.

Use of capital

The actual capital cost for a sample group of fully installed PV units, 2/3 roof-mounted and 1/3 free field-mounted, in Switzerland lies at or above 1000 CHF/m2 with large cost variations of up to 30%, due principally to the uncertainty in the price developments of PV modules. The NREL (National Renewable Energy Laboratory of the U.S. DOE) reports capital cost for fully installed PV units in the lower end of the price range given above. The 1000 CHF/m2 cost, translated into specific cost for installed peak power is 6000 CHF/kWp and is a result of personal experience of the authors. Now, we can compensate for the differing capacity factors of PV (9%) and fossil or nuclear (85%) plants multiplying by 9.44. This enables a comparison between PV and a nuclear power plant, which itself is much more capital intensive than other, fossil-fueled plants. The overnight cost of a large, advanced nuclear power plant is estimated currently at 5500 CHF/ kW, from a report (International Energy Agency-Projected Costs of Generating Electricity (IEA)-2015 Edition, according to Table 8.2).

The capital resource taken by the PV technology is therefore around 10 times that of a nuclear power plant and nearly 45 times that of fossil-fueled power plants.

The purpose of this section is to define and present the calculations for the total energy invested. For this, it is important first to define the system under investigation, its boundaries and what flows across them – i.e. materials, money and energy. There are several stages in the life cycle of an energy system.

These include the production of the necessary materials, the manufacture of the components, their transportation, installation, commissioning, operation and maintenance, decommissioning, financing, administration, their integration in the electricity supply system duly revised according to the needs of the users, and finally the essential accompanying research and development work. It is important with respect to this latter point that the quality of the energy produced be considered.

Photovoltaic plants are material, labor and capital intensive, but provide only intermittent and irregular energy production.

These characteristics have a significant and clear effect on the total energy, which must be invested in each system, whereby a system must be understood to consist of a segment of the production and manufacturing industries and then of a unit-sized PV plant and the contribution demanded by it from the revised electricity supply infrastructure.

There are many definitions of the energy invested for the ERoEI. The article “Year in review-EROI or energy return on (energy) invested” (Murphy and Hall, 2010) outlines some definitions for the EI such as: a) The energy required to collect the energy to be returned, or b) The energy required to collect, deliver, and use that energy.

Most ERoEI analyses are not very clear in de fining the system boundary for the energy invested. Here we consider on one side, the methodology used by the IEA, which uses in principle the definition a) for the calculation of the ERoEI , which we shall refer to as ERoEIIEA and our own methodology, using the definition b) for the calculation of the extended ERoEI as referred to by Murphy and Hall as ERoEIEXT.

The reader will note that the costs for the use of materials, labor and capital are all expressed in terms of equivalent electrical energy. PV technologies, consume per unit of electricity produced, 64 times more material resources, 7 times more human resources und 10 times more capital than nuclear technology.

This is a clear indication of the extreme inefficiency of the PV technologies in regions of moderate insolation in helping to achieve the objective of providing an efficient electricity supply system, which consumes a minimum of resources.

We have still not considered the facts that in the winter period the PV is producing at its peak power for the equivalent of only 1.7 hours per day on average and in the summer period, still for only 3.3 hours daily, and due to the intermittent nature of electricity produced, a parallel electricity supply infrastructure also has to be provided.

The Report IEA-PVPS T12-03: 2011 ( IEA-PVPS T12, 2011) has been prepared as a document of the International Energy Agency (IEA) by a group of experts involved in the photovoltaic industry and is more suitable for a comparison of the different PV technologies rather than for the determination of the efficiency and sustainability of the PV system as energy source. For the determination of the ERoEI, the guideline has the following deficiencies:

  1. The energy flux across the system boundaries and invested for the labor is not included.
  2. The energy flux across the system boundaries and invested for the capital is not included.
  3.  The energy invested for integration of the PV-generated electricity into a complex and flexible electricity supply and distribution system is not included (energy production does not follow the needs of the customer).  
  4. The IEA guidelines specify the use of “primary energy equivalent ” as a basis. However, since the energy returned is measured as secondary electrical energy, the energy carrier itself, and since some 64% to 67% of the energy invested for the production of solar-silicon and PV modules is also in the form of electricity (Weissbach et al., 2013) and since moreover, the rules for the conversion from carrier or secondary energy back to primary energy are not scientifically perfect (Giampietro and Sorman, 2013), it is both easier and more appropriate to express the energy invested as electrical energy. The direct contribution of fossil fuel, for instance in providing energy for process heating, also has to be converted into secondary energy. The conversion from a fossil fuel’s internal chemical energy to electricity is achieved in modern power plants with an efficiency of 38% according to the BP statistic protocol (BP Statistical Review of World Energy, June 2015). In the present paper, in order to avoid conversion errors, we shall continue to use electrical (i.e. secondary) energy in kW he/m² as our basic energy unit.
  5. The recommended plant lifetime of 30 years, based on the experiences to date, must be regarded as unrealistic.  
  6. The energy returned can and should be based on actual experimental data measured in the field. Use of this procedure will yield values in general much lower than the electricity production expected by investors and politicians.

Estimated ERoEI values for a variety of cases, have been calculated by several authors following the IEA guidelines: 5.8 was given, for example, by Brandt et al. (2013); 5.9 by Raugei et al. (2012). Weissbach et al. (2013) indicated in Table 3 in their paper an EROI of 4.95 expressed in coherent units. The tendency, when using the IEA methodology is to make use of ideal parameter values, which, in their turn, tend to yield optimistic levels of EROI.

In the authors’ opinion the IEA-guideline is not suitable for evaluating the ERoEI of the PV systems against non-PV systems in view of the fact that, as stated above, the PV technology is extremely material, labor and capital intensive, the capacity factor during the winter period is only about 3% (or more recently in Germany during January 2015, only 2%). The methodology is only suitable for comparing the various PV technologies with each other.

Methodology based on “extended ERoEI

Historically the methodology for the “extended ERoEI” is derived from the works of the ecologist Howard T. Odum, who was introducing a generalized approach to analysing energy systems, the concept of “net energy” of renewable and non-renewable energy sources and the concept of “emergy” as an expression of all the energy and material resources used in the work processes that generate a product or service (now termed embodied energy). In Odum’s book, “Environmental Accounting: Emergy and Environmental Decision Accounting (Odum, 1995) he showed that from a PV installation, considering the labour associated with the construction, operation and decommissioning no “net energy” is obtained. Charles Hall and his team, developed further the concept of ERoEI in Hall et al. (2009), in Murphy and Hall (2010) and in Murphy and Hall (2011). They have suggested that a technology with an ERoEIEXT less than 5 be considered as unsustainable.

In the extended ERoEI, the system ’s boundaries are defined so as to encompass all energy-relevant activities related to the ability to deliver a reliable, flexible and available product to the consumer on demand.

The first has to do with “upstream” factors, such as, for example, the energy it took to construct the plant for the purification of silicon to solar grade Silicon. According to the Hemlock Semiconductor Group (HSC), the investment required for the construction for such a plant for 21,000 tonnes of yearly production was approximately 4 billion US $. Due to the high flow of materials necessary to produce 1 kW he from photovoltaic installations in comparison with those from other types of energy sources, such factors should, strictly speaking, be taken into consideration. Only vague data are available at present, so in the present study they have not been included. This reduces (optimistically) the amount of energy input during the “upstream” phase. The remaining factors for the ERoEIEXT are the “downstream“ energy fluxes and losses attributable to PV.

The book “Spain’s Photovoltaic Revolution-The Energy Return on Investment” (Prieto and Hall, 2013) indicate more than 20 activities or tasks, outside the production process of the modules, which should be included in defining the system boundary and the energy or equivalent energy fluxes, which cross it. The activities are based on the comprehensive experience gained by Pedro A. Prieto during the construction of several photovoltaic projects in Spain. The estimated ERoEI including labor and financing as given in Section 7 of Prieto and Hall’s book and using coherent units, results in an ERoEI of 2.45. According to our calculations, their values of the specific embodied energy for the modules, inverters and Balance of Plant are somewhat too low. Moreover, in Spain the PV installations are in operation typically for 1.9 times the annual productive operational hours of PV installations in Switzerland or Germany, so it is possible to deduce that PV technology is not sustainable for these regions with their more modest levels of insolation.

Apart from the work of Prieto and Hall, only a few other studies have corrected any of the weak points of the IEA methodology. One of these was that by Weissbach et al. (2013), in which an energy storage capacity of 10 full-load days was estimated to be necessary to enable a system’s service target to be met. Adding this storage capacity to a system, according to Table 3 in Weissbach et al. (2013) results in an additional 10 years of equivalent energy payback time and a dramatic EROI reduction to 2.3, using coherent units. Such a result cannot be ignored and is a sound justification for working with the ERoEIEXT.

In this section the calculations made for the energy invested are reported. In addition to the system boundary as recommended in the IEA-guidelines, the following additional factors have been considered: 1. The integration of intermittent, PV-generated electricity into the grid, 2. The labour and the capital requirements.

The treatments and detail used for the estimations presented here correspond closely to those described by Prieto and Hall (2013). “Upstream” activities, such as the energy invested in building manufacturing plant, have not been included in either case. The resulting reduction of the invested energy represents again an optimistic assumption.

Cumulative energy demand (CED) or energy invested in the PVbased system

As shown in the review by Dale and Benson (2013) the results of the 28 cases reported indicate a considerable scattering of CED values. Our analysis of these studies indicates that those originally done in Japan, India, China and Malaysia all show a higher CED and a limited scattering. Whilst a large part of the solar module production industry was located in Europe before 2010, including companies such as Q-Cell, SolarWorld, BP Solar, Siemens, Bosch and REC, today almost all European companies have either been closed, have suffered huge losses or have undergone bankruptcies. Leadership of the solar industry has been taken over by Chinese companies who now represent over 70% of current world production. The main reason for this shift is the high cost of electricity in Europe, and this is very important for the energy intensive solar industry.

The production of PV modules requires a process consisting of approximately 200 steps [I’ve reformatted the paragraph to emphasize the main steps below. Every step takes ENERGY]:

  • starting from crystalline silica mining,
  • upgrading silica sand to metallurgical grade silicon,
  • upgrading metallurgical grade silicon to solar grade silicon.
  • The pulverized metallurgical grade is combined with hydrochloric acid to produce trichlorosilane.
  • This is subjected to a multistage distillation process, referred to commonly as the Siemens process, to obtain polysilicon.
  • Solar cells are produced by transforming polysilicon into cylindrical ingots of monocrystalline silicon,
  • which are then shaped and sliced into thin wafers.
  • Next a textured pattern is imparted to the surface of the wafer in order to maximize the absorption of light.
  • The wafer is then doped at high temperature with phosphorus oxychloride,
  • provided with an anti-reflective coating of silicon nitride
  • and finally printed with a silver paste (lead should be avoided) to facilitate the transport of electrical energy away from the cell.
  • A typical PV module consists of several cells wired together and encapsulated in a protective material, commonly made of ethylene vinyl acetate.
  • To provide structural integrity the encapsulated cells are mounted on a substrate frequently made of polyvinyl fluoride.
  • A transparent cover, commonly hardened glass, further protects these components.
  • The entire module is held together in an aluminum frame.

The cumulative energy demand (CED) values of some of the oriental-based cases reviewed by Dale and Benson (2013) have been analyzed and the results transformed into our coherent units, kW he per square meter in Table 2.

Table 2. CED for production of PV-systems

Reference of the

study                                     KWhe/m²            Notes

NawazandTiwari(2006) 1380       Roof-installed

NawazandTiwari(2006) 1710       Free-field

Lu andYang(2010)            1237       Roof-mounted

Kannan etal.(2006)          1224       Roof-mounted

Kato etal.(1998)                1291       Only modules, no Balance of System

Ferroni(2014)                     1287       2/3roof,1/3free field

Lundin (2013)                    1317       Nosupportincluded

Many potentially hazardous chemicals are used during the production of solar modules. To be mentioned here is, for instance, nitrogen trifluoride (NF3), (Arnold et al., 2013), a gas used for the cleaning of the remaining silicon-containing contaminants in process chambers. According to the IPCC (Intergovernmental Panel on Climate Change) this gas has a global warming potential of approximately 16600 times that of CO2.

Two other similarly undesirable “greenhouse” gases appearing are hexafluoroethane (C2F6) and sulphur hexafluoride (SF6). For further information on the chemicals involved in the solar industry, please read the White Paper “Towards a Just and Sustainable Solar Energy Industry” by the Silicon Valley Toxics Coalition (Silicon Valley Toxics Coalition, 2009).

It is stressed that, in addition to the flow of materials necessary for the production and installation estimated at 44.5 kg/m2, one must also account for the energy used to treat and transport all used chemicals and the sludge waste to a final repository. These quantities are estimated at 20 kg per square meter of solar panels.

Therefore, the energy required for the total quantity of material to be transported and estimated to be 64.5 kg per square meter of panel cannot be neglected.

For the evaluation made for the present paper of a hypothetical situation in Switzerland, the case was assumed to concern a production volume, from which 2/3 of the PV installations were destined for roof-mounting and the remaining 1/3 for free field placement. The CED value is approximately 1300 kW he/m2, consistent with the other examples in the table.

Integration of the intermittent PV-electricity into the existing grid

The intermittent generation of energy by photovoltaic and wind sources implies a need for availability of a mixture of backup power plants, mainly fossil-fueled, and for large-scale energy storage systems.

Many concepts for energy storage are available, such as hydroelectric pumped storage schemes, pressurized air storage, hydrogen production by electrolysis and storage or batteries. Here we shall consider only the pumped storage option, since this system has the lowest energy losses, at 25%, in pumping up the water and then letting it down through the turbine. Our estimation assumes further that 25% of the electricity generated by the PV system will be used to pump the water into an upper storage lake to be discharged when the consumers need electricity. In addition, losses due to conversion from low to high voltage for the pumps estimated to be 2.1% are to be included. Furthermore, in order to guarantee creation of a reliable electricity system, back-up power preferably from gas turbine driven generating plants and a smart grid will have to be devised and constructed. This too implies energy invested or energy needed for the operation of the smart grid. It has to be noted that a smart grid cannot save energy, but will consume energy to fulfil its task. Of course, the existing grid itself needs adaptation to the different electricity supply.

In Table 3, we list the calculated energy losses and extra energy to be invested in order that the customers are served according to their requirements in an integrated power supply system.

Table 3 Principal energy losses and extra energy investments due to plant and grid

integration

kWhe/m²            Losses or energy invested for additional infrastructure

149         Losses due to the pump-storage hydroelectric system 2203(el. production) x 25% X 27.1%(efficiency losses)

100         Construction of pump storage systems(1m3 Concrete–> 300 kWhe)

25           Construction of back-up gas turbine power plant

25           Grid-adaptation (1 kg copper – 11 kW he) 

50           Operation of smart-grid infrastructure

—           ——————————————–

349         TOTAL

Energy intensity in an advanced economy

It is a widely held assumption that energy consumption is related to economic activity and plays a key role in the process of economic growth. In addition, the relationship of energy to GDP (Gross Domestic Product) is also termed the “Energy Intensity” that is to say, the energy required to produce a unit of income or GDP. This gives the connection between monetary units and energy units. The publication:  “The underestimated contribution of energy to economic growth” (Ayres et al., 2013) underlines the fact that “The rather standard assumption that economic growth is independent of energy availability must be discarded absolutely” and that neither labor nor capital can function in an advanced economy without inputs of energy to the different sectors such as materials, manufacturing and services, etc.

This interdependence is seen clearly in the work of Gael Giraud, Research Director at CNRS (Centre de la recherche scientifique) in Paris. The presentation by Giraud and Kahraman (2014) summarizes the literature on the subject, showing that primary energy consumption is indeed a key factor of growth in OECD countries.

The comprehensive study “Energy and Growth: the Stylized Facts” (Csereklyei et al., 2016) analyses the energy to GDP data of 99 countries from 1971 to 2010. The main findings are that over the last 40 years there has been a stable relationship between per capita energy use and income per capita. Furthermore, energy intensity has declined globally as the world economy has grown and there has been a convergence of the figures for wealthy nations towards a value (see Figure 18 of the study) of 7.4 MJ/USD, which converts to 2.05 kW hth primary energy per dollar. This value has remained stable during recent years due to the global technological progress in advanced economies in using energy more efficiently and wisely. Of course it is related to the overall make-up of the economy, which includes energy-intensive sectors as well as less energy-intensive sectors, such as service industries.

No statistical data are available for the energy intensity due to the installation, operation, repair, servicing and decommissioning of PV-systems. Since the manufacturing sector – a sector in content similar to the diverse activities necessary for a PV system – exhibits an energy intensity higher than the overall value, we assume as a conservative value for the energy intensity of labor the typical overall value in an advanced economy. For the energy intensity of capital generation, it is reasonable again to assume the overall value of an advanced economy. Capital is the result of energy invested in previous economic activities for housing, transport, food, goods, services and other. Therefore, knowing the amount of money required and the energy intensity, it is possible to calculate the energy use.

For this analysis, since we are using the higher Swiss costs of labor and goods, we will also determine separately the Swiss secondary energy intensity to avoid statistical weak points as explained (Giampietro and Sorman, 2013). The internal national secondary energy consumption for the year 2014 may be extracted from the Swiss annual energy statistics (Swiss Federal Office of Energy, 2015). It is the sum of the primary energy of imported fossil fuels, converted to secondary energy assuming a 38% conversion efficiency according the BP statistic protocol and added to the electricity produced inland, mainly by hydro-electric or nuclear power, the figures for which already available in terms of secondary energy.

Furthermore it is necessary to consider the nature of the Swiss economy, going through a process of de-industrialization and now having practically no energy-intensive industries, but with a huge imports of energy embodied in the materials used in products made inland, such as in metals, plastics, paper and construction materials etc.. To estimate this value, using Fig. 18 of the (German language) study by the Swiss Federal Office of the Environment (2013), “Climate Change in Switzerland” (2013) and assuming that the net energy imported is proportional to the net CO2- emissions (i.e.: CO2-import minus export), it is evinced that we have to multiply the internal Swiss energy consumption by a factor of 2.17 to determine the total energy consumption. It is important to note that the national energy statistics do not attach sufficient attention to the European de-industrialization process, giving the impression that we are saving energy. However, in reality we are outplacing energy-intensive industries to regions offering low price energy and labor. This, for instance, has been the case for the energy-intensive production of solar-grade silicon.

Using the Swiss GDP, a secondary energy intensity of 0.43 kW he/CHF is obtained. Note that this value is lower than the primary global value of 2.05 kW hth/ USD that, converted to secondary energy with an efficiency of 38%, would result in 0.78 kW he/CHF. Low energy intensity indicates high energy-effi- ciency – that is to say, the generation of more units of GDP per unit of energy consumed. The higher efficiency in Switzerland is also due to the fact that the energy consumption there shows a stronger correlation with the proportion of energy used in the form of electricity. Use is made here of the BP statistics protocol for the USA, where this protocol is always used, and for Switzerland. The comparison demonstrates the proportion of electrical energy consumed in Switzerland is 48% in against 40% in the USA.

Energy invested for the labor

An additional factor neglected in the majority of studies on ERoEI is the human labor associated with the installation, operation, decommissioning and final disposal of the hazardous materials used in the production of the PV plant and of the modules themselves, where such materials as, for example, Cd, Ga and Pb are present. According to Section 3.2 we have shown that the labor involved is proportionately so much higher for PV systems than for other types of energy generation systems and therefore it must be taken into account. Equally, the human resources involved for back-up power plants and power storage systems must be considered. This, optimistically again, has not yet been included in the present study, due to a high degree of uncertainty in the chosen development plans. Based upon the authors’ experiences for typical local labor costs per square meter of PV module are: project management (10% of capital cost), installation (506 CHF per m2), operation for 25 years, including insurance (1.67% of capital cost per year for 25 years) and decommissioning (30% of installation). The total labor costs amount to 1175 CHF/m2.

To derive from these cost figures the energy involved, we use the energy intensity (kW he/CHF) for Switzerland as calculated in 5.3.1 which is 0.43. Therefore, the amount of energy invested for the human resources is an optimistic 505 kW he /m². Faulty modules and inverters appearing during the lifetime of the PV installation must be considered as a loss of embodied energy. According to the experience in Spain (Prieto and Hall, 2013) about 2% of the modules were returned or scrapped during their installation. In Switzerland many modules have been damaged by the weight of snow or the intensity of hail impacts.

In addition, inverters too, are subject to failure and during the plant’s operational lifetime an inverter often has to be replaced. The embodied energy calculated for the faulty modules and inverters amounts to 90 kW he /m².

Energy invested for the capital

We were able to see that solar energy in the form of electricity is capital intensive compared to other energy sources. Capital is the result of labor previously performed and therefore of energy previously consumed.

We assume an average capital requirement of 1100 CHF/m ² for a mix of PV plants consisting of two thirds as roof-installations and one third as free field installations including project management activities. For the sake of simplicity, we neglect the capital necessary for the construction of the back-up power sources and the power storage system as well as the capital for the necessary land to install all the equipment. We apply the method of constant annuity in order to calculate the capital required to service the necessary capital of 1100 CHF/m2, assuming an amortization period of 25 years and an average interest rate of 5%. The annuity is 7.1% minus the amortization of the energy invested over the 25 years at 4%, leaving 3.1%. The total capital necessary to serve the capital invested for 25 years is 872 CHF/m2 or 436 kW he/m2.

Table 4 Summary of the components of the total energy investments

kW he/m²            Principal energy investments

1300       Cumulative energy demand (CED) for the production of the PV-system

  349       Integration of the intermittent PV-electricity in the grid and buffering

  505       Energy invested for the labor

    90       Energy embodied for faulty equipment 

420         Energy invested necessary for the capital

—-         —————————————–

2664       Total  

The renewable energy will have to compensate for the same amounts of taxes, duties or levies as are paid by the existing electric power supply system. In Switzerland these amount to 0.0424 CHF/kW he with the addition of the Value Added Tax for the maintenance work. The total amounts to 127 CHF/m2 or 54 kW he/m2.

We see now, that the total energy required for obtaining and servicing the capital necessary for a PV-system is the sum of 366 and 54 = 420 kW he/m2.

Total energy invested

Table 4 summarizes the calculated essential energy investments for a PV system which can guarantee a reliable electricity supply to the customers. The energy contributions of subsequent activities, such as the research and development for the PV industry, have not been included. Also not included are the additional personnel that have been employed within the utility companies and the state-owned renewable energy agency, the energy required for the final disposal of the hazardous conditioned material and the energy loss due to the dumping of excess energy. Such energy dumping is a necessity to stabilize the grid during summer weekends, when, for instance, excess energy is dissipated by heating railway tracks or by disconnecting hydraulic turbines, which use river water.

Conclusion and policy implications

The calculated value for ERoEI is dimensionless, constituting the energy return (2203 kW he/m2) divided by the energy invested (2664 kW he/m2)– a ratio of 0.82.

It is estimated that these numbers could have an error of  +/- 15%, so that, despite a string of optimistic choices resulting in low values of energy investments, the ERoEI is significantly below 1. In other words, an electrical supply system based on today’s PV technologies cannot be termed an energy source, but rather a non-sustainable energy sink or a non-sustainable NET ENERGY LOSS.

The methodology recommended by the expert working group of the IEA appears to yield EROI levels which lie between 5 and 6, but which are really not meaningful for determining the efficiency, sustainability and affordability of an energy source. The main conclusions to be drawn are:

The result of rigorously calculating the “extended ERoEI” for regions of moderate insolation levels as experienced in Switzerland and Germany proves to be very revealing. It indicates that, at least at today’s state of development, the PV technology cannot offer an energy source but a NET ENERGY LOSS, since its ERoEIEXT is not only very far from the minimum value of 5 for sustainability suggested by Murphy and Hall (2011), but is less than 1.

Our advanced societies can only continue to develop if a surplus of energy is available, but it has become clear that photovoltaic energy at least will not help in any way to replace fossil fuel. On the contrary we find ourselves suffering increased dependence on fossil energy. Even if we were to select, or be forced to live in a simpler, less rapidly expanding economic environment, photovoltaic technology would not be a wise choice for helping to deliver affordable, environmentally favorable and reliable electricity regions of low, or even moderate insolation, since it involves an extremely high expenditure of material, human and capital resources.

References

Arnold, T., Harth, C.M., Mühle, J., Manning, A.J., Salameh, P.K., Kim, J., Ivy, D.J., Steele, L.P., Petrenko, V.V., Severinghaus, J.P., Baggenstos, D., Weiss, R. F., 2013. Nitrogen trifluoride global emissions estimated from updated atmospheric measurements. In: Proceedings of the National Academy of Sciences 110, no. 6 (February 5, 2013): pp. 2029–2034.

Ayres, R.U., van den Bergh, J.C.J.M., Lindenberger, D., Warr, B., 2013. The underestimated contribution of energy to economic growth. Struct. Change Econ. Dyn. 27 (2013), 79–88.

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Brandt, A. R., Dale, M., Barnhart, C.J., 2013. Calculating systems-scale energy effi- ciency and net energy return: a bottom-up matrix-based approach. Energy 62, 235–247, Dec. 2013.

Csereklyei, Z., Rubio Varas, Md.M., Stern, D.I., 2016. Energy and Economic Growth: the Stylized Facts. The Energy Journal. International Association for Energy Economics, Vol. 0 (2).

 Dale, M., Benson, S.M., 2013. Energy balance of the global photovoltaic (PV) industry – is the PV industry a net electricity producer? Environ. Sci. Technol. 2013 (47), 3482–3489.

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EPIA – Job creation, 2012. European Photovoltaic Industry Association – EPIA FACT SHEET – September.

Ferroni, F., 2014. Photovoltaic installations in Switzerland are energy sinks (in German – Photovoltaik-Stromanlagen in der Schweiz sind Energievernichter), Presentation to the Technische Gesellschaft Zürich (TGZ – Zürich Technical Society), 3rd March 2014. http://bit.ly/1QP6aK8.

Giampietro, M., Sorman, A.H., 2013. Are energy statistics useful for making energy scenarios? Energy 37 (2012) 5-1.

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Haeberlin, H., 2010. Photovoltaik-Strom aus Sonnenlicht für Verbundnetz und Inselanlagen, electrosuisse Verlag, 710 pp.

Hall, C.A.S., Balogh, S., Murphy, D.J.R., 2009. What is the minimum EROI that a sustainable society must have? Energies 2009 (2), 25–47. http://dx.doi.org/10. 3390/en20100025.

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Jahn, U., Nordmann, T., Clavadetscher, L., 2005. Performance of Grid- Connected PV Systems: Overview of PVPS Task 2 Results. IEA PVPS 2 Meeting, Florida, USA.

Jordan, D.C., Kurtz, S.R., 2012 Photovoltaic Degradation Rates – An Analytical Review. NREL/JA-pp. 5200–51664.

Kannan, R., Leong, K.C., Osman, R., Ho, H.K., Tso, C.P., 2006. Life cycle assessment study of solar PV systems: an example of a 2,7 kWp distributed solar PV system in Singapore. Sol. Energy 80 (2006), 555–563.

Kato, K., Murata, A., Sakuta, K., 1998. Energy pay-back time and life-cycle CO2 emission of residential PV power system with silicon PV module. Prog. Photovolt. Res. Appl. 6 (105–115), 1998.

Lu, I., Yang, H.X., 2010. Environmental payback time analysis of a roof-mounted building- integrated photovoltaic (BIPV) system in Hong Kong. Appl. Energy 87 (2010), 3625–3631.

Lundin, J., 2013. EROI of Crystalline Silicon Photovoltaics by Johan Lundin, Student Thesis, Master Programme in Energy Systems Engineering, University of Uppsala, 51 pp.

Murphy, D.J.R., Hall, C.A.S., 2010. Year in review-EROI or energy return on (energy) invested. Ann. N. Y. Acad. Sci. Spec. Issue Ecol. Econ. Rev. 1185, 102–118.

Murphy, D.J.R., Hall, C.A.S., 2011. Energy return on investment, peak oil and the end of economic growth. Ann. N.Y. Acad. Sci. Spec. Issue Ecol. Econ. 1219, 52–72.

Myrans, K., 2009. Comparative Energy and Carbon Assessment of Three Green Technologies for a Toronto Roof. University of Toronto, Department of Geography and Center for Environment.

Nawaz, I., Tiwari, G.N., 2006. Embodied energy analysis of photovoltaic (PV) system based on micro- and micro-level. Energy Policy 34 (17), 3144–3152.

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Pickard, W.F., 2014. Energy return on energy invested (EROI): a quintessential but possibly inadequate metric for sustainability in a solar-powered world. Proc. IEEE 102 (8), 1118–1122.

Prieto, P.A., Hall, C.A.S., 2013. Spain’s Photovoltaic Revolution – The Energy Return on Investment. By Pedro A. Prieto and Charles A.S. Hall, Springer.

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Raugei, M., Fullana-i-Palmer, P., Fthenakis, V., 2012. The energy return on energy investment (EROI) of photovoltaic: methodology and comparisons with fossil fuel cycles. Energy Policy 45, 576–582.

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Weissbach, D., Ruprecht, G., Huke, A., Czerski, K., Gottlieb, S., Hussein, A., 2013. Energy intensities, EROIs (energy returned on invested), and energy payback times of electricity generating power plants. Energy 52, 210–221.

Several of the authors below and others in a group like this one that is very pro-renewables told me that I would lose all respect in the energy community by having written about a paper that was clearly flawed and incorrect as shown in this rebuttal was written by Marco Raugei, Vasilis Fthenakis, Ugo Bardi, Charles Barnhart, Michael Carbajales-dale, and about 20 other authors: Energy Return on Energy Invested (ERoEI) for photovoltaic solar systems in regions of moderate insolation: A comprehensive response.

 

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Government plans to reduce dependency on fossil fuels won’t work

Preface. Yikes!  These government plans from 2009 won’t help the energy crisis much!  I do like these ideas though:

  • Get Yucca mountain ready to take nuclear waste. We need to sequester nuclear wastes while there is still energy to do so and not expose future generations for hundreds of thousands of years to radioactive materials.  
  • IV. Reducing demand for oil: improving efficiency A. Aggressively implement fuel-economy standards established in the Energy Independence and Security Act of 2007 (EISA).  

But electrify transportation and enhancing the national electric system?  I explain why that won’t work in “When Trucks Stop Running: Energy and the Future of Transportation”. Worst of all is enhancing the biofuels system because the energy return is negative and destroys ecosystems, topsoil, drains aquifers, and poisons the land, air, and water with pesticides, and much more — covered at great length in of “Life After Fossil Fuels: A Reality Check on Alternative Energy”.

Many items in ”Increasing energy access: expanding domestic supply” won’t work. Oil shale, methane hydrates, and coal to liquids are far from commercial and have a negative energy return, and don’t substitute for diesel.  Nor will methane hydrates see post “Why we aren’t mining methane hydrates now – or perhaps ever”.  

Nor will the arctic and Alaskan oil / coal / natural gas be exploited because icebergs will knock out offshore drills and permafrost will buckle roads and topple drills, bridges, and buildings (see arctic oil posts here).

The section “V. Managing risks and global issues” scares me. Sounds like there will be more wars in the Middle East over oil.

And nothing mentioned at all about how to keep trucks running.  If there are plans to cope with the coming energy crisis, perhaps they are classified at Homeland Security or some other agency.

Alice Friedemann  www.energyskeptic.com  Author of Life After Fossil Fuels: A Reality Check on Alternative Energy; When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Women in ecology  Podcasts: WGBH, Jore, Planet: Critical, Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, Kunstler 253 &278, Peak Prosperity,  Index of best energyskeptic posts

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Senate Hearing 111-2 (2009) Testimony on Current Energy Security Challenges. Hearing before the committee on energy and natural resources. U.S. Senate. 

The Oil Dependence Crisis

Oil is the lifeblood of the U.S. economy, providing nearly 40 percent of our primary energy needs, more than any other fuel.  Within the transportation sector, petroleum fuels account for 93 percent of delivered energy, and there are currently no substitutes available at scale.  This severe oil dependence ties the fate of our economy to the global oil market—and jeopardizes both our national security and economic prosperity as a result.

Outline of the energy security leadership council’s national strategy for energy security: Recommendations to the nation on reducing U.S. Oil Dependence

I. Diversify energy supplies for the transportation sector

A. Electrification of the transportation sector

1. Establish development of advanced battery technology as a top research priority and spend at least $500 million per year toward their development.

2. Replace existing vehicle tax credits with new tax credits of up to $8,000 per vehicle for the first two million domestically produced highly efficient vehicles.

3. Federal government should help create a market and exercise leadership by purchasing highly efficient vehicles.

4. Establish production tax incentives to aid in the retooling of U.S. vehicles manufacturing facilities and to create and maintain a domestic capacity to manufacture advanced batteries.

5. To encourage business participation, extend and modify federal subsidies for hybrid medium-duty vehicles (Classes 3–6) and heavy-duty vehicles (Classes 7–8) to 2012 and remove the cap on the number of eligible vehicles.

6. Grants to municipalities and tax credits to commercial real estate developers to encourage the installation of public recharging stations.

B. Enhancing the nation’s electrical system

a. Increasing Nuclear Power Generation and Addressing Waste Storage

1. Continue licensing process for Yucca Mountain while initiating a program of interim storage as an alternative to Yucca Mountain.

2. Extend the deadline and increase the funding levels for loan guarantees for new nuclear generation.

b. Deploying Advanced Coal Technology

1. Significantly increase investment in advanced coal R&D including development of carbon capture and storage technology and policy frame-work.

2. Increase funding for loan guarantees for advanced coal generation.

c. Promoting Renewable Energy

1. Reform and extend the Production Tax Credit (PTC) and the Investment Tax Credit (ITC) through December 31, 2013, while providing certain guidance for the transition to a fundamentally improved, next-generation incentives program.

d. Development of a Robust Transmission Grid to Move Power to Where It is Needed

1. Extend backup federal eminent domain for transmission lines to help expand the use of renewable power and to enhance reliability by moving power from surplus to deficit regions.

2. Require the Federal Energy Regulatory Commission (FERC) to approve enhanced rates of return on investments to modernize electrical grid system.

e. Transforming Consumer Demand for Electricity

1. Direct states to implement time of day pricing for electricity, and grant FERC backstop authority to implement time-of-day pricing if states will not.

2. Require utilities to install smart meters for all new installations after a specified date.

C. Reforming the biofuels program

a. Shift focus of biofuels deployment by concentrating on R&D and commercialization efforts on next-generation biofuels, fostering competition among fuels derived from differing feedstocks.

b. Require increasing production of Flexible Fuel Vehicles (FFVs).

c. Accelerate Department of Energy and Environmental Protection Agency testing and performance validation of unmodified gasoline engines running on intermediate-levels, first- and second generation biofuels blends.

d. Replace the 45-cents-per-gallon ethanol tax credit with a ‘smart subsidy’.

e. Eliminate tariffs on imported ethanol over a period of three years.

II. Increasing energy access: expanding domestic supply

A. Target federal policy and resources to encourage the expanded use of

carbon dioxide for enhanced oil recovery.

B. Support federal investment in technologies that can limit the adverse environmental impacts of oil shale and coal-to-liquids (CTL) production toensure long-term viability before undertaking public investment in production.

C. Increase access to U.S. oil and natural gas reserves on the Outer Continental Shelf (OCS) with sharply increased and expanded environmental protections.

D. Increase access to U.S. resources in the Arctic and Alaska.

E. Federal support for construction of a natural gas pipeline from Alaska to the continental United States.

F. Expand federal R&D initiatives studying the opportunities to exploit methane hydrates, including the initiation of small-scale production tests.

III. Accelerating the development and deployment of new energy-related technology

A. Annual public investment in energy R&D should be increased by roughly an order of magnitude to approximately $30 billion.

B. Reform the existing institutions and processes governing federal R&D spending.

C. Develop a more effective federal R&D investment strategy.

D. Establish new institutions to provide funding for early-stage R&D and for later-stage deployment and commercialization.

E. Invest in the next-generation workforce for the energy industry.

IV. Reducing demand for oil: improving efficiency

A. Aggressively implement fuel-economy standards established in the Energy Independence and Security Act of 2007 (EISA).

B. Increase allowable weight to 97,000 lbs. gross vehicle weight for tractor-trailer trucks that have a supplementary sixth axle installed but which replicate current stopping distances and do not fundamentally alter current truck architecture. In addition, government should study further the safety impacts of significantly longer and heavier tractor-trailers used in conjunction with slower speed limits.

C. Require the Federal Aviation Administration (FAA) to implement and fund improvements to commercial air-traffic routing in order to increase safety and decrease fuel consumption.

V. Managing risks and global issues

A. Direct the Department of Energy to develop workable guidelines for the use of the Strategic Petroleum Reserve and evaluate its proper size based on those criteria.

B. Work with foreign governments to eliminate fuel subsidies.

C. Promote a robust China-U.S. partnership on carbon capture and storage that focuses on private-sector collaboration and sharing of best practices.

D. Establish a National Energy Council at the White House to coordinate the development of the nation’s energy policy and to advise the president with regard to energy policy.

E. The National Intelligence Council should complete a comprehensive National Intelligence Estimate on energy security that assesses the most vulnerable aspects of the infrastructure critical to delivering global energy supplies and the future stability of major energy suppliers.

F. Working with the Department of State, the Department of Justice should bolster programs designed to train national police and security forces to defend and secure energy infrastructure in key countries.

G. As called for in its recent Maritime Strategy, the U.S. Navy should leverage the maritime forces of other countries to provide protection against terrorists and pirates for oil tankers in vulnerable regions.

H. The Department of Defense should engage NATO and other allies in focused negotiations with the intention of creating an architecture that improves the security of key strategic terrain.

I. The intelligence community should bolster collection and analysis capabilities on potential strategic conflicts that could disrupt key energy supplies. The State Department should improve its capacity to intervene diplomatically in conflicts that impact U.S. energy security.

J. The intelligence community should expand the collection of intelligence on national oil companies and their energy reserves in order to allow policy-makers to make better decisions about future alliances and the nation’s strategic posture on energy suppliers.

The Energy Security Leadership Council (ESLC) brings together some of America’s most prominent business and military leaders to support a comprehensive, long-term policy to reduce U.S. oil dependence and improve energy security.  

Corporate members include:

  • Frederick W. Smith, Chairman, President, and CEO of FedEx Corporation
  • David Steiner, CEO of Waste Management
  • Jeffrey Sprecher. chairman New York Stock Exchange & Intercontinental exchange
  • Herbert Kelleher, Chairman and founder of Southwest Airlines
  • Eric Schwartz  Goldman Sachs asset management
  • Military members include:
  • John Lehman former secretary of the U.S. Navy
  • General James Conway (Ret.), former Marine Corps Commandant,
  • General P.X. Kelley (Ret.), former Marine Corps Commandant and member of the Joint Chiefs of Staff.
  • General John Handy, U.S. Air Force (Ret.)
  • General John Keane, U.S. Army (Ret.)
Posted in Government on what to do, U.S. Congress Energy Dependence | Tagged , , , , , , | 3 Comments

Why we aren’t mining methane hydrates now — or perhaps ever

Preface. Methane hydrates are far from being commercial, and probably always will be. Scientists and companies have been trying to exploit them since the first energy crisis in 1973 to no avail. Nor are they likely to trigger a runaway greenhouse as I show in “Methane Apocalyse. Not Likely“.

Methane hydrate extraction in the news:

NREL 2021 Japan’s phase 4 methane hydrate research: There is still a long way to go to achieve the project’s goal of introducing marine methane hydrates into the Japanese domestic resource portfolio. The last two phases had operational problems with sand control, flow assurance, and a production rate high enough to be commercially viable. Nonetheless, there will be phase 4 from 2019 to 2022.

Alice Friedemann  www.energyskeptic.com Women in ecology  author of 2021 Life After Fossil Fuels: A Reality Check on Alternative Energy best price here; 2015 When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Podcasts: Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity
***

Gas-hydrate technologies remain at an early stage of development, despite the maturity of many of the individual exploration technologies being used. While some technologies may be widely deployed in the conventional oil and gas industry, most are not mature in the context of gas hydrates. For example, while core recovery is common practice in the oil and gas industry, coring technologies had to be adapted to enable gas-hydrate coring, and none of the pressure corers have yet reached a commercial scale; 2 Addressing issues relating to operations, e.g. number and type of wells, and size of drilling vessels; 3 Controlled-Source Electromagnetic Methods; 4 Lab work / theoretical research; 5 Bench-scale; 6 Pilot-scale; 7 Proved commercial-scale process, with optimization work in progress; 8 Commercial-scale, widely deployed, with limited optimization potential. Source: SBC Energy Institute analysis

Gas-hydrate technologies remain at an early stage of development, despite the maturity of many of the individual exploration technologies being used. While some technologies may be widely deployed in the conventional oil and gas industry, most are not mature in the context of gas hydrates. For example, while core recovery is common practice in the oil and gas industry, coring technologies had to be adapted to enable gas-hydrate coring, and none of the pressure corers have yet reached a commercial scale; 2 Addressing issues relating to operations, e.g. number and type of wells, and size of drilling vessels; 3 Controlled-Source Electromagnetic Methods; 4 Lab work / theoretical research; 5 Bench-scale; 6 Pilot-scale; 7 Proved commercial-scale process, with optimization work in progress; 8 Commercial-scale, widely deployed, with limited optimization potential. Source: SBC Energy Institute analysis

Methane hydrates are crystalline structures that are mostly water: four methane molecules per 23 water molecules. Methane is trapped within this matrix of ice, so they don’t amass in commercial quantities and the majority are too spread out to harvest for energy.

Their formation depends on low temperatures, high pressures, and water.  They’re found 2,000 to 8,000 feet deep in the ocean, often in thin and discontinuous layers, or below 600 to 3,000 foot layers of permafrost in high latitudes.

Big oil companies have known about them since 1970 yet so far haven’t found a way to extract them.

The United States Geological Survey estimates the total energy content of natural gas in methane hydrates is greater than all of the known oil, coal, and gas deposits in the world.

But that’s a wild ass guess since we can’t measure this resource, for reasons such as coring equipment that can’t handle the expansion of the gas hydrate as it’s brought to the surface.  And if you do work around this problem, there’s tremendous variability within the same area (Riedel).  Since less than 1% of is potentially extractable, there’s no point in throwing around large numbers and getting the energy illiterate excited.

According to petroleum engineer Jean Laherrère, no way do methane hydrates dwarf fossil fuels.  “Most hydrates are located in the first 600 meters of recent oceanic sediments at an average water depth of 500 meters or more, which represents just a few million years.  Fossil fuel sediments were formed over a billion years and are much thicker — typically over 6,000 meters (Laherrère).

So here it is 2014, with no commercially produced gas hydrate, despite 30 years of research at hundreds of universities, government agencies, and energy companies in the United States, Japan, Brazil, Canada, Germany, India, Norway, South Korea, China, and Russia.

Japan alone has spent about $700 million on methane-hydrate R&D over the past decade (Mann) and gotten $16,000 worth of natural gas out of it (Nelder).  I think this reflects the likely EROI of methane hydrates — .0000228 (16000/700,000,000, and yes, I know money and EROI aren’t the same). But EROI doesn’t capture the insanity as understandably as money does. Basically, for every $43,750 you spend, you get $1 back ($700,000,000 / $16,000).

Of course, it’s all theoretical.  Maybe you get $500 or $5,000 back.  Who knows? There is no commercial production now or in the foreseeable future. And we’ve tried all kinds of thermal techniques to unleash it — hot brine injection, steam injection, cyclic steam, fire flooding, and electromagnetic heating — all of them too inefficient and expensive to scale up to a commercial project (DOE 2009).

Heating them requires just 7% of the energy content released by burning them, the problem is that distributing the heat in the gas hydrate layer because “the normal pore space within the sediments is plugged up by the gas hydrates, so simple injection of a hot fluid into the hydrate layer probably will not work”. Another method would be to convince the water to migrate to a substance more attractive than the methane, an “anti-freeze”. This has been tried with methanol to no effect (Deffeyes).

Even if we found a way to get some of them, they’re so thin and dispersed that the most we could hope for is about 100 Tcfg (trillion cubic feet of gas), about 1% of the present gas URR, despite the fact that the total resources are orders of magnitude higher (Boswell).

1) Gas hydrates are cotton candy crystals mainly found in dispersed, deeply buried impermeable marine shale.

methane hydrate cotton candy
Figure 1. methane hydrate crystals form from dodecahedral clusters of water which create a cage around a single methane molecule. Source: Ken Jordan. 2005. Water Water Everywhere. Projects in Scientific computing.

In Figure 2 below, methane hydrates (yellow) in porous sands are the only resource with any chance of being exploited — a very small fraction of the overall methane hydrate resource.  Most methane hydrates are locked up in marine shales (gray) where they’ll probably remain forever because:

  • The average concentrations are extremely low, about .9 to 1.5% by volume, even in the less than 1% of highly porous sediments where there’s any chance of extracting them
  • Marine shales are impermeable, very deep, widely dispersed, with very low concentrations of methane hydrate  (Moridis et al., 2008).
  • Clathrates are far from oil and gas infrastructure, which you must use to get the methane hydrates stored and delivered
  • The infrastructure, technology, and equipment to extract gas hydrates hasn’t been invented yet
  • The energy required to get the methane hydrate out has negative Energy Returned on Energy Invested (EROEI).  It takes too much energy to heat them in order to release them plus break the bonds between the hydrates’ water molecules.
  • Inhibitor injection requires significant quantities of fairly expensive chemicals

methane hydrate resource pyramid 2

Source: Boswell, Ray, et al. 14 Sep 2010. Current perspectives on gas hydrate resources. Energy Environ. Sci., 2011,4, 1206-1215

2) Methane Hydrates are Explosive Cotton Candy

Because as temperature rises or pressure goes down when you bring these ice cubes to the surface, the gas hydrates expand to 164 times their original size. Though most are the size of sugar grains mixed in with other sediments.

methane hydrate real cotton candy

Methane hydrates bubbling up to the surface

methane hydrate green hulk 1

methane hydrate green hulk 2

3) How do you store and get these giant gas bubbles to market?

If you could keep the gas hydrates small, crystalline, and pacified, there would still be that niggling worry you might offend them into their 164-fold fury.  So it’s best to let that happen — but now where are you going to store all this gas and how will you deliver it?

You’d have to use oil and gas infrastructure in the Arctic and other questionable places where ownership isn’t settled and potentially create  geopolitical tensions.

And imagine how Exxon will feel about that!  Their oil rigs are already dodging icebergs.   Oil companies avoid drilling through methane hydrates because they can fracture and disrupt bottom sediments, wrecking the wellbore, pipelines, rig supports, and potentially take out a billion dollar offshore platform as well as other oil and gas production equipment and undersea communication cables.

4) The Mining of Gas Hydrates can cause Landslides…

Eastman states that normally, the pressure of hundreds of meters of water above keeps the frozen methane stable. But heat flowing from oil drilling and pipelines has the potential to slowly destabilize it, with possibly disastrous results: melting hydrate might trigger underwater landslides as it decomposes and the substrate becomes lubricated…

5) Which can Trigger Tsunamis

Landslides can create tsunamis that migh result in fatalities, long term health effects, and destruction of property and infrastructure.

6) Methane Hydrates are a greenhouse gas 23 times more potent than carbon dioxide

Climate scientists like James E. Hansen worry that methane hydrates in permafrost may be released due to global warming, unleashing powerful feedback loops that could cause uncontrollable runaway climate change.

Scientists believe that sudden, massive releases of methane hydrates may have led to mass extinction events in the past.

Considering that the amount of methane onshore and offshore could be 3,000 times as much as in the atmosphere, it ought to be studied a bit more before proceeding, don’t you think? (Whiteman 2013, Kvenvolden 1999).

7) Ecological Destruction

They’re dispersed across vast areas at considerable depths, which makes them very ecologically destructive to mine, since you have to sift through millions of cubic yards of silt to get a few chunks of hydrate.

8) Toxic Waste

The current state of technology uses existing oil drilling techniques, which generate wastes including produced formation water (PFW), drilling fluid chemicals, oil and water-based drilling muds and cuttings, crude oil from extraction processes and fuel/diesel from ships and equipment (Holdway 2002).

9) EROI

There are only two studies on EROI, both by Callarotti, and he looks only at the heat energy used to free the clathrates up, and it’s published in a journal called Sustainability that would better be named Gullibility when it comes to the topic of energy which is not their specialty.  He comes up with an EROI of 4/3 to 5/3 using just that one parameter.  Callarotti knows this is a dishonest figure because he says “If one were to consider the energy required for the construction of the heaters, the pipes, and the pipe and the installation process, the total EROI would be even less.”

Is he kidding?  What about the energy used to mine and crush the ore to get the metals to build the pipelines, drilling, dredging and sifting through the sediment equipment, methane hydrate processing plant, the vessel and the diesel burned to get to the remote (arctic) location, and so on.

10) Technical challenges (House 2009)

Gas hydrate wells will be more complex than most conventional and unconventional gas wells due a number of technical challenges, including:

  1. Maintaining commercial gas flows with high water production rates
  2. Operating with low temperatures and low pressures in the well-bore
  3. Controlling formation sand production into the well-bore
  4. Ensuring well structural integrity with reservoir subsidence

Technologies exist to address all of these issues, but will add to development costs. Gas hydrate development also has one distinct challenge compared to other unconventional resources, and that is the high cost of transportation to market.

Most gas fields require some compression to maximize reserve recovery, but this typically occurs later in the life of the field after production starts to fall below the plateau rate. For a gas hydrate development, the required pressure to cause dissociation will require the use of inlet compression throughout the life of the field including the plateau production time. This will require a larger capital investment for compression at the front end of the project, and will also result in higher operating costs over the life of the project.

Water production is not uncommon in gas wells, however water rates are typically less than say 10 bbls/MMscf (barrels of water per million standard cubic feet of gas) for water of condensation and/or free water production. Wells that produce excessive amounts of water are typically worked-over to eliminate water production or shut-in as non-economic. The water production from a gas hydrate reservoir could be highly variable, however water:gas ratios in excess of 1,000 bbls/MMscf are possible. This water must be removed from the reservoir and wellbore to continue the dissociation process. On this basis, a gas hydrate development will require artificial lift such as electric submersible pumps or gas lift, which will also increase capital and operating costs over the life of the field. But it is important to highlight that the water in gas hydrate contains no salts or impurities, it is fresh water and may be a valuable coproduced product of a gas hydrate development.

The combination of low operating pressures and high water rates will require larger tubing and flowlines for a gas hydrate development, in order to minimize friction losses and maximize production. Additional water handling facilities and water disposal will also be required. Larger inhibitor volume (such as glycol) will be required to prevent freezing and hydrate formation in tubing and flow-lines. Other items such as sand control, reservoir subsidence, down-hole chemical injection, possible requirements for near well-bore thermal stimulation, etc., will also require additional capital and operating costs for gas hydrate developments compared to conventional gas developments.

Onshore gas hydrates in North America are located on the North Slope of Alaska and on the Mackenzie Delta in Canada. These resources, along with significant volumes of already discovered conventional gas, are stranded without a pipeline to market. In order to compete for pipeline capacity, the economics of onshore gas hydrate developments must be attractive at prevailing gas prices.

By all estimates, the majority of gas hydrates considered for production are located in sandstone reservoirs in deepwater environments. Deepwater drilling technology and experience continues to evolve, and the worldwide deepwater fleet continues to expand. However the deepwater environment is still a very high cost and very high risk area of operation. Offshore gas hydrate developments must have strong economic drivers in order to compete with other deepwater exploration and development opportunities. Adding on the risk of gas hydrates is yet another level of risk to add onto the existing high-risk drilling in deep water.

Significant scientific and exploration work must be completed before gas hydrates can be considered as a viable source of natural gas. Critical among these tasks remains the validation reservoir and well performance through extended field testing that demonstrates the ability to produce gas hydrates at commercial rates with current technology.

So far the small-scale experiments have not been able to bring gas hydrates as far as the surface of the ocean.

On the basis of the studies done to date, gas hydrate developments will have capital and operating costs significantly higher than other unconventional or conventional developments due to well productivity, low operating pressures and temperatures, and high water production rates. Surface facilities for gas hydrate developments will also be higher due to the requirements for larger surface flowlines and inlet facilities (required because of low pressures and water production rates) and the requirement for inlet compression into the processing plant.

The reason methane hydrate production rates peak in later years, while conventional natural gas wells peak immediately is because unconventional hydrocarbons are so called because they are found in
formations other than the typical sandstone or carbonate reservoirs i.e. extremely low permeability or tight,reservoirs, shale, or coal beds the hydrocarbons are in their normal fluid condition and can typically flow without undergoing a fundamental change (except of course for bitumen). The types of reservoirs targeted for gas hydrate testing (and eventual development) are relatively high permeability conventional sandstone reservoirs however the methane gas is locked in a solid gas hydrate crystal so actually the gas is unconventional, not the reservoir. Based on simulation studies, the maximum gas production rate therefore occurs not on days one as with conventional gas reservoirs, but some time into the future, typically years.

All gas reservoirs, conventional or unconventional, are capable of their maximum rate on day one of operation. This is because the reservoir pressure is at its maximum (average reservoir pressure declines with production for most reservoirs), the gas that initially flows into the well is in the near wellbore area, and of course the gas is continuous throughout the reservoir. As gas production continues the gas that flows into the wellbore flows through the reservoir rock from greater and greater distances away. Flowing gas through the reservoir rock results in additional pressure loss, and the production rate begins to decline. Some gas wells in high permeability conventional reservoirs can flow at a more or less constant rate or steady state condition for some time, but eventually the production rate will decline. Unconventional gas reservoir production rates typically decline quite rapidly, and may never actually reach any sort of steady state production, although the rate of decline will drop and the wells may produce for many years. At the start of production for a gas hydrate reservoir, there is no free gas in the reservoir it is all locked up in the hydrate crystals in the pores space of the reservoir rock. The hydrate must first be dissociated, and then the water and free gas can flow to the well. Because water and gas is flowing simultaneously (termed multi-phase flow), the pressure loss through the reservoir will be higher than if just gas only was flowing. Gas and water saturations through the dissociated region will change with time, and gravity will affect the gas and water phases, therefore the flow mechanism will be quite complex.

Conclusion

You don’t have to be a scientist to see how difficult the problem is: 

  • Somehow you’ve got to capture the energy in thousands of square miles of exploding grains of sugar that erupt into a gas 164 times their size. 
  • There are huge deposits of natural gas that are easier to get at and far more valuable that aren’t being exploited because they’re stranded (not near pipeline infrastructure), so who’s going to invest in a resource of much lower quality at the bottom of the pyramid with such dismal prospects?
  • We can’t even drill for oil in most of the Arctic (Patzek) which is where a lot of the methane hydrates are, and that infrastructure has to be there to even think of trying to get at the methane hydrates.
  • Most of the hydrates are in a thin film on the deep ocean floor.  Are you going to build a thousand square mile blanket to trap the bubbles like a school of fish? Or use expensive fracking & coalbed methane techniques?
  • Permafrost gas hydrate is so shallow there’s not enough pressure to get it to flow fast enough to be worth mining

Gas hydrates are stranded in distant regions and deep oceans. It would be far cheaper to go after large natural gas reservoirs than attempt to go after mostly small deposits of methane hydrates we don’t even know how to extract yet.

Despite all the happy talk that says we can meet these challenges by 2025 if only there were more funding, we’re out of time.

It’s highly unlikely that Methane Hydrates will ever fuel the diesel engines that do the actual work of civilization, all of them screaming “Feed Me!” as oil declines in the future.

Methane hydrate little shop of horrors boats

References

Arango, S. O. May 7, 2013. Canada drops out of race to tap methane hydrates Funding ended for research into how to exploit world’s largest fossil energy resource. CBC News
Benton, Michael J. 2003. When Life Nearly Died: The Greatest Mass Extinction of All Time. Thames & Hudson.

BBC. 5 December 2002. The Day The Earth Nearly Died. Permian-Triassic Extinction Event

Boswell, R. 2009. Is gas hydrate energy within reach? Science.
Callarotti, R. C. 2011. Energy Return on Energy Invested (EROI) for the Electrical Heating of Methane Hydrate Reservoirs. sustainability 2011, 3.

Collett T. S. April 19-23, 2002. “Detailed analysis of gas hydrate induced drilling and production hazards,” Proceedings of the Fourth International Conference on Gas Hydrates, Yokohama, Japan.

Carrington, Damian. 23 Nov 1999. Fossil fuel revolution begins.

Deffeyes, K.S. 2005. Beyond Oil. The View from Hubbert’s Peak. Hill and Wang.

DOE 2009. U.S. Department of Energy. 2009. International Energy Outlook 2009

Eastman, Q. 2004. Energy Saviour? Or Impending Disaster? Science Notes.

Holdway, D. A. 2002. The acute and chronic effects of wastes associated with offshore oil and gas production on temperate and tropical marine ecological processes. Marine Pollution Bulletin, Vol 44: 185-203.

House. 2009. UNCONVENTIONAL FUELS PART II: THE PROMISE OF METHANE HYDRATES. U.S. House of Representatives.

Jayasinghe, A.G. 2007. Gas hydrate dissociation under undrained unloading conditions. P. 61 in Submarine Mass Movements and Their Consequences. Vol. IGCP-511. UNESCO.

Kaneshiro-Pineiro, M. et al. Dec 4, 2009. Report on the Science, Issues, Policy, and Law of Gas Hydrates as an Alternative Energy Source. East Carolina University. Coastal Resources Management Program.

Kvenvolden, K.A. 1999. Potential effects of gas hydrate on human welfare. Proceedings in the National Academy of Science. USA. 96: 3420 – 3426.

Laherrère, Jean. July 17, 2009. Update on US Gulf of Mexico: Methane Hydrates. theoildrum europe.

Mann, C. C. May 2013. What If We Never Run Out of Oil? New technology and a little-known energy source suggest that fossil fuels may not be finite. This would be a miracle—and a nightmare. The Atlantic.

Moridis, George. 2006. “Geomechanical implications of thermal stresses on hydrate-bearing sediments,” Fire in the Ice, Methane Hydrate R&D Program Newsletter.

Moridis, G.J., et al. 2008. Toward production from gas hydrates: Current status, assessment of resources, and simulation-based evaluation of technology and potential. Paper SPE 114163.Presented at the SPE Unconventional Reservoirs Conference, Keystone, Colo., February 10–12, 2008.

Nelder, C. 2013. Are Methane Hydrates Really Going to Change Geopolitics? The Atlantic.
Office of Naval Research. 5 Nov 2002. Fiery Ice From The Sea: A New World Energy Source?

NAS 2009. America’s Energy Future: Technology and Transformation. 2009. National Academy of Sciences, National Research Council, National Academy of Engineering.

Patzek, Tad. 29 Dec 2012. Oil in the Arctic. LifeItself blog.

Riedel M  and the Expedition 311 Scientists. 2006. Proceedings of the IODP, 311: Washington, DC (Integrated Ocean Drilling Program Management International, Inc).

Whiteman, G. et al. 25 July 2013. Vast costs of Arctic change. Nature, 499, 401-3.

Posted in Alternative Energy, Global Warming, Methane Hydrates | Tagged , , , , , , , | Comments Off on Why we aren’t mining methane hydrates now — or perhaps ever

Book Review of Richard Heinberg’s 2011 “The End of Growth”

Preface. This is not a book review really, it’s more a few of my kindle notes. Heinberg writes so well, so clearly, that I am sure history will remember him as the most profound and wide-ranging expert on energy and ecological overshoot. Just a few of the topics in this book include:

  • The depletion of important resources including fossil fuels and minerals
  • The proliferation of environmental impacts arising from both the extraction and use of resources (including the burning of fossil fuels)—leading to snowballing costs from both these impacts themselves and from efforts to avert them and clean them up
  • Financial disruptions due to the inability of our existing monetary, banking, and investment systems to adjust to both resource scarcity and soaring environmental costs—and their inability (in the context of a shrinking economy) to service the enormous piles of government and private debt that have been generated over the past couple of decades.

As always, I noted only what interested me.  So much is left out, so do buy this book!  And not just for yourself — I write a lot about why the electric grid will eventually come down for good in both of my Springer Books, so buy it for your grandchildren to preserve knowledge and so that future generations will understand why collapse happened.

Alice Friedemann    www.energyskeptic.com   author of 2021 Life After Fossil Fuels: A Reality Check on Alternative Energy best price here; 2015 When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”. Podcasts: Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity, XX2 report

***

Richard Heinberg. 2011. The End of Growth: Adapting to Our New Economic Reality.  New Society Publishers.

The Deepwater Horizon incident also illustrates to some degree the knock-on effects of depletion and environmental damage upon financial institutions. Insurance companies have been forced to raise premiums on deepwater drilling operations, and impacts to regional fisheries have hit the Gulf Coast economy hard.

payments forced the company to reorganize and resulted in lower stock values and returns to investors. BP’s financial woes in turn impacted British pension funds that were invested in the company. This is just one event—admittedly a spectacular one. If it were an isolated problem, the economy could recover and move on. But we are, and will be, seeing a cavalcade of environmental and economic disasters, not obviously related to one another, that will stymie economic growth in more and more ways. These will include but are not limited to: •  Climate change leading to regional droughts, floods, and even famines; • Shortages of water and energy; and • Waves of bank failures, company bankruptcies, and house foreclosures.

Each will be typically treated as a special case, a problem to be solved so that we can get “back to normal.” But in the final analysis, they are all related, in that they are consequences of growing human population striving for higher per-capita consumption of limited resources (including non-renewable, climate-altering fossil fuels), all on a finite and fragile planet.

The result: we are seeing a perfect storm of converging crises that together represent a watershed moment in the history of our species. We are witnesses to, and participants in, the transition from decades of economic growth to decades of economic contraction.

we are adding about 70 million new “consumers” each year. That makes further growth even more crucial: if the economy stagnates, there will be fewer goods and services per capita to go around.

We harnessed the energies of coal, oil, and natural gas to build and operate cars, trucks, highways, airports, airplanes, and electric grids—all the essential features of modern industrial society. Through the one-time-only process of extracting and burning hundreds of millions of years’ worth of chemically stored sunlight, we built what appeared (for a brief, shining moment) to be a perpetual-growth machine. We learned to take what was in fact an extraordinary situation for granted. It became normal.

But as the era of cheap, abundant fossil fuels comes to an end, our assumptions about continued expansion are being be shaken to their core. The end of growth is a very big deal indeed. It means the end of an era, and of our current ways of organizing economies, politics, and daily life. Without growth, we will have to virtually reinvent human life on Earth.

World leaders, if they are deluded about our actual situation, are likely to delay putting in place the support services that can make life in a non-growing economy survivable, and they will almost certainly fail to make needed, fundamental changes to monetary, financial, food, and transport systems. As a result, what could have been a painful but endurable process of adaptation could become history’s greatest tragedy. We can survive the end of growth, but only if we recognize it for what it is and act accordingly.

As early as 1998, petroleum geologists Colin Campbell and Jean Laherrère were discussing a Peak Oil impact scenario that went like this. Sometime around the year 2010, they theorized, stagnant or falling oil supplies would lead to soaring and more volatile petroleum prices, which would precipitate a global economic crash. This rapid economic contraction would in turn lead to sharply curtailed energy demand, so oil prices would then fall; but as soon as the economy regained strength, demand for oil would recover, prices would again soar, and as a result of that the economy would relapse. This cycle would continue, with each recovery phase being shorter and weaker, and each crash deeper and harder, until the economy was in ruins. Financial systems based on the assumption of continued growth would implode, causing more social havoc than the oil price spikes would themselves generate.

Meanwhile, volatile oil prices would frustrate investments in energy alternatives: one year, oil would be so expensive that almost any other energy source would look cheap by comparison; the next year, the price of oil would have fallen far enough that energy users would be flocking back to it, with investments in other energy sources looking foolish. But low oil prices would discourage exploration for more petroleum, leading to even worse fuel shortages later on. Investment capital would be in short supply in any case because the banks would be insolvent due to the crash, and governments would be broke due to declining tax revenues. Meanwhile, international competition for dwindling oil supplies might lead to wars between petroleum importing nations, between importers and exporters, and between rival factions within exporting nations.

But what happened next riveted the world’s attention to such a degree that the oil price spike was all but forgotten: in September 2008, the global financial system nearly collapsed. The reasons for this sudden, gripping crisis apparently had to do with housing bubbles, lack of proper regulation of the banking industry, and the over-use of bizarre financial products that almost nobody understood. However, the oil price spike had played a critical (if largely overlooked) role in initiating the economic meltdown

In the immediate aftermath of that global financial near-death experience, both the Peak Oil impact scenario proposed a decade earlier and the Limits to Growth standard-run scenario of 1972 seemed to be confirmed with uncanny and frightening accuracy. Global trade was falling. The world’s largest auto companies were on life support. The U.S. airline industry had shrunk by almost a quarter. Food riots were erupting in poor nations around the world. Lingering wars in Iraq (the nation with the world’s second-largest crude oil reserves) and Afghanistan (the site of disputed oil and gas pipeline projects) continued to bleed the coffers of the world’s foremost oil-importing nation.

Meanwhile, the debate about what to do to rein in global climate change exemplified the political inertia that had kept the world on track for calamity since the early ’70s. It had by now become obvious to nearly every person of modest education and intellect that the world has two urgent, incontrovertible reasons to rapidly end its reliance on fossil fuels: the twin threats of climate catastrophe and impending constraints to fuel supplies. Yet at the Copenhagen climate conference in December, 2009, the priorities of the most fuel-dependent nations were clear: carbon emissions should be cut, and fossil fuel dependency reduced, but only if doing so does not threaten economic growth.

We must convince ourselves that life in a non-growing economy can be fulfilling, interesting, and secure. The absence of growth does not necessarily imply a lack of change or improvement. Within a non-growing or equilibrium economy there can still be continuous development of practical skills, artistic expression, and certain kinds of technology. In fact, some historians and social scientists argue that life in an equilibrium economy can be superior to life in a fast-growing economy: while growth creates opportunities for some, it also typically intensifies competition—there are big winners and big losers, and (as in most boom towns) the quality of relations within the community can suffer as a result. Within a non-growing economy it is possible to maximize benefits and reduce factors leading to decay, but doing so will require pursuing appropriate goals: instead of more, we must strive for better; rather than promoting increased economic activity for its own sake, we must emphasize whatever increases quality of life without stoking consumption. One way to do this is to reinvent and redefine growth itself.

 “Classical” economic philosophers such as Adam Smith (1723–1790), Thomas Robert Malthus (1766–1834), and David Ricardo (1772–1823) introduced basic concepts such as supply and demand, division of labor, and the balance of international trade.

These pioneers set out to discover natural laws in the day-to-day workings of economies. They were striving, that is, to make of economics a science admired the ability of physicists, biologists, and astronomers to demonstrate the fallacy of old church doctrines, and to establish new universal “laws” by means of inquiry and experiment.

Economic philosophers, for their part, could point to price as arbiter of supply and demand, acting everywhere to allocate resources far more effectively than any human manager or bureaucrat could ever possibly do—surely this was a principle as universal and impersonal as the force of gravitation!

The classical theorists gradually adopted the math and some of the terminology of science. Unfortunately, however, they were unable to incorporate into economics the basic

Economic theory required no falsifiable hypotheses and demanded no repeatable controlled experiments. Economists began to think of themselves as scientists, while in fact their discipline remained a branch of moral philosophy—as it largely does to this day.

Importantly, these early philosophers had some inkling of natural limits and anticipated an eventual end to economic growth. The essential ingredients of the economy were understood to consist of labor, land, and capital. There was on Earth only so much land (which in these theorists’ minds stood for all natural resources), so of course at some point the expansion of the economy would cease. Both Malthus and Smith explicitly held this view. A somewhat later economic philosopher, John Stuart Mill (1806-1873), put the matter as follows: “It must always have been seen, more or less distinctly, by political economists, that the increase in wealth is not boundless: that at the end of what they term the progressive state lies the stationary state…”

But starting with Adam Smith, the idea that continuous “improvement” in the human condition was possible came to be generally accepted.

A key to this transformation was the gradual deletion by economists of land from the theoretical primary ingredients of the economy (increasingly, only labor and capital really mattered—land having been demoted to a sub-category of capital). This was one of the refinements that turned classical economic theory into neoclassical economics; others included the theories of utility maximization and rational choice.

While this shift began in the 19th century, it reached its fruition in the 20th through the work of economists who explored models of imperfect competition, and theories of market forms and industrial organization, while emphasizing tools such as the marginal revenue curve (this is when economics came to be known as “the dismal science”—partly because its terminology was, perhaps intentionally, increasingly mind-numbing). Meanwhile, however, the most influential economist of the 19th century, a philosopher named Karl Marx, had thrown a metaphorical bomb through the window of the house that Adam Smith had built. In his most important book, Das Kapital, Marx proposed a name for the economic system that had evolved since the Middle Ages: capitalism. It was a system founded on capital. Many people assume that capital is simply another word for money, but that entirely misses the essential point: capital is wealth—money, land, buildings, or machinery—that has been set aside for production of more wealth. If you use your entire weekly paycheck for rent, groceries, and other necessities, you may have money but no capital. But even if you are deeply in debt, if you own stocks or bonds, or a computer that you use for a home-based business, you have capital. Capitalism, as Marx defined it, is a system in which productive wealth is privately owned. Communism (which Marx proposed as an alternative) is one in which productive wealth is owned by the community, or by the nation on behalf of the people. In any case, Marx said, capital tends to grow.  

Marx also wrote that capitalism is inherently unsustainable, in that when the workers become sufficiently impoverished by the capitalists, they will rise up and overthrow their bosses and establish a communist state (or, eventually, a stateless workers’ paradise). The ruthless capitalism of the 19th century resulted in booms and busts, and a great increase in inequality of wealth—and therefore an increase in social unrest. With the depression of 1893 and the crash of 1907, and finally the Great Depression of the 1930s, it appeared to many social commentators of the time that capitalism was indeed failing, and that Marx-inspired uprisings were inevitable; the Bolshevik revolt in 1917 served as a stark confirmation of those hopes or fears (depending on one’s point of view).

The next few decades saw a three-way contest between the Keynesian social liberals, the followers of Marx, and temporarily marginalized neoclassical or neoliberal economists who insisted that social reforms and Keynesian meddling by government with interest rates, spending, and borrowing merely impeded the ultimate efficiency of the free Market.

the fall of the Soviet Union at the end of the 1980s, Marxism ceased to have much of a credible voice in economics. Its virtual disappearance from the discussion created space for the rapid rise of the neoliberals, who for some time had been drawing energy from widespread reactions against the repression and inefficiencies of state-run economies. Margaret Thatcher and Ronald Reagan both relied heavily on advice from neoliberal economists of the Chicago School

One of the most influential libertarian, free-market economists of recent decades was Alan Greenspan (b. 1926), who, as U.S. Federal Reserve Chairman from 1987 to 2006, argued for privatization of state-owned enterprises and de-regulation of businesses—yet Greenspan nevertheless ran an activist Fed that expanded the nation’s money supply in ways and to degrees that neither Friedman or Hayek would have approved of. As

There is a saying now in Russia: Marx was wrong in everything he said about communism, but he was right in everything he wrote about capitalism. Since the 1980s, the nearly worldwide re-embrace of classical economic philosophy has predictably led to increasing inequalities of wealth within the U.S. and other nations, and to more frequent and severe economic bubbles and crashes. Which brings us to the global crisis that began in 2008. By this time all mainstream economists (Keynesians and neoliberals alike) had come to assume that perpetual growth is the rational and achievable goal of national economies. The discussion was only about how to maintain it—through government intervention or a laissez-faire approach that assumes the Market always knows best. But

It is clearly a challenge to the neoliberals, whose deregulatory policies were largely responsible for creating the housing bubble whose implosion is generally credited with stoking the crisis. But it is a conundrum also for the Keynesians, whose stimulus packages have failed in their aim of increasing employment and general economic activity. What we have, then, is a crisis not just of the economy, but also of economic theory and philosophy.

The ideological clash between Keynesians and neoliberals (represented to a certain degree in the escalating all-out warfare between the U.S. Democratic and Republican political parties) will no doubt continue and even intensify. But the ensuing heat of battle will yield little light if both philosophies conceal the same fundamental errors. One such error is of course the belief that economies can and should perpetually grow. But that error rests on another that is deeper and subtler. The subsuming of land within the category of capital by nearly all post-classical economists had amounted to a declaration that Nature is merely a subset of the human economy—an endless pile of resources to be transformed into wealth. It also meant that natural resources could always be substituted with some other form of capital—money or technology. The reality, of course, is that the human economy exists within, and entirely depends upon Nature, and many natural resources have no realistic substitutes. This fundamental logical and philosophical mistake, embedded at the very heart of modern mainstream economic philosophies, set society directly upon a course toward the current era of climate change and resource depletion, and its persistence makes conventional economic theories—of both Keynesian and neoliberal varieties—utterly incapable of dealing with the economic and environmental survival threats to civilization in the 21st century.

For help, we can look to the ecological and biophysical economists, whose ideas have been thoroughly marginalized by the high priests and gatekeepers of mainstream economics—and, spectacular growth of debt—in obvious and subtle forms—that has occurred during the past few decades. That phenomenon in turn must be seen in light of the business cycles that characterize economic activity in modern industrial societies, and the central banks that have been set up to manage them.

We’ve already noted how nations learned to support the fossil fuel-stoked growth of their physical economies by increasing their money supply via fractional reserve banking. As money was gradually (and finally completely) de-linked from physical substance (i.e., precious metals), the creation of money became tied to the making of loans by commercial banks.

This meant that the supply of money was entirely elastic—as much could be created as was needed, and the amount in circulation could contract as well as expand. And the growth of money was tied to the growth of debt. The system is dynamic and unstable, and this instability manifests in the business cycle. In the expansionary phase of the cycle, businesses see the future as rosy, and therefore take out loans to build more productive capacity and hire new workers. Because many businesses are doing this at the same time, the pool of available workers shrinks; so, to attract and keep the best workers, businesses have to raise wages. With wages rising, worker-consumers have more money in their pockets. Worker-consumers spend much of that money on products from the businesses that hire them, helping spread even more optimism about the future. Amid all this euphoria, worker-consumers go into debt based on the expectation that their wages will continue to grow, making it easy to repay loans. Businesses go into debt expanding their productive capacity. Real estate prices go up because of rising demand (former renters deciding they can now afford to buy), which means that houses are worth more as collateral if existing homeowners want to take out big loans to do some remodeling or to buy a new car. All of this borrowing and spending increases the money supply and the velocity of money. At some point, however, the overall mood of the country changes. Businesses have invested in as much productive capacity as they are likely to need for a while. They feel they have taken on as much debt as they can handle, and don’t feel the need to hire more employees. Upward pressure on wages ceases, and that helps dampen the general sense of optimism about the economy. Workers likewise become shy about taking on more debt, as they are unsure whether they will be able to make payments. Instead, they concentrate on paying off existing debts. With fewer loans being written, less new money is being created; meanwhile, as earlier loans are paid off, money effectively disappears from the system. The nation’s money supply contracts in a self-reinforcing spiral. But if people increase their savings during this downward segment of the cycle, they eventually will feel more secure and therefore more willing to begin spending again. Also, businesses will eventually have liquidated much of their surplus productive capacity and thereby reduced their debt burden. This sets the stage for the next expansion phase.

A bubble consists of trade in high volumes at prices that are considerably at odds with intrinsic values, but the word can also be used more broadly to refer to any instance of rapid expansion of currency or credit that’s not sustainable over the long run. Bubbles always end with a crash—a rapid, sharp decline in asset values.

The upsides and downsides of the business cycle are reflected in higher or lower levels of inflation. Inflation is often defined in terms of higher wages and prices, but (as the Austrian economists have persuasively argued) wage and price inflation is actually just the symptom of an increase in the money supply relative to the amounts of goods and services being traded, which in turn is typically the result of exuberant borrowing and spending. The downside of the business cycle, in the worst instance, can produce the opposite of inflation, or deflation. Deflation manifests as declining wages and prices, consequent upon a declining money supply relative to goods and services traded, due to a contraction of borrowing and spending.

As we have seen, bubbles are a phenomenon generally tied to speculative investing. But in a larger sense our entire economy has assumed the characteristics of a bubble—even a Ponzi scheme. That is because it has come to depend upon staggering and continually expanding amounts of debt: government and private debt; debt in the trillions, and tens of trillions, and hundreds of trillions of dollars; debt that, in aggregate, has grown by 500 percent since 1980; debt that has grown faster than economic output (measured in GDP) in all but one of the past 50 years; debt that can never be repaid; debt that represents claims on quantities of labor and resources that simply do not exist.

Looking at the problem close up, the globalization of the economy looms as a prominent factor. In the 1970s and ’80s, with stiffer environmental and labor standards to contend with domestically, corporations began eyeing the regulatory vacuum, cheap labor, and relatively untouched natural resource base of less-industrialized nations as a potential goldmine. International investment banks started loaning poor nations enormous sums to pay for ill-advised infrastructure projects (and, incidentally, to pay kickbacks to corrupt local politicians), later requiring these countries to liquidate their natural resources at fire-sale prices so as to come up with the cash required to make loan payments. Then, prodded by corporate interests, industrialized nations pressed for the liberalization of trade rules via the World Trade Organization (the new rules almost always subtly favored the wealthier trading partner).

All of this led predictably to a reduction of manufacturing and resource extraction in core industrial nations, especially the U.S. (many important resources were becoming depleted in the wealthy industrial nations anyway), and a steep increase in resource extraction and manufacturing in several “developing” nations, principally China. Reductions in domestic manufacturing and resource extraction in turn motivated investors within industrial nations to seek profits through purely financial means. As a result of these trends, there are now as many Americans employed in manufacturing as there were in 1940, when the nation’s population was roughly half what it is today—while the proportion of total U.S. economic activity deriving from financial services has tripled during the same period. And speculative investing has become an accepted practice that is taught in top universities and institutionalized in the world’s largest corporations.

The most important financial development during the 1970s was the growth of securitization—a financial practice of pooling various types of contractual debt (such as residential mortgages, commercial mortgages, auto loans, or credit card debt obligations) and selling it to investors in the form of bonds, pass-through securities, or collateralized mortgage obligations (CMOs). The principal and interest on the debts underlying the security are paid back to investors regularly. Securitization provided an avenue for more investors to fund more debt. In effect, securitization caused (or allowed) claims on wealth to increase far above previous levels.

In 1970 the top 100 CEOs earned about $45 for every dollar earned by the average worker; by 2008 the ratio was over 1,000 to one.

In the 1990s, as the surplus of financial capital continued to grow, investment banks began inventing a slew of new securities with high yields. In assessing these new products, rating agencies used mathematical models that, in retrospect, seriously underestimated their levels of risk. Until the early 1970s, bond credit ratings agencies had been paid for their work by investors who wanted impartial information on the credit worthiness of securities issuers and their various offerings. Starting in the early 1970s, the “Big Three” ratings agencies (Standard & Poors, Moody’s, and Fitch) were paid instead by the securities issuers for whom they issued those ratings. This eventually led to ratings agencies actively encouraging the issuance of collateralized debt obligations (CDOs).   The Clinton administration adopted “affordable housing” as one of its explicit goals (this didn’t mean lowering house prices; it meant helping Americans get into debt), and over the decade the percentage of Americans owning their homes increased 7.8 percent. This initiated a persistent upward trend in real estate prices.

In the late 1990s investors piled into Internet-related stocks, creating a speculative bubble. The dot-com bubble burst in 2000 (as with all bubbles, it was only a matter of “when,” not “if”), and a year later the terrifying crimes of September 11, 2001 resulted in a four-day closure of U.S. stock exchanges and history’s largest one-day decline in the Dow Jones Industrial Average. These events together triggered a significant recession. Seeking to counter a deflationary trend, the Federal Reserve lowered its federal funds rate target from 6.5 percent to 1.0 percent, making borrowing more affordable.   Downward pressure on interest rates was also coming from the nation’s high and rising trade deficit. Every nation’s balance of payments must sum to zero, so if a nation is running a current account deficit it must balance that amount by earning from foreign investments, by running down reserves, or by obtaining loans from other countries. In other words, a country that imports more than it exports must borrow to pay for those imports. Hence American imports had to be offset by large and growing amounts of foreign investment capital flowing into the U.S. Higher bond prices attract more investment capital, but there is an inevitable inverse relationship between bond prices and interest rates, so trade deficits tend to force interest rates down.   Foreign investors had plenty of funds to lend, either because they had very high personal savings rates (in China, up to 40 percent of income saved), or because of high oil prices (think OPEC). A torrent of funds—it’s been called a “Giant Pool of Money” that roughly doubled in size from 2000 to 2007, reaching $70 trillion—was flowing into the U.S. financial markets. While foreign governments were purchasing U.S. Treasury bonds, thus avoiding much of the impact of the eventual crash, other foreign investors, including pension funds,

By this time a largely unregulated “shadow banking system,” made up of hedge funds, money market funds, investment banks, pension funds, and other lightly-regulated entities, had become critical to the credit markets and was underpinning the financial system as a whole. But the shadow “banks” tended to borrow short-term in liquid markets to purchase long-term, illiquid, and risky assets, profiting on the difference between lower short-term rates and higher long-term rates. This meant that any disruption in credit markets would result in rapid deleveraging, forcing these entities to sell long-term assets (such as MBSs) at depressed prices.

Between 1997 and 2006, the price of the typical American house increased by 124%.

People bragged that their houses were earning more than they were, believing that the bloating of house values represented a flow of real money that could be tapped essentially forever. In a sense this money was being stolen from the next generation: younger first-time buyers had to burden themselves with unmanageable debt in order to enter the market, while older homeowners who bought before the bubble were able to sell, downsize, and live on the profit.

For a brief time between 2006 and mid-2008, investors fled toward futures contracts in oil, metals, and food, driving up commodities prices worldwide. Food riots erupted in many poor nations, where the cost of wheat and rice doubled or tripled. In part, the boom was based on a fundamental economic trend: demand for commodities was growing—due in part to the expansion of economies in China, India, and Brazil—while supply growth was lagging. But speculation forced prices higher and faster than physical shortage could account for. For Western economies, soaring oil prices had a sharp recessionary impact, with already cash-strapped new homeowners now having to spend eighty to a hundred dollars every time they filled the tank in their SUV. The auto, airline, shipping, and trucking industries were sent reeling.

The U.S. real estate bubble of the early 2000s was the largest (in terms of the amount of capital involved) in history. And its crash carried an eerie echo of the 1930s: Austrian and Post-Keynesian economists have argued that it wasn’t the stock market crash that drove the Great Depression so much as farm failures making it impossible for farmers to make mortgage payments—along with housing bubbles in Florida, New York, and Chicago.

Real estate bubbles are essentially credit bubbles, because property owners generally use borrowed money to purchase property (this is in contrast to currency bubbles, in which nations inflate their currency to pay off government debt). The amount of outstanding debt soars as buyers flood the market, bidding property prices up to unrealistic levels and taking out loans they cannot repay. Too many houses and offices are built, and materials and labor are wasted in building them. Real estate bubbles also lead to an excess of homebuilders, who must retrain and retool when the bubble bursts. These kinds of bubbles lead to systemic crises affecting the economic integrity of nations.   Indeed, the housing bubble of the early 2000s had become the oxygen of the U.S. economy—the source of jobs, the foundation for Wall Street’s recovery from the dot-com bust, the attractant for foreign capital, the basis for household wealth accumulation and spending. Its bursting changed everything.  

And there is reason to think it has not fully deflated: commercial real estate may be waiting to exhale next. Over the next five years, about $1.4 trillion in commercial real estate loans will reach the end of their terms and require new financing. Commercial property values have fallen more than 40 percent nationally since their 2007 peak, so nearly half the loans are underwater. Vacancy rates are up and rents are down.   The impact of the real estate crisis on banks is profound, and goes far beyond defaults upon outstanding mortgage contracts: systemic dependence on MBSs, CDOs, and derivatives means many of the banks, including the largest, are effectively insolvent and unable to take on more risk (we’ll see why in more detail in the next section).   The demographics are not promising for a recovery of the housing market anytime soon: the oldest of the Baby Boomers are 65 and entering retirement. Few have substantial savings; many had hoped to fund their golden years with house equity—and to realize that, they must sell. This will add more houses to an already glutted market, driving prices down even further.  

With regard to debt, what are those limits likely to be and how close are we to hitting them?  There are practical limits to debt within such a system, and those limits are likely to show up in somewhat different ways for each of the four categories of debt indicated in the graph.   With government debt, problems arise when required interest payments become a substantial fraction of tax revenues. Currently for the U.S., the total Federal budget amounts to about $3.5 trillion, of which 12 percent (or $414 billion) goes toward interest payments. But in 2009, tax revenues amounted to only $2.1 trillion; thus interest payments currently consume almost 20 percent, or nearly one-fifth, of tax revenues.

By the time the debt reaches $20 trillion, roughly ten years from now, interest payments may constitute the largest Federal budget outlay category, eclipsing even military expenditures. If Federal tax revenues haven’t increased by that time, Federal government debt interest payments will be consuming 20 percent of them.

Once 100 percent of tax revenues have to go toward interest payments and all government operations have to be funded with more borrowing—on which still more interest will have to be paid—the system will have arrived at a kind of financial singularity: a black hole of debt, if you will. But in all likelihood we would not have to get to that ultimate impasse before serious problems appear.

Many economic wags suggest that when government has to spend 30 percent of tax receipts on interest payments, the country is in a debt trap from which there is no easy escape. Given current trajectories of government borrowing and interest rates, that 30 percent mark could be hit in just a few years. Even before then, U.S. credit worthiness and interest costs will take a beating.

However, some argue that limits to government debt (due to snowballing interest payments) need not be a hard constraint—especially for a large nation, like the U.S., that controls its own currency. The United States government is constitutionally empowered to create money, including creating money to pay the interest on its debts. Or, the government could in effect loan the money to itself via its central bank, which would then rebate interest payments back to the Treasury (this is in fact what the Treasury and Fed are doing with Quantitative Easing 2,

The most obvious complication that might arise is this: If at some point general confidence that external U.S. government debt (i.e., money owed to private borrowers or other nations) could be repaid with debt of equal “value” were deeply and widely shaken, potential buyers of that debt might decide to keep their money under the metaphorical mattress (using it to buy factories or oilfields instead), even if doing so posed its own set of problems. Then the Fed would become virtually the only available buyer of government debt, which might eventually undermine confidence in the currency, possibly igniting a rapid spiral of refusal that would end only when the currency failed. There are plenty of historic examples of currency failures, so this would not be a unique occurrence.

But as long as deficit spending doesn’t exceed certain bounds, and as long as the economy resumes growth in the not-too-distant future, then it can be sustained for quite some time. Ponzi schemes theoretically can continue forever—if the number of potential participants is infinite. The absolute size of government debt is not necessarily a critical factor, as long as future growth will be sufficient so that the proportion of debt relative to revenues remains the same. Even an increase in that proportion is not necessarily cause for alarm, as long as it is only temporary. This, at any rate, is the Keynesian argument. Keynesians would also point out that government debt is only one category of total debt, and that U.S. government debt hasn’t grown proportionally relative to other categories of debt to any alarming degree (until the current recession).

Baby Boomers (the most numerous demographic cohort in the nation’s history, encompassing 70 million Americans) are reaching retirement age, which means that their lifetime spending cycle has peaked. It’s not that Boomers won’t continue to buy things (everybody has to eat), but their aggregate spending is unlikely to increase, given that cohort members’ savings are, on average, inadequate for retirement (one-third of them have no savings whatever). Out of necessity, Boomers will be saving more from now on, and spending less. And that won’t help the economy grow.  

When demand for products declines, corporations aren’t inclined to borrow to increase their productive capacity. Even corporate borrowing aimed at increasing financial leverage has limits. Too much corporate debt reduces resiliency during slow periods—and the future is looking slow for as far as the eye can see. Durable goods orders are down, housing starts and new home sales are down, savings are up. As a result, banks don’t want to lend to companies, because the risk of default on such loans is now perceived as being higher than it was a few years ago; in addition, the banks are reluctant to take on more risk of any sort given the fact that many of the assets on their balance sheets consist of now-worthless derivatives and CDOs.   Meanwhile, ironically and perhaps surprisingly, U.S. corporations are sitting on over a trillion dollars because they cannot identify profitable investment opportunities and because they want to hang onto whatever cash they have in anticipation of continued hard times.   If only we could get to the next upside business cycle, then more corporate debt would be justified for both lenders and borrowers. But so far confidence in the future is still weak.

One of the main reforms enacted during the Great Depression, contained in the Glass Steagall Act of 1933, was a requirement that commercial banks refrain from acting as investment banks. In other words, they were prohibited from dealing in stocks, bonds, and derivatives. This prohibition was based on an implicit understanding that there should be some sort of firewall within the financial system separating productive investment from pure speculation, or gambling. This firewall was eliminated by the passage of the Gramm–Leach–Bliley Act of 1999 (for which the financial services industry lobbied tirelessly). As a result, all large U.S. banks have for the past decade become deeply engaged in speculative investment, using both their own and their clients’ money.   With derivatives, since there is no requirement to own the underlying asset, and since there is often no requirement of evidence of ability to cover the bet, there is no effective limit to the amount that can be wagered. It’s true that many derivatives largely cancel each other out, and that their ostensible purpose is to reduce financial risk. Nevertheless, if a contract is settled, somebody has to pay—unless they can’t.

In the heady years of the 2000s, even the largest and most prestigious banks engaged in what can only be termed criminally fraudulent behavior on a massive scale. As revealed in sworn Congressional testimony, firms including Goldman Sachs deliberately created flawed securities and sold tens of billions of dollars’ worth of them to investors, then took out many more billions of dollars’ worth of derivatives contracts essentially betting against the securities they themselves had designed and sold. They were quite simply defrauding their customers, which included foreign and domestic pension funds. To date, no senior executive with any bank or financial services firm has been prosecuted for running these scams. Instead, most of the key figures are continuing to amass immense personal fortunes, confident no doubt that what they were doing—and in many cases continue to do—is merely a natural extension of the inherent logic of their industry.   The degree and concentration of exposure on the part of the biggest banks with regard to derivatives was and is remarkable: as of 2005, JP Morgan Chase, Bank of America, Citibank, Wachovia, and HSBC together accounted for 96 percent of the $100 trillion of derivatives contracts held by 836 U.S. banks.

Even though many derivatives were insurance against default, or wagers that a particular company would fail, to a large degree they constituted a giant bet that the economy as a whole would continue to grow (and, more specifically, that the value of real estate would continue to climb). So when the economy stopped growing, and the real estate bubble began to deflate, this triggered a systemic unraveling that could be halted (and only temporarily) by massive government intervention.  

Suddenly “assets” in the form of derivative contracts that had a stated value on banks’ ledgers were clearly worth much less. If these assets had to be sold, or if they were “marked to market” (valued on the books at the amount they could actually sell for), the banks would be shown to be insolvent. Government bailouts essentially enabled the banks to keep those assets hidden, so that banks could appear solvent and continue carrying on business.   Despite the proliferation of derivatives, the financial system still largely revolves around the timeworn practice of receiving deposits and making loans. Bank loans are the source of money in our modern economy. If the banks go away, so does the rest of the economy.

But as we have just seen, many banks are probably actually insolvent because of the many near-worthless derivative contracts and bad mortgage loans they count as assets on their balance sheets.   One might well ask: If commercial banks have the power to create money, why can’t they just write off these bad assets and carry on? Ellen Brown explains the point succinctly in her useful book Web of Debt: [U]nder the accountancy rules of commercial banks, all banks are obliged to balance their books, making their assets equal their liabilities. They can create all the money they can find borrowers for, but if the money isn’t paid back, the banks have to record a loss; and when they cancel or write off debt, their assets fall. To balance their books . . . they have to take the money either from profits or from funds invested by the bank’s owners [i.e., shareholders]; and if the loss is more than its owners can profitably sustain, the bank will have to close its doors.

So, given their exposure via derivatives, bad real estate loans, and MBSs, the banks aren’t making new loans because they can’t take on more risk. The only way to reduce that risk is for government to guarantee the loans. Again, as long as the down-side of this business cycle is short, such a plan could work in principle.   But whether it actually will in the current situation is problematic. As noted above, Ponzi schemes can theoretically go on forever, as long as the number of new investors is infinite. Yet in the real world the number of potential investors is always finite. There are limits. And when those limits are hit, Ponzi schemes can unravel very quickly.

The shadow banks can still write more derivative contracts, but that doesn’t do anything to help the real economy and just spreads risk throughout the system. That leaves government, which (if it controls its own currency and can fend off attacks from speculators) can continue to run large deficits, and the central banks, which can enable those deficits by purchasing government debt outright—but unless such efforts succeed in jump-starting growth in the other sectors, that is just a temporary end-game strategy.

Remember: in a system in which money is created through bank loans, there is never enough money in existence to pay back all debts with interest. The system only continues to function as long as it is growing.   So, what happens to this mountain of debt in the absence of economic growth? Answer: Some kind of debt crisis. And that is what we are seeing.   Debt crises have occurred frequently throughout the history of civilizations, beginning long before the invention of fractional reserve banking and credit cards. Many societies learned to solve the problem with a “debt jubilee”: According to the Book of Leviticus in the Bible, every fiftieth year is a Jubilee Year, in which slaves and prisoners are to be freed and debts are to be forgiven.

For householders facing unaffordable mortgage payments or a punishing level of credit card debt, a jubilee may sound like a capitol idea. But what would that actually mean today, if carried out on a massive scale—when debt has become the very fabric of the economy? Remember: we have created an economic machine that needs debt like a car needs gas.   Realistically, we are unlikely to see a general debt jubilee in coming years; what we will see instead are defaults and bankruptcies that accomplish essentially the same thing—the destruction of debt. Which, in an economy like ours, effectively means a destruction of wealth and claims upon wealth. Debt will have to be written off in enormous amounts—by the trillions of dollars. Over the short term, government will attempt to stanch this flood of debt-shedding in the household, corporate, and financial sectors by taking on more debt of its own—but eventually it simply won’t be able to keep up, given the inherent limits on government borrowing discussed above.   We began with the question, “How close are we to hitting the limits to debt?” The evident answer is: we have already probably hit realistic limits to household debt and corporate debt; the ratio of U.S. total debt-to-GDP is probably near or past the danger mark; and limits to government debt may be within sight, though that conclusion is more controversial and doubtful.  

For the U.S., actions undertaken by the Federal government and the Federal Reserve bank system have so far resulted in totals of $3 trillion actually spent and $11 trillion committed as guarantees. Some of these actions are discussed below; for a complete tally of the expenditures and commitments, see the online CNN Bailout Tracker.

The New Deal had cost somewhere between $450 and $500 billion and had increased government’s share of the national economy from 4 percent to 10 percent. ARRA represented a much larger outlay that was spent over a much shorter period, and increased government’s share of the economy from 20 percent to 25 percent.

At the end of 2010, President Obama and congressional leaders negotiated a compromise package of extended and new tax cuts that, in total, would reduce potential government revenues by an estimated $858 billion. This was, in effect, a third stimulus package.

Critics of the stimulus packages argued that transitory benefits to the economy had been purchased by raising government debt to frightening levels. Proponents of the packages answered that, had government not acted so boldly, an economic crisis might have turned into complete and utter ruin.

While the U.S. government stimulus packages were enormous in scale, the actions of the Federal Reserve dwarfed them in terms of dollar amounts committed.   During the past three years, the Fed’s balance sheet has swollen to more than $2 trillion through its buying of bank and government debt. Actual expenditures included $29 billion for the Bear Sterns bailout; $149.7 billion to buy debt from Fannie Mae and Freddie Mac; $775.6 billion to buy mortgage-backed securities, also from Fannie and Freddie; and $109.5 billion to buy hard-to-sell assets (including (MBSs) from banks. However, the Fed committed itself to trillions more in insuring banks against losses, loaning to money market funds, and loaning to banks to purchase commercial paper. Altogether, these outlays and commitments totaled a minimum of $6.4 trillion.

Documents released by the Fed on December 1, 2010 showed that more than $9 trillion in total had been supplied to Wall Street firms, commercial banks, foreign banks, and corporations, with Citigroup, Morgan Stanley, and Merrill Lynch borrowing sums that cumulatively totaled over $6 trillion. The collateral for these loans was undisclosed but widely thought to be stocks, CDSs, CDOs, and other securities of dubious value.   In one of its most significant and controversial programs, known as “quantitative easing,” the Fed twice expanded its balance sheet substantially, first by buying mortgage-backed securities from banks, then by purchasing outstanding Federal government debt (bonds and Treasury certificates) to support the Treasury debt market and help keep interest rates down on consumer loans. The Fed essentially creates money on the spot for this purpose (though no money is literally “printed”), thus monetizing U.S. government debt.  

In November 2008 China announced a stimulus package totaling 4 trillion yuan ($586 billion) as an attempt to minimize the impact of the global financial crisis on its domestic economy. In proportion to the size of China’s economy, this was a much larger stimulus package than that of the U.S. Public infrastructure development made up the largest portion, nearly 38 percent, followed by earthquake reconstruction, funding for social welfare plans, rural development, and technology advancement programs.

What’s the bottom line on all these stimulus and bailout efforts? In the U.S., $12 trillion of total household net worth disappeared in 2008, and there will likely be more losses ahead, largely as a result of continued fall in real estate values though increasingly as a result of job losses as well. The government’s stimulus efforts, totaling less than $1 trillion, cannot hope to make up for this historic evaporation of wealth. While indirect subsidies may temporarily keep home prices from falling further, that just keeps houses less affordable to workers making less income. Meanwhile, the bailouts of banks and shadow banks have been characterized as government throwing money at financial problems it cannot solve, rewarding the very people who created them. Rather than being motivated by the suffering of American homeowners or governments in over their heads, the bailouts of Fannie Mae and Freddie Mac in the U.S., and Greece and Ireland in the E.U. were (according to critics) essentially geared toward securing the investments of the banks and the wealthy bonds holders.

The stimulus-bailout efforts of 2008-2009—which in the U.S. cut interest rates from 5 percent to zero, spent up the budget deficit to 10 percent of GDP, and guaranteed $6.4 trillion to shore up the financial system—arguably cannot be repeated. These constituted quite simply the largest commitments of funds in world history, dwarfing the total amounts spent in all the wars of the 20th century in inflation-adjusted terms (for the U.S., the cost of World War II amounted to $3.2 trillion). Not only the U.S., but Japan and the European nations as well have exhausted their arsenals.   But more will be needed as countries, states, counties, and cities near bankruptcy due to declining tax revenues. Meanwhile the U.S. has lost 8.4 million jobs—and if loss of hours worked is considered that adds the equivalent of another 3 million; the nation will need to generate an extra 450,000 jobs each month for three years to get back to pre-crisis levels of employment. The only way these problems can be allayed (not fixed) is through more central bank money creation and government spending.

Once a credit bubble has inflated, the eventual correction (which entails destruction of credit and assets) is of greater magnitude than government’s ability to spend. The cycle must sooner or later play itself out.   There may be a few more arrows in the quiver of economic policy makers: central bankers could try to drive down the value of domestic currencies to stimulate exports; the Fed could also engage in more quantitative easing. But these measures will sooner or later merely undermine currencies

Further, the way the Fed at first employed quantitative easing in 2009 was minimally productive.

QE1 amounted to adding about a trillion dollars to banks’ balance sheets, with the assumption that banks would then use this money as a basis for making loans.[2] The “multiplier effect” (in which banks make loans in amounts many times the size of deposits) should theoretically have resulted in the creation of roughly $9 trillion within the economy. However, this did not happen: because there was reduced demand for loans (companies didn’t want to expand in a recession and families didn’t want to take on more debt), the banks just sat on this extra capital. A better result could arguably have been obtained if the Fed were somehow to have distributed the same amount of money directly to debtors, rather than to banks, because then at least the money would either have circulated to pay for necessities, or helped to reduce the general debt overhang.

QE2 was about funding Federal government debt interest-free. Because the Federal Reserve rebates its profits (after deducting expenses) to the Treasury, creating money to buy government debt obligations is an effective way of increasing that debt without increasing interest payments. Critics describe this as the government “printing money” and assert that it is highly inflationary; however, given the extremely deflationary context (trillions of dollars’ worth of write-downs in collateral and credit), the Fed would have to “print” far more than it is doing to result in real inflation. Nevertheless, as we will see in Chapter 5 in a discussion of “currency wars,” other nations view this strategy as a way to drive down the dollar so as to decrease the value of foreign-held dollar-denominated debt—in effect forcing them to pay for America’s financial folly.

Central banks and governments are barely keeping the wheels on society, but their actions come with severe long-term costs and risks. And what they can actually accomplish is most likely limited anyway.

Deflation represents a disappearance of credit and money, so that whatever money remains has increased purchasing power. Once the bubble began to burst back in 2007-2008, say the deflationists, a process of contraction began that inevitably must continue to the point where debt service is manageable and prices for assets such as homes and stocks are compelling based on long-term historical trends.   However, many deflationists tend to agree that the inflationists are probably right in the long run: at some point, perhaps several years from now, some future U.S. administration will resort to truly extraordinary means to avoid defaulting on interest payments on its ballooning debt, as well as to avert social disintegration and restart economic activity. There are several scenarios by which this might happen—including government simply printing money in enormous quantities and distributing it directly to banks or citizens. The net effect would be the same in all cases: a currency collapse.

In general, what we are actually seeing so far is neither dramatic deflation nor hyperinflation. Despite the evaporation of trillions of dollars in wealth during the past four years, and despite government and central bank interventions with a potential nameplate value also running in the trillions of dollars, prices (which most economists regard as the signal of inflation or deflation) have remained fairly stable. That is not to say that the economy is doing well: the ongoing problems of unemployment, declining tax revenues, and business and bank failures are obvious to everyone. Rather, what seems to be happening is that the efforts of the U.S. Federal government and the Federal Reserve have temporarily more or less succeeded in balancing out the otherwise massively deflationary impacts of defaults, bankruptcies, and falling property values. With its new functions, the Fed is acting as the commercial bank of last resort, transferring debt (mostly in the form of MBSs and Treasuries) from the private sector to the public sector.

The Fed’s zero-interest-rate policy has given a huge hidden subsidy to banks by allowing them to borrow Fed money for nothing and then lend it to the government at a 3 percent interest rate. But this is still not inflationary, because Federal Reserve is merely picking up the slack left by the collapse of credit in the private sector. In effect, the nation’s government and its central bank are together becoming the lender of last resort and the borrower of last resort—and (via the military) increasingly also both the consumer of last resort and the employer of last resort.

While leaders will make every effort to portray this as a gradual return to growth, in fact the economy will be losing ground and will remain fragile, highly vulnerable to upsetting events that could take any of a hundred forms—including international conflict, terrorism, the bankruptcy of a large corporation or megabank, a sovereign debt event (such as a default by one of the European countries now lined up for bailouts), a food crisis, an energy shortage or temporary grid failure, an environmental disaster, a curtailment of government-Fed intervention based on a political shift in the makeup of Congress, or a currency war

Extreme social unrest would be an inevitable result of the gross injustice of requiring a majority of the population to forego promised entitlements and economic relief following the bailout of a small super-wealthy minority on Wall Street. Political opportunists can be counted on to exacerbate that unrest and channel it in ways utterly at odds with society’s long-term best interests. This is a toxic brew

Growth requires not just energy in the most general sense, but forms of energy with specific characteristics. After all, the Earth is constantly bathed in energy—indeed, the amount of solar energy that falls on Earth’s surface each hour is greater than the amount of fossil-fuel energy the world uses every year. But sunlight energy is diffuse and difficult to use directly. Economies need sources of energy that are concentrated and controllable, and that can be made to do useful work. From a short-term point of view, fossil fuels proved to be energy sources with highly desirable characteristics: they could be extracted from Earth’s crust quite cheaply (at least in the early days), they were portable, and they delivered a lot of energy per unit of weight and/or volume—in most instances, far more than the firewood that people had been accustomed to using.

2009 Post Carbon Institute and the International Forum on Globalization undertook a joint study to analyze 18 energy sources (from oil to tidal power) using 10 criteria (scalability, renewability, energy density, energy returned on energy invested, and so on).

(Searching for a Miracle: Net Energy Limits and the Fate of Industrial Societies),

Our conclusion was that there is no credible scenario in which alternative energy sources can entirely make up for fossil fuels as the latter deplete.

Given oil’s pivotal role in the economy, high prices did more than reduce demand, they had helped undermine the economy as a whole in the 1970s and again in 2008. Economist James Hamilton of the University of California, San Diego, has assembled a collection of studies showing a tight correlation between oil price spikes and recessions during the past 50 years. Seeing this correlation, every attentive economist should have forecast a steep recession beginning in 2008, as oil price soared.

By mid-2009 the oil price had settled within the “Goldilocks” range—not too high (so as to kill the economy and, with it, fuel demand), and not too low (so as to scare away investment in future energy projects and thus reduce supply). That just-right price band appeared to be between $60 and $80 a barrel. How long prices can stay in or near the Goldilocks range is anyone’s guess but as declines in production in the world’s old super-giant oilfields continue to accelerate and exploration costs continue to mount, the lower boundary of that just-right range will inevitably continue to migrate upward. And while the world economy remains frail, its vulnerability to high energy prices is more pronounced, so that even $80-85 oil could gradually weaken it further, choking off signs of recovery.  In other words, oil prices have effectively put a cap on economic recovery. This problem would not exist if the petroleum industry could just get busy and make a lot more oil, so that each unit would be cheaper. But despite its habitual use of the terms “produce” and “production,” the industry doesn’t make oil, it merely extracts the stuff from finite stores in the Earth’s crust. As we have already seen, the cheap, easy oil is gone. Economic growth is hitting the Peak Oil ceiling.  

As more and more resources acquire the Goldilocks syndrome, general commodity prices will likely spike and crash repeatedly, making a hash of efforts to stabilize the economy.

There are three main solutions to the problem of Peak Phosphate: composting of human wastes, including urine diversion; more efficient application of fertilizer; and farming in such a way as to make existing soil phosphorus more accessible to plants.

It’s worth noting that for the past few decades a vocal minority of farmers, agricultural scientists, and food system theorists including Wendell Berry, Wes Jackson, Vandana Shiva, Robert Rodale, and Michael Pollan, has argued against centralization, industrialization, and globalization of agriculture, and for an ecological agriculture with minimal fossil fuel inputs. Where their ideas have taken root, the adaptation to Peak Oil and the end of growth will be easier. Unfortunately, their recommendations have not become mainstream, because industrialized, globalized agriculture has proved capable of producing larger short-term profits for banks and agribusiness cartels. Even more unfortunately, the available time for a large-scale, proactive food system transition before the impacts of Peak Oil and economic contraction arrive is gone. We’ve run out the clock.   In his book, Dirt, David Montgomery makes a powerful case that soil erosion was a major cause of the Roman economy’s decline.

Data from the U.S. Geological Survey shows that within the U.S. many mineral resources are well past their peak rates of production.[4] These include bauxite (whose production peaked in 1943), copper (1998), iron ore (1951), magnesium (1966), phosphate rock (1980), potash (1967), rare earth metals (1984), tin (1945), titanium (1964), and zinc (1969).[5]

There are 17 rare earth elements (REEs) with names like lanthanum, neodymium, europium, and yttrium. They are critical to a variety of high-tech products including catalytic converters, color TV and flat panel displays, permanent magnets, batteries for hybrid and electric vehicles, and medical devices; to manufacturing processes like petroleum refining; and to various defense systems like missiles, jet engines, and satellite components. REEs are even used in making the giant electromagnets in modern wind turbines. But rare earth mines are failing to keep up with demand. China produces 97 percent of the world’s REEs, and has issued a series of contradictory public statements about whether, and in what amounts, it intends to continue exporting these elements.

Indium is used in indium tin oxide, which is a thin-film conductor in flat-panel television screens. Armin Reller, a materials chemist, and his colleagues at the University of Augsburg in Germany have been investigating the problem of indium depletion. Reller estimates that the world has, at best, 10 years before production begins to decline; known deposits will be exhausted by 2028, so new deposits will have to be found and developed. Some analysts are now suggesting that shortages of energy minerals including indium, REEs, and lithium for electric car batteries could trigger trade wars. 

Armin Reller and his colleagues have also looked into gallium supplies. Discovered in 1831, Gallium is a blue-white metal with certain unusual properties, including a very low melting point and an unwillingness to oxidize. These make it useful as a coating for optical mirrors, a liquid seal in strongly heated apparatus, and a substitute for mercury in ultraviolet lamps. Gallium is also essential to making liquid-crystal displays in cell phones, flat-screen televisions, and computer monitors. With the explosive profusion of LCD displays in the past decade, supplies of gallium have become critical; Reller projects that by about 2017 existing sources will be exhausted. 

Palladium (along with platinum and rhodium) is a primary component in the autocatalysts used in automobiles to reduce exhaust emissions. Palladium is also employed in the production of multi-layer ceramic capacitors in cellular telephones, personal and notebook computers, fax machines, and auto and home electronics. Russian stockpiles have been a key component in world palladium supply for years, but those stockpiles are nearing exhaustion, and prices for the metal have soared as a result.

Uranium is the fuel for nuclear power plants and is also used in nuclear weapons manufacturing; small amounts are employed in the leather and wood industries for stains and dyes, and as mordants of silk or wool. Depleted uranium is used in kinetic energy penetrator weapons and armor plating. In 2006, the Energy Watch Group of Germany studied world uranium supplies and issued a report concluding that, in its most optimistic scenario, the peak of world uranium production will be achieved before 2040. If large numbers of new nuclear power plants are constructed to offset the use of coal as an electricity source, then supplies will peak much sooner. Tantalum for cell phones. Helium for blimps. The list could go on. Perhaps it is not too much of an exaggeration to say that humanity is in the process of achieving Peak Everything.

Accidents and natural disasters have long histories; therefore it may seem peculiar at first to think that these could now suddenly become significant factors in choking off economic growth. However, two things have changed.   First, growth in human population and proliferation of urban infrastructure are leading to ever more serious impacts from natural and human-caused disasters.

There are also limits to the environment’s ability to absorb the insults and waste products of civilization, and we are broaching those limits in ways that can produce impacts of a scale far beyond our ability to contain or mitigate. The billions of tons of carbon dioxide that our species has released into the atmosphere through the combustion of fossil fuels are not only changing the global climate but also causing the oceans to acidify. Indeed, the scale of our collective impact on the planet has grown to such an extent that many scientists contend that Earth has entered a new geologic era—the Anthropocene. Humanly generated threats to the environment’s ability to support civilization are now capable of overwhelming civilization’s ability to adapt and regroup.

GDP impacts from the 2010 disasters were substantial. BP’s losses from the Deepwater Horizon gusher (which included cleanup costs and compensation to commercial fishers) have so far amounted to about $40 billion. The Pakistan floods caused damage estimated at $43 billion, while the financial toll of the Russian wildfires has been pegged at $15 billion.[4] Add in other events listed above, plus more not mentioned, and the total easily tops $150 billion for GDP losses in 2010 resulting from natural disasters and industrial accidents.[5] This does not include costs from ongoing environmental degradation (erosion of topsoil, loss of forests and fish species). How does this figure compare with annual GDP growth? Assuming world annual GDP of $58 trillion and an annual growth rate of three percent, annual GDP growth would amount to $1.74 trillion. Therefore natural disasters and industrial accidents, conservatively estimated, are already costing the equivalent of 8.6 percent of annual GDP growth.   As resource extraction moves from higher-quality to lower-quality ores and deposits, we must expect worse environmental impacts and accidents along the way. There are several current or planned extraction projects in remote and/or environmentally sensitive regions that could each result in severe global impacts equaling or even surpassing the Deepwater Horizon blowout. These include oil drilling in the Beaufort and Chukchi Seas; oil drilling in the Arctic National Wildlife Refuge; coal mining in the Utukok River Upland, Arctic Alaska; tar sands production in Alberta; shale oil production in the Rocky Mountains; and mountaintop-removal coal mining in Appalachia.

Since climate is changing mostly because of the burning of fossil fuels, averting climate change is largely a matter of reducing fossil fuel consumption.[9] But as we have seen (and will confirm in more ways in the next chapter), economic growth depends on increasing energy consumption. Due to the inherent characteristics of alternative energy sources, it is extremely unlikely that society can increase its energy production while dramatically curtailing fossil fuel use.

Anther environmental impact that is relatively slow and ongoing and even more difficult to put a price tag on is the decline in the number of other species inhabiting our planet. According to one recent study, one in five plant species faces extinction as a result of climate change, deforestation, and urban growth.

Non-human species perform ecosystem services that only indirectly benefit our kind, but in ways that turn out to be crucial. Phytoplankton, for example, are not a direct food source for people, but comprise the base of oceanic food chains—in addition to supplying half of the oxygen produced each year by nature. The abundance of plankton in the world’s oceans has declined 40 percent since 1950, according to a recent study, for reasons not entirely clear. This is one of the main explanations for a gradual decline in atmospheric oxygen levels recorded worldwide.  A 2010 study by Pavan Sukhdev, a former banker, to determine a price for the world’s environmental assets, concluded that the annual destruction of rainforests entails an ultimate cost to society of $4.5 trillion—$650 for each person on the planet. But that cost is not paid all at once; in fact, over the short term, forest cutting looks like an economic benefit as a result of the freeing up of agricultural land and the production of timber. Like financial debt, environmental costs tend to accumulate until a crisis occurs and systems collapse.

Declining oxygen levels, acidifying oceans, disappearing species, threatened oceanic food chains, changing climate—when considering planetary changes of this magnitude, it may seem that the end of economic growth is hardly the worst of humanity’s current problems. However, it is important to remember that we are counting on growth to enable us to solve or respond to environmental crises. With economic growth, we have surplus money with which to protect rainforests, save endangered species, and clean up after industrial accidents. Without economic growth, we are increasingly defenseless against environmental disasters—many of which paradoxically result from growth itself.

Talk of limits typically elicits dismissive references to the failed warnings of Thomas Malthus—the 18th century economist who reasoned that population growth would inevitably (and soon) outpace food production, leading to a general famine. Malthus was obviously wrong, at least in the short run: food production expanded throughout the 19th and 20th centuries to feed a fast-growing population. He failed to foresee the introduction of new hybrid crop varieties, chemical fertilizers, and the development of industrial farm machinery. The implication, whenever Malthus’s ghost is summoned, is that all claims that environmental limits will overtake growth are likewise wrong, and for similar reasons. New inventions and greater efficiency will always trump looming limits.

The main advantages of electrics are that their energy is used more efficiently (electric motors translate nearly all their energy into motive force, while internal combustion engines are much less efficient), they need less drive-train maintenance, and they are more environmentally benign (even if they’re running on coal-derived electricity, they usually entail lower carbon emissions due to their much higher energy efficiency). The drawbacks of electric vehicles have to do with the limited ability of batteries to store energy, as compared to conventional liquid fuels. Gasoline carries 45 megajoules per kilogram, while lithium-ion batteries can store only 0.5 MJ/kg. Improvements are possible, but the theoretical limit of chemical energy storage is still only about 3 MJ/kg. This is why we’ll never see battery-powered airliners: the batteries would be way too heavy to allow planes to get off the ground.

The low energy density (by weight) of batteries tends to limit the range of electric cars. This problem can be solved with hybrid power trains—using a gasoline engine to charge the batteries, as in the Chevy Volt, or to push the car directly part of the time, as with the Toyota Prius—but that adds complexity and expense.  

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