Energy's Water Demand:
Trends, Vulnerabilities, and Management

January 5, 2011 (R41507)

Contents

Figures

Tables

Appendixes

Summary

The energy choices before Congress represent vastly different demands on domestic freshwater because water is used in varying amounts in most aspects of the energy sector. Transitions in the energy sector, such as the pursuit of greater energy independence and security, produce changes in how much and where the energy sector uses water. The energy sector is the fastest-growing water consumer in the United States, in part because of energy policies. Whether the federal government addresses the energy sector's rising water demand, and if so how, is one of the many energy decisions that may be considered by the 112th Congress.

Much of the growth in the energy sector's water demand is concentrated in regions with already intense competition over water. Whether the energy sector exacerbates or alleviates future water tensions is influenced by near-term energy policy and investment decisions. These decisions also may determine whether water will limit or harm U.S. capability to reliably meet the nation's energy demand. Part of the policy issue for Congress is identifying the extent of the federal role in responding to the energy sector's water use. Currently, the energy industry and states have the most responsibility for managing and meeting the energy sector's water demand.

The energy sector's water consumption is projected to rise 50% from 2005 to 2030. Projections attribute to the energy sector 85% of the growth in domestic water consumption between 2005 and 2030. The drivers of the energy sector's increasing water use are rising energy demand, greater development of domestic energy, and shifts to more water-intense energy sources and technologies. The more water used by the energy sector, the more vulnerable the energy system is to water availability. Climate change alterations of historic water patterns may exacerbate this vulnerability in some regions. While the energy sector's water demand is anticipated to rise across the United States, the West is likely to experience some of the more significant constraints in meeting this demand. Examples of regional water use concerns related to energy are shale gas production using hydraulic fracturing in many regions across the nation, some solar electricity generation in the Southwest, and current biofuel feedstock production in the High Plains.

The 112th Congress may see the issue of energy's water demand in a variety of contexts, including oversight and legislation on energy, infrastructure, environment, agriculture, public lands, climate, research, and water. Approaches for addressing energy's water demand range from maintaining the current approach to taking a range of actions. One set of available actions includes those that attempt to minimize the growth in energy's freshwater use (e.g., through promotion of water-efficient energy alternatives and energy demand management), which could be accomplished through changes to broad policies or legislation targeted at water use. Many of the possible actions to decrease water use come with energy cost, generation, and reliability penalties. Another set of actions includes measures that facilitate access to water for the energy sector. While water allocations and permits generally are a state responsibility, limited federal actions to provide water to the energy sector are possible (e.g., access to surplus water at federal reservoirs). An additional set of actions encompasses investments in data and research to inform decision making and to expand water-efficient energy technology choices. These approaches represent different potential roles and expenses for government, the energy sector, and energy consumers. Legislation in the 111th Congress proposed a variety of actions, including provisions in H.R. 469, H.R. 2454, H.R. 3598, H.R. 1145, S. 1462, S. 1733, S. 3396, and the Secure Water Act of 2009, Subtitle IV of P.L. 111-11 (H.R. 146). A significant challenge to a federal response to the energy sector's water demand is that the available options are not equally needed, attractive, or feasible across the United States.


Energy's Water Demand:
Trends, Vulnerabilities, and Management

Energy's Water Use: A Policy Introduction

The nation's energy choices embody many tradeoffs. Water use is one of those tradeoffs. The energy sector is the fastest-growing water consumer in the United States. Projections attribute to the energy sector 85% of the growth in domestic water consumption between 2005 and 2030. This projected growth derives from anticipated demand for more energy, increased development of domestic energy sources, and greater use of water-intense energy alternatives. Much of the energy sector's growing water demand is concentrated in water-constrained regions. Affordable water supplies are limited, and competition for water is becoming more intense. Whether the energy sector helps exacerbate or alleviate future water tensions is influenced by current energy policy and investment choices. These choices also may determine whether water limits or harms the nation's ability to reliably meet energy demand. Water limitations may hinder some water-dependent energy activities in specific locations.

Water already plays a significant role in the energy sector, and water use by the energy sector already shapes national water use. For example, more than 80% of U.S. electricity is generated at thermoelectric facilities. With few exceptions, these thermoelectric power plants are cooled with water.1 In 2005, withdrawal of water for cooling represented 41% of water withdrawn nationally,2 and 6% of the water consumed nationally.3 The more water used by the energy sector, the more vulnerable energy production and reliability are to competition with other water uses and water constraints such as droughts. Climate change impacts on water supplies in some regions may exacerbate this vulnerability. Water availability can affect both existing and new energy activities, as well as all those economic activities that depend on the fuels and electricity produced.

The energy sector is changing. Paths chosen and capital investments made in the near term are likely to establish long-term trajectories for energy's water use. Trends indicate that energy's changing water use has national and regional significance for water consumption. A question for Congress is: what is the appropriate federal role in responding to energy's water demand? In the aggregate, current federal energy policies contribute to energy's rising water demand, while energy interests and the state and local governments are responsible for managing and meeting water demands and resolving competition over water resources.

Questions for Congress include who is the most appropriate entity to respond to energy's growing water demand and water vulnerability and how to respond. At present, little direct federal action is aimed at managing the energy sector's water demand; instead, the current division of responsibilities relies on energy interests and state and local governments to meet and manage energy's water demand and resolve energy-water conflicts. The role of federal policies in contributing to rising water demand is bringing into question the future federal role in this policy arena. Local or regional competition for water with existing users is often what makes energy's water demand significant; at the same time, the regional and local scales of water resources availability and management complicate many federal water-related actions.

Options for managing and meeting energy's water demand range from maintaining the current approach, with little federal action targeted at managing energy's water demand, to taking a variety of federal actions. One option is to minimize growth in energy's freshwater use. This could be accomplished through changes to broad policies (e.g., energy demand management) or legislation specifically targeted at water use (e.g., promotion of water-efficient energy alternatives). Another option is to improve the energy sector's access to water. Access is generally a responsibility of the state, but some limited federal actions are possible. An additional option is investing in data and research to inform decision-making and expand water-efficient energy technologies. These alternative policy approaches, which are not mutually exclusive, represent different potential roles and costs for the energy sector; energy consumers; and federal, state, and local governments. Legislation in the 111th Congress proposed many of the above options; examples include H.R. 469, H.R. 2454, H.R. 3598, H.R. 1145, S. 1462, S. 1733, S. 3396, and Subtitle IV of P.L. 111-11 (H.R. 146), the Secure Water Act of 2009.

During the 112th Congress, energy's water use may arise in a variety of contexts, including during consideration of energy, agriculture, public land, and water legislation and oversight. While the water tradeoffs of energy choices may be raised in a variety of contexts, they are unlikely to be the focus of energy debates. Instead, the priority on and investments toward different policy goals—low-cost reliable energy, energy independence and security, climate change mitigation, and job creation—are likely to be more significant drivers in congressional energy deliberations.

Scope and Structure of This Report

This report focuses on the factors shaping the energy sector's water demand, how that demand fits into national water consumption, and options for managing and meeting water demand. The report first lays out the trends shaping energy's water use; second, it discusses energy's vulnerability to water constraints; and third, it discusses projections of energy's water use. It then explores three regional examples of energy's water use: shale gas in Texas, solar energy in the Southwest, and biofuels in the High Plains. Finally, it discusses policy options and legislative approaches for managing energy's water use. Several appendixes provide more detailed information on specific technologies, fuels, and trends. The report does not discuss in detail the energy sector's water quality impacts, although they represent their own challenges, as shown by concerns over the water quality effects of hydraulic fracturing, mountaintop mining,4 and the Deepwater Horizon oil spill.5 Energy use by the water sector also is not discussed in this report, although water conservation is one of many available means for reducing energy demand.

The Federal Role in Water Allocation, Management, and Planning

The United States is endowed with considerable water resources; even in the drier West there are some major rivers and substantial groundwater supplies. Responsibility for development, management, and allocation of the nation's water resources is spread among federal, state, local, tribal, and private interests.

Water Allocation

The states administer most water rights allocation, deciding how to distribute freshwater among users. The mechanisms for distribution differ for each state, with states in the East and West historically following two different systems of water law. Distribution becomes more contentious as local or regional demand and environmental needs outpace sustainable and affordable supplies. States in large part decide whether and how to adapt allocation mechanisms and institutions to meet changing demands and priorities, and whether to allow or facilitate the movement of water among alternate uses. However, the federal role in allocation increases as the ramifications of state water allocations are felt in other states or internationally, or when they run contrary to federal law, such as the Endangered Species Act or the Clean Water Act. Rather than directly influencing state allocation laws, decisions, and institutions, the federal government usually uses indirect means to influence water use, such as programs for agricultural water conservation, investments in water augmentation research, and support for water resource planning.

Water Management

The federal government has been called upon to assist with and pay for a multitude of water resource development projects. Federal works range from improvements to facilitate navigation beginning in the earliest days of the nation, to more recent efforts to reduce flood damages and expand irrigation. In recent decades, the federal government also has regulated water quality, protected fish and wildlife, and facilitated some water supply augmentation. Criticism of the fractured nature of federal water policy and concerns about the efficiency of current water use have been recurrent themes for decades. Congress has not enacted comprehensive changes in federal water resources management or national water policy since enactment of the 1965 Water Resources Planning Act (P.L. 89-80; 42 U.S.C. § 1962). While many stakeholders call for better coordination and a clearer national "vision" for water management, Congress often has reacted to such proposals as attempts to exert federal control over state and local matters or as attempts to concentrate power in the executive branch. Instead, Congress has enacted numerous incremental changes, agency by agency, statute by statute. Both the executive and judicial branches have responded to these changes and, over time, have developed policy and planning mechanisms on an ad hoc basis. When coordination of federal activity has occurred, it has been driven largely by pending crises, such as potential threatened or endangered species listings, droughts, floods, and hurricanes; and by local or regional initiatives. Concern about water supply, however, has bolstered recent interest in legislation to establish a national water commission and strategy. (For more information on national water policy and a previous commission, see CRS Report R40573, Thirty-Five Years of Water Policy: The 1973 National Water Commission and Present Challenges, coordinated by [author name scrubbed] and [author name scrubbed]).

Water Planning

Energy's rising water demand and the potential for climate change to decrease water supply availability and reliability in some regions are part of a recent interest in water planning. Consensus, however, does not exist about the utility of or proper federal role in planning. Following the 1965 Water Resources Planning Act, the federal government supported federal, state, and river basin planning. By the late 1970s, this planning was both positively received and criticized for its costs and usefulness. The challenge of water planning is summed up in a 1973 report:

A persistent tendency of water resources planning has been the issuance of single valued projections of water use into the future under a continuation of present policies, leading to astronomical estimates of future water requirements.... The amount of water that is actually used in the future will depend in large measure on public policies that are adopted. The National Water Commission is convinced that there are few water "requirements."... But there are "demands" for water and water-related services that are affected by a whole host of other factors and policy decisions, some in fields far removed from what is generally considered to be water policy. (National Water Commission, Water Policies for the Future: Final Report to the President and to the Congress of the United States (Washington: GPO, 1973), p. 2)

In the late 1970s and early 1980s, federal funding for state planning declined, and federal involvement shrank with the defunding of the executive-level Water Resources Council and most federal river basin commissions. Some water resources stakeholders continue to view federal involvement in planning as infringing on state primacy, while other stakeholders support greater federal involvement in watershed, multi-objective, or integrated planning efforts. Some states, such as California, Texas, and Florida, have undertaken their own planning efforts.

Energy Trends Shape Water Demand

Trends in national energy investments, domestic energy use, population, and climate change impacts and responses can affect how much and where the energy sector uses water. Increased emphasis on domestic energy production and efforts to meet increasing energy demand are expected to increase freshwater use by the energy sector. A shift in the electricity sector away from traditional coal power plants may result in either more or less water consumption, depending on alternative fuels or electricity technologies. Carbon capture and sequestration (CCS) by electric utilities has the potential to consume significant quantities of water.6 Actions such as substituting wind for thermoelectric electricity generation could potentially reduce energy's water demand, but may raise other challenges for energy reliability, dispatchability, and transmission. Other impacts, such as the movement of irrigated agriculture from food crops to energy crops, raise other concerns. These and other examples of energy trends and their effects on energy's water use are summarized in Table 1. Appendix A has a more extensive list of trends.

Table 1. Energy Trends Produce Water Use Trends

Energy Trend

Resulting Trend in Energy's Water Use

Shift from foreign oil to biofuels

Increases energy's water consumption if domestic agricultural irrigation water (and other inputs) is needed for fuel production.

Shift to shale gas

Natural gas development using hydraulic fracturing may raise water quantity concerns if well development is geographically concentrated in areas with water constraints. However, natural gas from fracturing consumes less U.S. freshwater than domestic ethanol or onshore oil.

Growth in domestic electricity demand

More water used for electricity generation; how much more depends on how the electricity is produced (e.g., smaller quantities needed if electricity demands are met with wind and photovoltaic solar, larger quantities if met with fossil fuels or certain renewable sources).

Shift to renewable electricity

Concentrating solar power technologies can use more water to produce electricity than coal or natural gas; these solar facilities are likely to be concentrated in water-constrained areas. Technologies are available to reduce this water use. Other renewable technologies, such as photovoltaic solar and wind, use little water.

Use of carbon mitigation measures

Carbon capture and sequestration may double water consumption for fossil fuel electric generation.

Source: CRS.

Whether and how much the energy sector's water demand grows in the next decades will be significantly influenced by whether energy demand increases. Projections of the size and mix of the future energy portfolio vary widely. These projections are highly uncertain and are sensitive to many factors, including market and economic conditions, energy and agricultural policies, resource availability, technology developments, and environmental regulations. By association, projections of energy's water demand also are highly uncertain. The Energy Information Administration (EIA) in the Department of Energy (DOE) projects that the United States will consume 22% more electricity and 12% more liquid fuel in 2030 than in 2010.7 Population growth and increased electricity use per capita are some drivers of increasing demand.

Significant shifts to more water-intense electricity generation (e.g., concentrating solar power facilities using evaporative cooling) or more water-intense fuels (e.g., oil shale) could increase energy's water demand in locations with these energy resources.8 The significance of energy's water demand depends in part on local conditions—how much water is locally available and what its alternative uses would be. The most growth in freshwater consumption by the energy sector is expected in the Southwest, the Northwest, and the High Plains—that is, regions already experiencing intense competition over water and disputes over river and aquifer management.

Transportation's Water Consumption Is Increasing

The transportation sector offers an example of how energy trends affect water use. Water consumption by transportation fuels is anticipated to increase between 2005 and 2030; this increase is shaped by multiple trends. As shown in the figure below, an increase in miles driven and the increasing water-intensity of fuels, as a result of irrigated biofuels (i.e., biofuels derived from irrigated feedstock), overwhelms the water gains from improving vehicle fuel efficiency. (Appendix B has more information on water consumed for a variety of transportation fuels.) For light-duty vehicles (LDVs), the Energy Information Administration (EIA) projects a 50% increase in miles traveled, while the water-intensity of those miles is projected to rise from 40 gallons per 100 miles traveled to almost 90 gallons, according to researchers. Consequently, water consumption for LDV travel is roughly projected to triple from 2005 to 2030. Water consumption for LDV travel increased 50% between 2005 and 2010.

Sources: C. W. King,, M. E. Webber, and I. J. Duncan, "The Water Needs for LDV Transportation in the United States," Energy Policy, vol. 38 (2010), pp. 1157-1167; EIA, Annual Energy Outlook 2008, Table 7, Transportation Sector Key Indicators and Delivered Energy Consumption, Line 15. The King 2010 article used 2008 EIA data.

Energy Sector's Vulnerability to Water Constraints

The more freshwater used by the energy sector, the more the sector is vulnerable to water constraints. However, as described above and in Appendix A, major energy trends are pushing the sector to become more water-intensive. Water availability problems, especially regional drought and low streamflow, can pose a risk to energy production and reliability. Electricity generation is particularly sensitive to low-flow conditions. More than 80% of U.S. electricity is generated at thermoelectric facilities that depend on access to cooling water. Low-flow conditions and water scarcity may constrain water-intense alternatives for thermoelectric cooling in counties across the country. Additional ways that water can constrain energy include a possible decrease in hydroelectric generation during drought. Bioenergy yields may be reduced by low precipitation, droughts, heat waves, or floods. Energy extraction, like coal mining, may be scaled back to avoid water quality impairments exacerbated by low water conditions. While water constraints are often perceived as an issue for the western United States, an increasing number of water bodies in the East are experiencing diminished stream flows.9 While multiple examples exist of water availability affecting siting and operations of thermoelectric facilities from New York to Arizona,10 generally there are ways to reduce the use of water and the risk posed by water constraints.

Water supplies often are most constrained during summer, when the energy sector's water use is at its height in many regions. Approximately 24 of the nation's 104 nuclear reactors are situated in drought-prone regions.11 The Nuclear Regulatory Commission sets minimum source water elevation levels for each plant, so that a plant does not operate when source water levels drop below plant cooling water intakes. If cooling water sources fall below the established minimum water level, or if the maximum thermal threshold for the discharge of cooling water cannot be met, a facility is required to power down or go offline. A commonly cited example of this occurred on August 16, 2007, when a nuclear reactor owned by the Tennessee Valley Authority (TVA) at the Browns Ferry Nuclear Power Plant in Alabama shut down for a day. Its cooling water discharge exceeded temperature regulations that protect the environment and wildlife of the Tennessee River. In the summer of 2010, the same plant cut its electricity production to 45% of capacity when the cooling water temperature again exceeded discharge regulations.12 The reduced generation resulted in $50 million in higher cost to customers. TVA subsequently initiated a $160 million upgrade and expansion of its cooling system to avoid similar cooling constraints in the future.13

Water Constraints on Thermoelectric Cooling

More than 80% of U.S. electricity is generated at thermoelectric facilities. Thermoelectric facilities generally can be used to produce power as needed, according to consumer demand and fuel supply. This responsiveness to demand makes electricity from these thermoelectric facilities particularly attractive. Thermoelectric facilities can be fueled by a variety of fuels; coal, nuclear, and natural gas are the most common. Renewable sources such as concentrating solar power (CSP), geothermal, and renewable biomass also use a thermoelectric steam cycle. Thermoelectric power plants use fuel to produce heat to generate steam, which turns a turbine connected to a generator that produces electricity. Cooling is required to condense the steam back into boiler feed water, so the process can be repeated. With few exceptions, water is used to cool existing U.S. thermoelectric power plants. Thermoelectric cooling represents 41% of the freshwater withdrawn nationally, and roughly 6% of the water consumed nationally.

The cooling options available for thermoelectric plants vary in their water withdrawal and consumption. Water withdrawal is the volume of water removed from a water source. Consumption is the volume lost, that is, no longer available for use. Excessive withdrawals can harm aquatic ecosystems, while excessive consumption depletes the water available for other uses. The two common cooling methods are once-through cooling and evaporative cooling. Once-through cooling pulls large quantities of water off a water body, discharges the power plant's waste heat into the water (which typically raises its temperature 10° to 20°F), then returns the majority of the withdrawn water. Once-through cooling, while largely a non-consumptive water use, requires that water be continuously available for power plant operations. This reduces the ability for this water to be put toward other water uses and can make cooling operations vulnerable to low streamflows. Evaporative cooling withdraws much smaller volumes of water for use in a cooling tower or reservoir, where waste heat is dissipated by evaporating the cooling water. Evaporative cooling consumes water. Many power plants operating in the East use once-through cooling, while the majority in the West use evaporative cooling, although some coastal facilities use saline water for once-through cooling. In general, older thermoelectric plants use once-through cooling. The withdrawal's effect on the ecology and quality of the water body (e.g., elevated temperature and chemicals of the discharged cooling water) in once-through cooling have resulted in newer power plants generally using evaporative cooling. The figure below was produced by Electric Power Research Institute (EPRI) in 2003. It projects the counties where thermoelectric cooling may be constrained as the result of water availability in 2025; this figure was created assuming historic water availability; that is, it did not account for potential climate change effects on water supply or electricity demand.

Figure source: EPRI, A Survey of Water Use and Sustainability in the United States with a Focus on Power Generation, Topical Report, Nov. 2003. EPRI's analysis did not include Alaska and Hawaii.

Climate Change Could Increase Energy's Freshwater Vulnerability

Snowpack, precipitation, and runoff are strongly related to climate. Climate change researchers predict both water quantity and timing changes. That is, the research indicates more precipitation in the form of rain and less in the form of snow, and changes to seasonal water availability in some areas (e.g., low-flows during dry seasons). Additionally, climate models predict more frequent floods and droughts. These changes present challenges for hydroelectric dam operation.14 Changes in the availability and temperature of water resources also may affect operations of power plants that require water for cooling and that have thermal discharge limitations for cooling water. Climate change also may increase the demand for air conditioning, the electricity it consumes, and the water used to produce the electricity. The decreased runoff anticipated in the West, Southwest, California, and Pacific Northwest15 would decrease the amount of water available for all uses, including the energy sector. That is, the water resource impacts of a changing climate would likely exacerbate already projected thermoelectric cooling constraints. The energy sector also is vulnerable to potential increased flood and storm hazards associated with climate change. An example is the disrupting effects of floods on fuel transport.16

How Much Water Does Energy Demand?

How much water will the energy sector use in the future? In part, interest in answering this question is rooted in other questions of national significance, such as: Will water limit U.S. capacity to meet the nation's energy demand? Will water constrain the transition to greater energy independence? Will water hamper adoption of some renewable energy alternatives?

Quantification of energy's water demand and its significance is limited by significant gaps in available data and analyses. Water has no federal data agency comparable to the Energy Information Administration that projects alternative demand scenarios.17 There is no authoritative government source to cite for the level of water use by the energy sector or for projections of how that use may change in future decades. For example, there are no forecasts that use multiple scenarios to identify sensitivity of water demand to multiple factors and policies, or that analyze energy's water use and water vulnerability in the context of factors significant to energy choices and policies, such as energy and transmission costs, emissions, and reliability.18

For over 50 years, the U.S. Geological Survey (USGS) of the Department of the Interior has collected and published water use data every five years; however, the agency stopped collecting water consumption data after its 1995 survey due to funding constraints and data reliability problems. (USGS continues to collect water withdrawal data.) The 1995 USGS data are the basis of most projections of future water consumption in the United States.19 In the Secure Water Act of 2009, Congress authorized the USGS to perform a water use and availability assessment that includes water use trends in the energy sector; however, to date the agency had received no congressional appropriations for this program. Every 10 years the Forest Service forecasts water resources trends based largely on extrapolations of the USGS data and using the USGS data categories.20 The energy sector falls into a number of USGS water use categories, and it is impossible to disaggregate the categories to determine a value for the energy sector's water use. (Except for thermoelectric water withdrawals, the USGS water use data and Forest Service projections do not break out energy water use from other agricultural and industrial water uses.) Because of these limitations, the analysis herein relies on the most comprehensive projections available on the energy sector's water consumption, with the main source being a 2010 article by Deborah Elcock, an Argonne National Laboratory researcher, based on an updated and refined analysis from a report published by the lab in 2008.21

Although currently available data are limited, there are prospects for improved data and analysis in the future. The Secretary of the Interior announced in October 2010 that the USGS is undertaking a Colorado River Basin Geographic focus study as part of the department's WaterSMART Water Availability and Use Assessments initiative; this focus study may eventually comprise a component of the USGS water use and availability assessment Congress authorized in 2009, which would represent the first national water census since 1978.22 Additionally, regional efforts may inform future decision-making. For instance, the Western Governors' Association initiated in 2010 an energy-water nexus project, as part of its renewable energy transmission expansion effort, which includes a water availability assessment.23 The assessment is looking into projected water demands for large river basins and aquifer systems in the West and is expected to consider drought and potential climate change implications on the availability of river flows and water supply for energy development in the West. The effort is anticipated to conclude with policy recommendations available in late 2012, and is funded primarily by DOE.

Energy Leads Projections of Increasing U.S. Water Consumption

Energy's Water Demand May Increase 50% from 2005 to 2030

During the 1980s and 1990s, as a result of improved water efficiencies, U.S. water consumption remained below the historic high level of 101 billion gallons per day (bgd) estimated for 1980.24 Estimates of recent consumption, however, put U.S. freshwater consumption above the previous high and predict it will increase further in the next decades. (See Figure 1.) The projected rise is dominated by energy's water use. Nationally, energy's water consumption exceeds municipal and industrial use; it is currently second only to agriculture.

By modeling current energy and water trends, available projections predict that water consumption by 2030 will increase by 7% above the level consumed in 2005, as shown in Figure 1. Eighty-five percent of this growth is attributed to the energy sector, and an increase has already been observed between 2005 and 2010, with greater energy sector water use for irrigated biofuels.25 (See Appendix B.) Energy's water consumption (excluding hydropower) in 2005 was roughly 12 bgd, as shown in Figure 2; it is estimated to increase to 18 bgd by 2030. As shown by the data summarized in Figure 2, roughly 60% of the anticipated expansion is associated with bioenergy, and 40% is associated with thermoelectric cooling and fossil fuel mining, production, and processing. The analyses behind these projections do not capture the effects on water consumption of various fuel and generation technology changes in the electricity sector and potential adoption of CCS, nor do they include hydropower's water consumption.

Although the total national increase in Figure 1 may not appear large (7% over 25 years), multiple factors make this a significant increase for the water sector. First, growth in water consumption between 2005 and 2010 has put current water consumption above the previous high set in 1980. Second, water in many basins is largely allocated (or even over-allocated), with the water being delivered under legally binding agreements or withdrawn under issued permits. This means that making water available to the energy sector would likely decrease water use in another sector, such as agriculture. Third, Figure 1 represents national freshwater use; local proportions and increases in water demand from energy may be significantly higher. To illustrate the role that energy's water demand plays at the state level, roughly 16% of the water diverted in Kansas in 2008 went to biofuels; another 16% was used for electric power generation, while roughly 9% was used for municipal purposes.26 Fourth, in some regions, climate change is anticipated to decrease the quantity and reliability of water supplies. In particular, lower-altitude and drier areas are anticipated to become drier; some regions (e.g., the West) may experience more frequent or intense drought years punctuated by wet years.27 Lower precipitation in a portion of the Great Plains, and reduction in temperature-vulnerable snowpack in the western near-coastal mountains, are some of the anticipated changes to water supply.28 Therefore, energy's demand for more water use may coincide with a decreasing and less predictable water supply.

Figure 1. Projection of U.S. Water Consumption

Source: CRS, using data from D. Elcock, "Future U.S. Water Consumption: The Role of Energy Production," Journal of the American Water Resources Association, vol. 46, no. 3 (June 2010), pp. 447-480.

Figure 2. Energy's U.S. Freshwater Consumption

(in billion gallons per day, bgd)

Source: CRS, using data sources noted below.

Notes: NA = not available

a. D. Elcock, "Future U.S. Water Consumption: The Role of Energy Production," Journal of the American Water Resources Association, vol. 46, no. 3 (June 2010), pp. 447-480.

b. NETL, Estimating Freshwater Needs to Meet Future Thermoelectric Generation Requirements (2009 Update), p. 64.

c. A 2003 National Renewable Energy laboratory (NREL) report estimated that evaporation at reservoirs at the 120 largest existing U.S. hydroelectric facilities represented 9 bgd (see P. Torcellini et al., Consumptive Water Use for U.S. Power Production (NREL, 2003), available at http://www.nrel.gov/docs/fy04osti/35190.pdf., hereafter referred to as NREL 2003). This estimate is not shown in the figure above because these reservoirs are used for multiple purposes; therefore, evaporation at these reservoirs cannot be attributed to hydropower alone.

Projections are based on assumptions that are subject to change; in particular, management of energy demand and wide deployment of water-efficient energy options may significantly lower water use below projected levels. A DOE Energy Efficiency and Renewable Energy (EERE) study found that expanding the nation's electricity portfolio to 20% wind by 2030 would reduce water consumption by 1.2 bgd compared to expanding the current electricity mix. The saved water would be 41% from the Midwest/Great Plains, 29% from the West, 16% from the Southeast, and 14% from the Northeast.29

Alternatively, the projections in Figure 1 could be underestimates. Some factors that may augment energy's water consumption are not accounted for in these projections. More water could be consumed if carbon capture and sequestration is widely employed (see discussion below), or if more water-intense energy is produced. For example, significant expansion of electricity from evaporative-cooled concentrating solar power (CSP), or new hydropower reservoirs in areas with high evaporation rates, could drive up energy's water consumption. Similarly, a significant increase in oil shale development could increase energy's water use in regions with those deposits. In summary, projections based on extrapolations of current trends can illustrate one potential path for water consumption, but many factors, such as the role of changing technologies and policies, can result in actual water consumption varying significantly from projections.

Carbon Capture May Create a New Energy Water Demand

The majority of current U.S. electric generation is from fossil fuels. The electric generation mix in 2009 was 45% coal, 23% natural gas, 20% nuclear, and 7% hydroelectric, less than 4% non-hydroelectric renewable generation, and less than 2% other sources.30 Carbon capture technologies in the fossil fuel industry may reduce carbon dioxide emission, but they come with investment and resource costs to manufacture and operate. Current carbon capture technologies consume energy and water.31 Water is used at two points in the carbon capture cycle: cooling water is required for capture and compression processes, and water generally is consumed for power plant cooling when generating power needed to perform CCS. A 2009 study by the National Energy Technology Laboratory found that by 2030, carbon capture and sequestration could increase water consumption for electric generation by anywhere from 0.9 bgd to 2.3 bgd, depending on the scenarios used for plant additions and for deploying carbon capture technologies.32

Hydroelectric Water Consumption Is Poorly Documented

Although most hydropower generation represents an in-stream water use, dams built to generate hydropower and for other purposes consume water by increasing evaporation above free-flowing river conditions. That is, more evaporation occurs at the reservoir behind the dam than at the river without the dam. How much evaporation occurs at a reservoir with a hydroelectric generation depends on site, climate, and water conditions. CRS was unable to locate national data on existing or future projections for water consumption for hydroelectric generation. The currently available water consumption data from the USGS do not include hydropower evaporation. The agency states: "Although the quantity of water evaporated in the actual generation of hydropower (consumptive use) is small, considerable depletion of the available water supply for hydroelectric power generation occurs as an indirect result of evaporation from reservoirs and repeated reuse of water within pumped-storage power facilities."33

As noted in Figure 2, a 2003 NREL report estimated evaporation at 120 reservoirs with hydroelectric facilities at 9 bgd.34 Because these reservoirs generally serve multiple purposes, this evaporation cannot be attributed to hydropower alone and is not shown in the figure. Moreover, many reservoirs enhance water availability for multiple functions by providing storage that regulates streamflow, at times minimizing the occurrence of naturally occurring low-flow levels. These benefits, however, often come with harm to aquatic ecosystems, species, and floodplains. The NREL data illustrate that evaporation at facilities with hydropower can vary widely based on geography and climate.35 Site-specific estimates of water consumption for new hydroelectric generation using new reservoirs (e.g., some pumped storage proposals), therefore, would be required to understand hydroelectric generation's impacts on water resources. That is, new hydropower reservoirs cannot be assumed to have minimal effect on water consumption. Efficiency improvements or additions of hydropower generation at existing facilities, however, have the potential to increase electricity generation without increasing water consumption from evaporation.

Regional Significance of Energy's Water Demand

Much of the anticipated growth in the energy sector's water demand is in water-constrained areas, potentially exacerbating competition and low flow condition for water during summer and droughts. That is, while energy's water demand is anticipated to rise across the United States, the West is likely to experience some of the more significant constraints and conflicts in meeting this demand. While local or regional competition for water is often what makes energy's water demand significant, the regional and local scales of water resources and how they are managed often complicate federal water-related actions. To illustrate one aspect of how energy's growing water demand varies across the country, Figure 3 shows projections for expanded electricity generation in many water-constrained states (e.g., California, Texas, Arizona), primarily owing to rising electricity demand. The following examples of regional water consumption concerns are discussed in more detail: shale gas production in Texas using hydraulic fracturing, solar electricity generation in the Southwest; and biofuel production in the High Plains.

Technologies and management practices exist for reducing water use in each of these energy activities; however, these options generally come with energy cost, generation, and reliability penalties. Whether the benefits from the water savings of adopting these technologies and practices are viewed as outweighing these penalties often is a matter of perspective and is site specific. Moreover, little reliable and systematic data is available on the costs and benefits of adopting these measures in a variety of circumstances to better inform decision-making.

Figure 3. Population and Electricity Generation Projections, 2010 to 2030

Source: EIA, Supplemental Tables, Updated Annual Energy Outlook 2009 Reference Case with ARRA, Wash., DC, April 2009, http://www.eia.doe.gov/oiaf/aeo/supplement/stimulus/suparra.htm); and U.S. Census Bureau, U.S. Population Projections, March 2004. EIA did not include Alaska and Hawaii.

Energy Development: Shale Gas in Texas

Shale gas development has expanded in the last decade, in part because of technological advances in horizontal drilling and hydraulic fracturing. Fracturing involves the pressurized injection of water-based fluids (water, sand, and chemical mixtures) into a well to fracture a rock formation so that natural gas is released. (For more information on shale gas development, see CRS Report R40894, Unconventional Gas Shales: Development, Technology, and Policy Issues, coordinated by [author name scrubbed].) Shale gas formations occur in many areas of the United States.36 Exploiting this resource is bringing the oil and gas industry into communities unaccustomed to energy development. Water use is one of a number of issues being raised with the expansion of unconventional gas development.

While technological developments allow for greater extraction of gas, these technologies result in an increasing average amount of water used per well. That is, the longer the well, the more water is needed to drill and stimulate gas production. Freshwater, rather than saline water, is preferred for drilling and fracturing. Water use is concentrated in the early stages of well development, usually in the first few months. Once the well is producing, little or no water is required, unless refracturing is necessary. Much shale gas development is on private lands, and no government agency requires operators to report water use. Some data on water use per well are available, such as data from a DOE report in 2009 for four shale gas formations, which show water use ranging from 2.7 million gallons to 3.9 million gallons of freshwater per well.37 Some limited data are available on the amount of water per unit of energy produced. Data from Chesapeake Energy shale gas wells indicate that drilling, fracturing, extraction, and processing use between 0.6 and 3.8 gallons of water per million British thermal units (MMBtu) produced, or 5 to 29 gallons per megawatt-hour (MWh), as fuel for a combined cycle natural gas facility (not including the power plant water use).38 This puts shale gas at the lower end of water use for transportation fuels such as domestic onshore oil and irrigated biofuels, and below the water use for most coal and nuclear fuel production for electricity, according to a 2006 DOE report.39

The water use issue for natural gas is often one of concentration. That is, if many wells are being developed in a limited geographic area, the cumulative water needs of multiple drilling and fracturing operations may be locally significant and constraining to expansion of energy development. This may be particularly the case in areas with water constraints and competing water demands for domestic, agricultural, and thermoelectric use or areas where water for new gas operations represents a substantial expansion in water use.

Water quantity concerns have been raised for the Texas Barnett formation, particularly when drilling was using primarily fresh groundwater supplies and reached a peak of more than 3,000 new wells in 2008.40 With the subsequent decline in gas prices, the number of new wells drilled annually has dropped to 1,000, and increasingly the water is coming from surface supplies purchased from municipal water utilities where available, such as in the Fort Worth area. Based on available projections, the maximum use for natural gas production annually in the affected Texas counties may reach 7.5 billion gallons (0.021 bgd) under a high drilling scenario; this would represent 1.15% of local water consumption.41 While this shale gas use represents a modest share of local consumption, communities in this region of Texas have faced significant concerns about the sufficiency of available supplies during drought conditions for the region's growing population. This concern has brought scrutiny to all water uses, including shale gas. For most wells, the majority of the fluids injected into formation are not returned to the surface. In the Barnett formation, the water that is returned to the surface, known as flowback or produced water, is typically reinjected deep underground in a permitted disposal well.

Texas A&M researcher C. J. Vavra estimates that more than half of the produced water could be reused in subsequent fracturing operations, and a quarter could be put to beneficial use.42 These actions could reduce the impact of shale gas development on local water supplies but could raise other concerns. Legislation was considered by the 111th Congress to support research on this subject. For example, H.R. 469, the Produced Water Utilization Act of 2009, would have directed the Secretary of Energy to carry out a program to demonstrate technologies for environmentally sustainable use of energy-related produced waters from underground sources.

Water quantity concerns related to shale gas development are often overshadowed by interest in the economic benefits of the gas development and other local concerns with development. These other concerns include the risk that fracturing-related activities may contaminate freshwater supplies, community disruption and air pollution from truck traffic related to gas development (e.g., truck transport of drilling equipment and materials and fracturing additives and freshwater on and wastewater off the well site), and short-term and long-term changes to the local landscape and community. Although shale gas in Texas is discussed above, rising water demand for natural gas development is occurring or is anticipated in many other states and regions, such as the Northeast (Pennsylvania, New York), the South (e.g., Arkansas), and the upper Missouri River basin (Wyoming, South Dakota, North Dakota).

Renewable Energy Presents Regional Water Opportunities and Challenges

Water resource opportunities and challenges in meeting energy demand with renewable energy vary regionally.

- The Southwest has high-quality solar and geothermal resources, but water constraints and drought vulnerability favor more expensive, water-efficient use of these renewable resources.

- The Northwest generates most of its electricity from hydropower, but is diversifying to include more wind in light of environmental protections, increasing off-stream uses, and climate change effects on hydropower.

- The Great Plains may reduce water competition among the thermoelectric and agricultural sectors by exploiting wind power to produce electricity. Grid balancing and transmission of that electricity, especially to other regions, may pose constraints. Increases in irrigation to support bioenergy crops may tax stressed aquifers.

- The Southeast could reduce its dependence on coal and nuclear fuel and decrease its vulnerability to electricity interruptions during drought by producing electricity from biomass and photovoltaics.

- The Midwest could reduce competition between the thermoelectric and agricultural sectors and reduce the regional energy sector's low flow, drought, and flood vulnerability by exploiting its wind resources. This would require overcoming significant regulatory transmission issues. The Midwest is participating in the production of bioenergy crops, in particular corn for ethanol, raising water quality concerns, including that excess nutrients in agricultural runoff are feeding the growth of the "dead zone" in the Gulf of Mexico.

- The Northeast is not experiencing a regional issue with energy's growing water consumption; however, fracturing in shale gas formations is raising water quality concerns.

- Hawaii could transition to water-efficient power generation technologies to protect limited freshwater resources consumed in thermoelectric generation, which is dominated by oil-fueled power plants.

- Coastal regions, including Alaska, have the potential to develop offshore wind, tidal energy, waves, or ocean thermal gradients to reduce energy's onshore water use and land requirements. However, public opposition, transmission challenges, resource availability mismatched with demand, and natural hazards can pose challenges.

Source: CRS, with support from visiting researchers Ashlynn Stillwell and Kelly Twomey.

Electricity Generation: Solar in the Southwest

Another example of energy's regional water demand is concentrating solar power (CSP) in the Southwest. 43 The region has abundant solar resources, but the region's water constraints can influence the attractiveness and feasibility of different solar technologies and the suitability of specific sites. Most concentrating solar power (CSP) consists of ground-based arrays of mirrors that concentrate the sun's heat, which is used in a thermoelectric process to generate electricity. The two primary technologies are solar troughs and solar towers. Although CSP does not emit greenhouse gases, its use of a thermoelectric process can raise water concerns, particularly if evaporative cooling is employed (that is, if water is evaporated to dissipate waste heat). Similar water concerns would be raised if new fossil-fuel thermoelectric power plants were to be similarly located in the Southwest. For some Southwest counties with relatively low water use, large-scale deployment of CSP or another thermoelectric facility (even with water-efficient cooling technologies) could significantly increase the current demand for water in the county.44

Some solar developers are using cooling alternatives that require less water (or have been encouraged or required to do so as part of state permitting or federal approval of facilities on federal lands). These alternatives include dry or hybrid cooling or use of impaired waters for cooling (see Appendix C). These options generally come at a cost premium and with energy and cooling efficacy tradeoffs. Other solar developers have purchased water rights from willing sellers in states with active water markets. Still other solar developers are using solar technologies that require little or no water; these include photovoltaic solar, which uses panels of solar cells to convert sunlight directly into electricity, and dish engine CSP, which uses engines rather than a thermoelectric process45 to produce electricity. (See Appendix C.) While these technologies are water-efficient, they have other constraints (e.g., cost, land use, dispatchability). In summary, freshwater constraints like those in the Southwest do not preclude solar development, but access to water shapes the technologies and costs of solar development.

Energy Crops: Biofuels in the High Plains46

An additional example of energy's regional water demand is biofuels in the High Plains. The expansion of biofuel use through incentives and consumption mandates is an example of how federal energy policies can affect water use. The water quantity used for (and water quality impacts of) biofuels is particularly sensitive to biofuel feedstock, use of irrigation, and local climate and soil conditions at the growing site. Average water consumption by the dominant U.S. biofuel, corn-based ethanol, significantly exceeds the water intensity of other U.S. transportation fuels if the corn feedstock is irrigated. (See Appendix B.) Irrigation of only a small amount of biofuel feedstock in areas without sufficient rainfall to support feedstock growth without irrigation has the potential to substantially increase national water consumption for transportation fuels. The High Plains—consisting of portions of Texas, New Mexico, Colorado, Kansas, Nebraska, Wyoming, and South Dakota—is one example of a low-rainfall area. Much of the High Plains has faced water supply issues for decades, such as the declining level of portions of the Ogallala aquifer since the mid-1960s.47 Expansion of biofuels in this area is an additional demand exacerbating already competing water uses. For example, in Colorado in 2008, 16 times the annual quantity of treated water supplied to Fort Collins water customers was used to produce biofuels in the state, with the majority used in eastern Colorado.48 Of particular concern to the High Plains is expanded biofuels production on new or marginal lands, which could lead to additional irrigation demand and increased fertilizer application, causing both water quantity and quality concerns.49 Expansion of existing biofuel crops on land in current production raises water quality concerns because of the possible increased application of fertilizers and pesticides necessary to increase yields.50

Recognition of water, land, and other issues related to biofuels, particularly irrigated corn- and soybean-based biofuels, has led to a search for feedstocks and other organisms that use fewer resources to produce.51 Recent federal biofuels policies have attempted to assist this search by focusing on the development of a cellulosic biofuels industry.52 Dedicated biomass crops, such as switchgrass, hybrid poplars, and hybrid willows are considered by many to be more desirable crops because they have a short rotation (regrow quickly after each harvest) and use fewer resources, such as water and fertilizers, than traditional field crop production. Despite potential environmental benefits, concerns persist about the additional use of fertilizers and water resources that could be required to increase the per-acre yields to economically feasible levels; for example, that cellulosic feedstocks may be irrigated to increase yields, even though irrigation may not be required.53 Also, land use pressure for expanded production also applies to cellulosic biomass feedstock, possibly creating direct competition with current land conservation programs and replicating the concerns of traditional biofuel feedstock stated above. Despite federal incentives, technological and economic hurdles continue to prevent the cellulosic biofuels industry from developing to commercial scale production.54

Meeting and Managing Energy's Water Demand: Policy Options

The previous sections described how energy's demand for water is increasing and provided some regional examples. This section discusses options for meeting and managing that demand. Historically the energy sector and the states have determined how water is used in the energy sector, but the significant role that current federal policies are playing in driving up energy's water demand is raising questions about the federal role in meeting and managing that demand. These questions include

Congress is faced with deciding not only whether, and if so how, to alter current policies to respond to energy's water demand, but also who is the most appropriate entity to respond to energy's growing water demand. Currently little direct federal action is aimed at managing the energy sector's water demand, although federal policies at times have significant indirect influence on this demand. Instead, present roles rely on the energy industry and the states and local governments to manage water constraints and to resolve energy-water conflicts.

The issue of the energy sector's water use may arise during the 112th Congress in a variety of contexts. Support or opposition for legislation affecting energy's water demand may be influenced by opinions about the proper federal role in water allocation and planning, as well as concerns about the cost of actions and who is responsible for those costs. Positions on the larger energy and climate debate and other factors may also be important. Federal responses to energy's water use are complicated by the wide-ranging and place-based nature of the issue, the variety of actors involved, the costs and other tradeoffs involved, and the existing institutions and divisions of responsibilities for water and energy.

If increased federal action to meet and manage energy's water demand is deemed appropriate, possible actions fall under a few broad options. Attempts can be made to minimize the growth in energy's freshwater use by adopting general energy policies that are less water intense and more sensitive to water constraints, or by specifically promoting activities that reduce energy's water use, such as incentives for adopting less water intense energy generation technologies. Another option is to make freshwater available for the energy sector (e.g., through allocations, permits, or facilitating water trading); however, the majority of water quantity allocation and permitting decisions are up to the states. An additional option is improving data and analysis on energy's water use to better inform decision-making (e.g., resource planning efforts and decision-support tools) and enhancing the availability and dissemination of water-efficient technological alternatives. These approaches are presented in Table 2, with examples of each from legislation reported by a congressional committee of the 111th Congress.

These options are not mutually exclusive and different options may be more or less appropriate and attractive for different components of the energy sector's water demand. These options also represent different potential roles and costs for federal and state governments, the energy sector, and energy consumers. No entity has performed a comparative analysis of these policy options using multiple criteria (e.g., cost-effectiveness; who bears the cost; risks, reliability, and vulnerability; opportunity costs; role of state entities; role of federal entities). One of the challenges of a federal response to energy's water demand is that the concerns, policy options, and technological options vary greatly by region.55

Table 2. Sample Legislative Responses to Energy's Water Demand

Response

Examples in Committee-Reported Legislation in the 111th Congress

No Federal Action Directed at Managing Water Use

Existing federal energy (including conservation and efficiency policies), climate, agricultural, and environmental laws and policies indirectly, but at times significantly, shape the energy sector's water use.

Minimize Energy Sector's Growth in Water Use

 

Promote water-efficient energy through standards, regulations, or incentives

Could be an outcome related to increased adoption of electric generation from wind, photovoltaics, or natural gas—which may occur as a result of energy markets, cap and trade legislation (e.g., H.R. 2454, American Clean Energy and Security Act of 2009, passed House and placed on Senate Legislative Calendar), or renewable electricity standards (e.g., S. 1462, American Clean Energy Leadership Act of 2009, reported by Senate ENR)—depending on how the energy industry responds to the legislation.

Promote use of technologies to reduce energy's water use though incentives or regulations

No explicit mention in legislation reported in the 111th Congress; however, state and federal energy permitting actions have required or promoted actions to reduce water use (e.g., roughly half of fast-tracked CSP development projects on federal lands are adopting dry cooling because of concerns about freshwater demands of other cooling options).

Promote conservation and efficiency measures through incentives or regulations

§ 2 of S. 3396, Supply Star Act of 2010 (reported by Senate ENR), would establish a federal program to promote resource-efficient industrial supply chains (such sums as necessary, $35 million total for five-year CBO authorization estimate).

§ 147 of Title I, Subtitle D, "Energy and Water Integration," in S. 1462 (reported by Senate ENR) would direct the Secretary of Energy to create a competitive energy-water conservation grant program for local governments, water agencies, and tribes ($100 million for each fiscal year from FY2010 to FY2015).

Develop and assess technologies to reduce energy's water use

§ 142 of S. 1462 would require a federal study to identify alternatives to optimize water and energy efficiency in the production of electricity (such sums as necessary).

§ 162 of S. 1733, Clean Energy Jobs and American Power Act (reported by Senate EPW), would require EPA to create a "1,000,000,000 Gallon Challenge Grant Program" to fund projects that have the potential for producing significant quantities of biofuels from renewable biomass, where surface and groundwater use and impacts are considered in determining whether the biofuel is renewable ($500 million for FY2010 through FY2014).

§ 196 of Title I of H.R. 2454 and § 152 of S. 1733 would authorize the Secretary of Energy to provide nonprofit entities with grants to conduct competitive programs to support start-up businesses in clean energy, including water conservation ($20 million).

Improve Energy Sector Access to Water

 

Allocate sustainably available water

Largely state responsibility; no explicit mention in federal legislation, but some federal actions underway (e.g., review of requests for surplus water contracts under Flood Control Act of 1944, 33 U.S.C. § 708). Also, already authorized efforts, if completed, could inform allocation decisions; for example, § 9503 of Subtitle IV, "Secure Water," in P.L. 111-11 authorizes the assessment and development of strategies to address water quantity effects of global climate change in Bureau of Reclamation service areas.

Facilitate transfer of water saved in non-energy sector

§ 9504 of P.L. 111-11 establishes a program to provide grants or enter into cooperative agreements to (among other purposes) conserve water, increase water use efficiency, and facilitate water markets in the 17 Reclamation states ($200 million).

Inform Decisions and Support Research Expanding Water-Efficient Energy Options

 

Data and Assessments

§ 9508 of P.L. 111-11 requires the Secretary of the Interior to establish a national water availability and use assessment program that reports on significant trends, including significant changes in water use due to the development of new energy supplies ($20.0 million for each of FY2009 through FY2013).

§ 3 of H.R. 3598, Energy and Water Integration Act (passed House), would create a council to recommend actions that promote improved energy and water resource data collection, and to conduct workshops to promote data exchange ($5 million for each of fiscal years 2011 through 2015).

§ 149 of S. 1462 would mandate a study, led by the Department of Energy, examining industrial water use, peak energy use in water treatment and delivery, and energy "embedded" in water (no authorization of appropriations specified).

§ 9505 of P.L. 111-11, requires the Secretary of Energy to assess federal hydroelectric power production to water supply risks posed by global climate change (such sums as necessary).

Research

§ 2 of H.R. 3598 would require DOE to develop a strategic plan for energy-water research needs within DOE research activities ($60 million for each of FY2011 through FY2015).

§ 171 of Subtitle H, Title I, of H.R. 2454 would direct the Secretary of Energy to establish energy innovation hubs to conduct research, including research that enhances water security (no specific sum set).

Integrated energy -water planning

No explicit mention in legislation in the 111th Congress

Technical assistance

§ 148 of S. 1462 would require the Secretary of Energy to create a technical assistance program for reducing energy use by rural water utilities ($7 million for each of FY2010 through FY2015).

§ 10 of H.R. 1145, National Water Research and Development Initiative Act of 2009, would require the EPA Administrator to establish a pilot program for energy audits of water related infrastructure (no amount specified for this section, entire bill has $2 million for each of FY2010 through Fy2014).

Source: CRS.

Notes: ENR = Energy and Natural Resources Committee, EPW = Environment and Public Works Committee, EPA = U.S. Environmental Protection Agency.

Whether these policy alternatives should be pursued at the local, state, or national level depends in part on perspectives on the appropriate role of each level of government. Perspectives on the policy options related to energy's water demand also are influenced by long histories of regulation, management, promotion, and oversight of the nation's energy and water resources and infrastructure. Current and evolving conditions also play a role: providing greater access to water for the energy sector (which is primarily up to the states) may be difficult and controversial in water-scarce, drought-prone, or environmentally sensitive areas, especially with climate change anticipated to affect the availability and reliability of water in some regions.

States have traditionally had primacy in water allocation, so decisions about permitting energy's water use largely have been non-federal. State and federal laws and policies can affect the ease or difficulty of, and incentives for, transferring water from existing uses to energy. The federal government can, if it chooses, promote change in state water laws, institutions, and decision-making.56 Some view this as infringing on states' rights.57 Similarly, while private entities make many of the decisions on the energy sector's water use, the public sector influences these decisions through numerous routes (e.g., tax incentives, loan guarantees, permits, regulations, planning, education); this influence can come from local, state, or federal policies.

The federal role in water resource allocation and management increases as the federal interest increases—for example, when the use occurs on federal lands. Competing water demands, including those from the energy sector, are raising questions for federal agencies about the operations of federal facilities. For instance, can water delivered to Bureau of Reclamation contractors (e.g., water delivered to irrigation districts in California's Central Valley) be used not for agriculture, but for energy development (e.g., evaporative cooling of a concentrating solar power facility)? Can water from an Army Corps of Engineers dam that has multiple purposes (e.g., flood control, navigation, and/or municipal or agricultural water supply) be used for the oil and gas development, and if so, how much water can the Corps provide under existing authorities?

Using Water Stored Behind Federal Dams for Oil and Gas Water Supply

Western North Dakota illustrates some stakeholders' interest in using water stored at federal dams for use by the energy sector. The region has experienced substantial expansion in shale oil production since 2008 using the same horizontal drilling and fracturing processes used for shale gas developments and at times waterflooding techniques to maintain pressure during production. There is concern about depletion of limited groundwater supplies as described in an August 2010 report Water Appropriation Requirements, Current Water Use & Water Availability for Energy Industries in North Dakota produced by the North Dakota State Water Commission. The industry's significant expansion in water demand since 2008 may reach 22 million gallons per day (24,400 acre-feet annually) depending on the specifics of drilling operations in 2011 and could continue to rise in subsequent years if drilling and fracturing expand. The water use in 2011 could represent more than 20% of total water usage in the 11 counties in Western North Dakota that are producing shale oil and located in proximity to a lake formed by a federal dam on the Missouri River, In December 2010, the Corps released a draft report, Garrison Dam/Lake Sakakawea Project, North Dakota, Draft Surplus Water Report (Dec. 2010), that if finalized would allow the Secretary of the Army to meet the industry's water demand for up to 10 years by allowing withdrawals from Lake Sakakawea at Garrison Dam (ND).

Observations and Concluding Remarks

The energy sector has long been a major water user, so why the current concern? Major energy trends are pushing the energy sector to become more dependent on, and therefore vulnerable to, freshwater availability. This is occurring at a time of increasing concerns about the adequacy and reliability of freshwater supplies due to population growth and climate change. Energy resource and technology paths chosen and capital investments made in the near term are likely to establish long-term trajectories for energy's water use.

Many of the current trends are in part driven by federal policy. The federal government partially shapes the energy sector and at times defines a vision for the nation's energy future (e.g., biofuel production targets). Some stakeholders have raised concerns about the feasibility and consequences of meeting various energy targets and policy proposals, including concerns about physical inputs like water, land, materials, and rare minerals.58 Because affordable freshwater is a finite resource, commitments of water supplies for the energy sector reduce availability for other sectors and for ecosystems. Local or regional competition for water is often what makes energy's water demand significant; at the same time, it is the regional and local scale of water resources and how they are managed that often complicates many federal water-related actions. The federal role in energy supply and demand raises questions about the policy direction for meeting and managing energy's water needs, among them: If energy security is a national security issue, is energy's water use by association a national security issue? Would this be a justification for federal spending on energy and water efficiency measures?

Water supply concerns are not only being raised in the context of energy. There also is growing concern about water availability and aquatic conditions for meeting the demands of the agricultural and municipal sectors and the needs of ecosystems and threatened and endangered species; these concerns are raised particularly in the context of droughts and impacts of climate change on water resources. Given available freshwater resources, a challenge for the nation will be to cost-effectively, sustainably, and reliably meet energy demands while satisfying agricultural, municipal, and industrial water demand, as well as ecosystem needs. This challenge raises fundamental and controversial questions about how U.S. freshwater resources are allocated and used for various purposes, and about the availability and value of water in different sectors of the economy and in the environment. At issue for Congress is the role that the federal government and federal funding plays in shaping, meeting, and managing energy's water demand, while accounting for the significant role of the states and private sector in water use decisions.

Appendix A. Energy's Water Consumption Trends

Ideally, policy and decision makers should know how energy choices and policies compare across a wide array of parameters (e.g., cost, reliability, dispatchability, emissions, land requirements, water use) under different scenarios. That is, informed decisions would require water use data, analyses of least-cost water and energy conservation and efficiency actions, understanding of other water uses and their costs and benefits, life-cycle assessments of energy's water uses and risks, and more. Such assessments are not available. While not addressing this shortfall, Table A-1 and Table A-2 summarize the freshwater impacts of numerous shifts in transportation fuels and the electricity sector, respectively.

Without such multi-variable assessments, it is difficult to understand the full implications of energy decisions. While this report focuses on energy's water use, there are a host of other factors to consider when analyzing energy policy tradeoffs. For example, fuel and technologies for generating electricity are not equally dispatchable; that is, is they are not equally able to increase or decrease generation, or to be brought online or shut down to match demand. Thermoelectric facilities using fossil fuel or geothermal sources are advantageous because they can be operated to produce electricity constantly or dialed up or down with demand. While electricity from hydropower, tidal, and wave energy generally can be produced fairly predictably, often the timing of operations is subject to the intensity of tides and waves, to water conditions such as drought or large storms, and to environmental restrictions regarding potential impacts on marine life and ecosystems. In contrast, until more advanced storage technologies become commercially competitive, photovoltaics and wind, which require very little water, remain intermittent sources that generally cannot be dispatched when the sun is not shining or the wind is not blowing.

Table A-1. Domestic Freshwater Impacts from Transportation Fuel Shifts

Shifts in Imported Fuel Use

Change in Domestic Freshwater Consumption

Impairments of domestic water quality and/or aquatic ecosystems

Domestic fuel sources displace foreign fuels

Little change or
depending on domestic fuel

 

Domestic oil using enhanced oil recovery displaces foreign gasoline

from produced water

Domestic offshore oil displaces foreign oil

Little change

from spill risk

Fuel conservation (e.g., resulting from increased fuel efficiency standards) decreases oil imports

Little change

Little change

Imported biofuels displace foreign gasoline

Little change

Little change

Source: CRS.

Table A-2. Domestic Freshwater Impacts from Electricity Sector Shifts

Shifts in Electricity Generation

Change in U.S. Freshwater Consumption

Impairment of Domestic Water Quality and/or Aquatic Ecosystems

Fuel Source Shift

 

 

Nuclear displaces coal

Unclear with current data

Shift in pollutants generated during fuel extraction, processing, and electricity generation

Concentrating solar power (with freshwater cooling) displaces coal

 

 

Domestic natural gas displaces coal

 

Shift from nonpoint source to more point source pollution

Hydropower without new reservoirs displaces coal

 

Shift from nonpoint source pollution to potential harm to aquatic ecosystem and species

Photovoltaics displace coal

 

 

Wind displaces coal

 

 

Ocean/tidal/hydrokinetic displace coal

 

Potential for harm to aquatic ecosystem and species

Geothermal displaces coal

 

 

Electricity Sector Shifts

 

 

CCS added to a power plant

 

unknown

Dry cooling replaces evaporative cooling

 

 

Electricity conservation decreases electricity consumption

 

 

Source: CRS.

Appendix B. Water Use by Transportation Fuels

D. Elcock's study projects that the energy sector's consumptive water use will increase from 6 billion gallons per day (bgd) in 2005 to 10 bgd in 2030 in the areas of fossil fuel mining, production, and processing and bioenergy.59 (See Figure B-1.) The growth is dominated by water consumed for bioenergy.60 The Elcock study and other sources show that the effect of bioenergy on energy's water use was already felt between 2005 and 2010.61 The projected water demand by bioenergy could drop, potentially significantly, if less-water intense bioenergy is developed and adopted. This projection covers most of the water used to fuel transportation and the water used for obtaining and preparing fossil fuels for use in either transportation or the electricity sector. Figure B-2 provides data from research on the comparative water intensity of different U.S. transportation fuels. Note that the figure has a logarithmic scale, and that the water consumed traveling on irrigated biofuels is orders of magnitude larger than the water embedded in other fuels.

Figure B-1. Biofuels Dominate Energy Production's Projected Water Consumption

Source: Elcock 2010.

Figure B-2. Water Intensity of Transportation Fuels

Source: CRS, modified from M. Mantell, "Abundant, Affordable, and Surprisingly Water Efficient," presented at 2009 GWCP Water/Energy Sustainability Symposium in Salt Lake City, September 13-16, 2009. Original data from C. King and M. Webber, "Water Intensity of Transportation," Environmental Science & Technology, vol . 42, no. 21 (2009), available at http://pubs.acs.org/doi/pdf/10.1021/es800367m.

Notes: NG = natural gas; CNG = compressed natural gas. Note the logarithmic scale.

Appendix C. Water Use for Electricity Generation

Trends in the electricity sector contributing to increased water consumption currently overwhelm actions that reduce water consumption. As a result, local water challenges presented by electric generation are becoming more common in many water-constrained areas. These challenges may drive action to reduce electricity's freshwater footprint, such as the adoption of water-efficient electricity generation and water-efficient thermoelectric cooling options, or the use of impaired water. This appendix describes the available data on the electricity sector's water consumption and data on the different electricity generation's water use. Then it presents alternative thermoelectric cooling choices that may reduce electricity's water use. Lastly, it discusses the tradeoffs between water use and other characteristics (e.g., environmental impacts, reliability, dispatchability) of electric generation from hydropower facilities, photovoltaic solar and wind installations, and geothermal resources.

Data on Electricity's Water Use

Available estimates for the electricity sector's water consumption focus primarily on thermoelectric cooling water needs because cooling dominates water use during generation. Other aspects of electric production (e.g., fuel mining and processing) also use water. (See Table C-1.) Data and projections on the water consumed in the mining, production, and processing of fuels for generating electricity are bundled with the production of fossil fuels used in the transportation sector, like the Elcock study. The projections in Figure 2 for thermoelectric cooling come from the Elcock study, which was based on projections in a 2007 report by NETL.62 The NETL projections are limited to coal, natural gas, and nuclear-powered facilities; that is, they do not calculate water use changes that would occur from shifts in the electricity sector broadly (e.g., adoption of more wind or photovoltaics) or shifts in thermoelectric generation more specifically (e.g., concentrating solar power or biomass generation). Elcock assumed that biomass generation for electricity production would be based in regions not requiring irrigation.63

No analyses of electricity's total water consumption or how it may change under different policies exist; this type of analysis is difficult to perform without reliable data on water intensities of different electricity generation technologies and fuels. No authoritative comparison of the various water intensities of electricity generation options exists. Figure C-1 and Figure C-2 illustrate the best available data for average water intensities for various electricity alternatives, with and without carbon mitigation using CCS, respectively. These figures are based on Table C-1, which represents the best available data on water consumed in producing electricity using various fuels and technologies.64 The data in Figure C-1 are imperfect and come from multiple sources, raising questions about whether the data can be used to make accurate comparisons across technologies.

Figure C-1. Water Intensity of Electricity Generation Alternatives without CCS

Source: CRS. Data represent evaporative-cooled thermoelectric, except for geothermal, see Table C-1. IGCC = Integrated Gasification Combined-Cycle; CC = Combined Cycle.

Figure C-2. Water Intensity of Electricity Generation Alternatives with CCS

Source: CRS. Data represent evaporative-cooled thermoelectric, except for geothermal, see Table C-1.

Table C-1. Water Consumption for Electricity Generation by Fuel Source

Generation Technology and Fuel

Water for Fuel Mining, Production, or Processing (gal/MWh)

Evaporative Cooling Water at Power Plant (gal/MWh)

Other Water Used for Power Plant Operations
(gal/MWh)

Avg. Total Water Intensity
(gal/MWh)

Data Sources

Biomass/Waste

 

 

 

 

 

Non-irrigated biomass

0

300-480

30

420

DOE 2006

Non-irrigated biomass with CCS

0

Not available

30

DOE 2006

Irrigated biomass

Highly variable

300-480

30

DOE 2006

Municipal waste

Not available

300-480

30

420

DOE 2006

Coal

 

 

 

 

 

Conventional/Subcritical coal

5-74

449

68

557

DOE 2006;
NETL 2009

Conventional/Subcritical coal with CCS

5-74

884

101

DOE 2006;
NETL 2009

Supercritical coal

5-74

392

59

491

DOE 2006;
NETL 2009

Supercritical coal with CCS

5-74

759

86

DOE 2006;
NETL 2009

Ultra-supercritical Coal

Not available

Not available

Not available

 

 

Ultra clean coal

Not available

Not available

Not available

 

 

Coal IGCC (slurry fed)

30-70

290

19

359

DOE 2006;
NETL 2009

Coal IGCC (slurry fed) with CCS

30-70

355

97

502

DOE 2006;
NETL 2009

Coal IGCC (dry fed)

5-74

243

53

336

DOE 2006;
NETL 2009

Coal IGCC (dry fed) with CCS

5-74

355

120

515

DOE 2006;
NETL 2009

Geothermal

 

 

 

 

 

Enhanced geothermal

0

Dry cooling

290-720

585

Argonne 2010

Geothermal binary

0

Dry cooling

80-270

175

Argonne 2010

Geothermal flash

0

Dry cooling

5-10

8

Argonne 2010

Hydroelectric

 

 

Evaporation varies with site

 

NREL 2003

Natural Gas

 

 

 

 

 

Natural gas combined-cycle

11

192

0

203

DOE 2006;
NETL 2009

Natural gas combined-cycle with CCS

11

338

0

349

DOE 2006;
NETL 2009

Nuclear

 

 

 

 

 

Nuclear steam cycle

45-150

720
(cooling pond)

30

848

DOE 2006

Nuclear boiling water

45-150

Not available

DOE 2006

High temperature gas cooled nuclear

45-15

Not Available

DOE 2006

Small modular nuclear

Not Available

Dry cooling possible

Not available

 

Ocean/Tidal

0

Not applicable

Not available

0

 

Oil

 

 

 

 

 

Oil

No data

300-480

Not available

DOE 2006

Oil from enhanced oil recovery

Highly variable, potentially significant

300-480

Not available

DOE 2006

Solar

 

 

 

 

 

CSP – solar trough

0

760-920

80

920

DOE 2006;
DOE n.d.

CSP – solar tower

0

750

90

840

DOE 2006;
DOE n.d.

Dish Engine Solar

0

Air cooled

4

4

NREL 2002

Photovoltaics

0

Not applicable

4, higher for locations requiring more panel washing

4

NREL 2002

Wind – onshore or offshore

negligible

 

 

0

DOE 2008

Sources:
Argonne National Laboratory released for comment the following report: ANL, DRAFT Water Use in the Development and Operation of Geothermal Power Plants, Sep. 2010.
Energy Demands on Water Resources: Report to Congress on the Interdependency of Energy and Water, Dec. 2006.
DOE, Concentrating Solar Power Commercial Application Study: Reducing Water Consumption of Concentrating Solar Power Electricity Generation, Washington, DC, no date (n.d.).
NETL, Estimating Freshwater Needs to Meet Future Thermoelectric Generation Requirements (2009 Update), 2009. NREL, Fuel from the Sky: Solar Power's Potential for Western Energy Supply, NREL/SR-550-32160 July 2002.
P. Torcellini et al., Consumptive Water Use for U.S. Power Production (NREL), 2003.

Notes: Evaporative cooling for thermoelectric facilities is assumed, unless otherwise noted in the table. Data do not include water consumed in manufacturing or construction. While the total column represents the average total water consumption for a unit of electricity, the water for fuel production may occur at a different location than the water consumed at the power plant.

Thermoelectric Cooling: Emerging Alternatives

The withdrawal and water quality impacts of once-through cooling have resulted in newer power plants generally using evaporative cooling.65 Emerging cooling technologies have the potential to use much less freshwater than once-through or evaporative cooling. These include dry cooling (previously discussed), hybrid dry-wet cooling, cooling with fluids other than freshwater, and more innovative technologies (e.g., wet-surface air coolers, advanced wet cooling). However, these alternatives have their own costs and disadvantages.

A DOE report found that dry cooling could reduce water consumption to roughly 80 gal/MWh for solar troughs and 90 gal/MWh for solar towers.66 While they consume less water, dry and hybrid cooling systems have financial as well as efficiency costs. Total annualized costs for dry cooling tower systems can be four times those of evaporative cooling tower systems.67 Due to the higher cooling and lower generation efficiency costs, the cost of electricity from a dry cooled solar thermal plant may be 3% to 8% higher than a similar wet cooled plant.68 Dry cooling uses fans to blow air for steam condensation. While power plants with dry cooling use considerably less water, dry cooling is less effective at cooling the power plant than evaporative cooling, thus reducing electric generation at the facility. The DOE report also found that electricity generation at a dry-cooled facility dropped off at ambient temperatures above 100°F. For a solar parabolic trough facility in the Southwest, the benefit in the reduction in water consumption from dry cooling resulted in cost increases of 2% to 9% and a reduction in energy generation of 4.5% to 5%.69 The cost and energy generation penalties for dry cooling depend largely on how much time a facility has ambient temperature above 100°F. Dry cooling would reduce generation on the same hot days when summer peak electricity demand is greatest.

Hybrid wet-dry cooling attempts to balance water consumption with power generation efficiency; it remains under development for commercial scale applications. To weigh the tradeoffs in energy generation, cost, and water use, DOE researched hybrid cooling processes that combine dry and evaporative cooling. The hybrid system consists of parallel evaporative and dry cooling facilities, with the evaporative cooling operating only on hot days. By using dry cooling generally and evaporative cooling above certain ambient temperatures, losses of thermal efficiency from dry cooling can be reduced. How often the evaporative cooling is used determines how much water is consumed and the effect of hot days on thermal efficiency. DOE found that a hybrid cooling system in the Southwest using 50% of the water of evaporative cooling would maintain 99% of the performance of an evaporative-cooled facility. A hybrid cooling system using 10% of the water of evaporative cooling would maintain 97% of the energy performance. A hybrid system requires greater capital investment and is more complicated to operate; its cost effectiveness over the life of the project depends in part of the cost of water.70

Another means for decreasing freshwater impacts is employing alternative water sources for evaporative-cooling.71 These alternative water sources include effluent from wastewater treatment plants72 or other reclaimed or impaired water, such as brackish or low-quality groundwater73 and mine pool water.74 These alternative water sources, however, may lead to additional scaling, corrosion, and fouling of cooling equipment or require pretreatment before cooling use. Additional research may be able to improve the viability of saline water cooling. Availability of alternative water sources in proximity to electricity generation facilities is a potential limitation to their use. Understanding of the opportunities for brackish cooling alternatives is likely to be improved when the assessment of brackish groundwater authorized by Section 9507 of P.L. 111-11, the Omnibus Public Land Management Act of 2009, becomes available.

Tradeoffs of Select Electricity Generation Technologies

Hydroelectric Generation

Hydroelectric power is produced when water passes through a turbine. Turbines for large-scale hydroelectric generation are located at dams. Electricity at U.S. hydropower facilities is produced with relatively low greenhouse gas emissions. However, hydropower's environmental effects can be significant. Conventional hydropower development through dam building often significantly alters river ecosystems, harming many indigenous species. Drought and changes to hydrology, such as possible reduction in snowpack under a changing climate, can reduce electricity generation at hydropower facilities because of the effects on reservoir operations and levels.

Constructing new large dams is contentious; therefore, efforts to identify opportunities for increasing hydropower generation have focused on smaller-scale opportunities or improved efficiency and expansion of hydropower at existing facilities.75 The Electric Power Research Institute estimates a potential capacity hydropower gain of 10 GW by 2025 as feasible, without the construction of new large dams.76 Six western states—Alaska, Washington, Oregon, California, Idaho, and Montana—have the highest potentials.77 Despite this identified potential, little additional hydropower generation has been installed in recent years for a number of reasons (e.g., hydropower and water-related permit and regulatory requirements, and public concerns and perceptions about environmental effects). Similarly, the number of applications for FERC preliminary permits for pumped storage has increased substantially in recent years; however, the proposals have not proceeded to construction.

Photovoltaic Solar and Wind

Renewable electricity technologies that do not use thermoelectric processes may have minimal water requirements for electricity generation. Wind turbines and solar photovoltaic (PV) panels, for example, require small volumes of water for cleaning, but otherwise use no water. However, the minimal water intensity of wind and PV comes with tradeoffs. Transmission constraints;78 cost; and regulatory, technical, and operational factors currently restrict the extent to which solar and wind resources can be exploited to meet electricity demand. As previously noted, wind and PV are intermittent electricity sources. Some storage options for these intermittent technologies exist (e.g., wind used in conjunction with a pumped storage hydropower facility); however, their applications are limited and intermittency continues to limit generation from wind and PV.79 Electricity from PV is also currently more expensive than electricity from CSP, although electricity from wind is less expensive than electricity from CSP. For a discussion of wind technologies and policy issues, see CRS Report RL34546, Wind Power in the United States: Technology, Economic, and Policy Issues, by [author name scrubbed].

Geothermal

There are several ways to use geothermal energy: electricity generation (discussed herein) as well as direct-use (recovering water heated by the earth) and heat pumps (using the earth's heat to cool/heat buildings). Traditional geothermal power production uses naturally occurring convective hydrothermal sources in hot rock formations to produce steam to run a thermoelectric power plant's turbines (i.e., a geothermal flash system). Alternatively, for lower temperature geothermal resources, a second working fluid is heated by the geothermal water using a heat exchanger; it is the working fluid that drives the turbines (i.e., a geothermal binary system). Finally, because the majority of hot rock is dry, electricity can also be generated by injecting water into fractured rock to be heated (i.e., an enhanced geothermal system).80 The water is then injected back into the rock formation to create a relatively closed-loop system. Because the geothermal or injected water is an essential component of geothermal electricity generation and the size of the plants are generally smaller than 50 MW, dry cooling is becoming the standard for new geothermal facilities. Smaller power plants are generally easier to dry-cool than larger plants.

A 2008 USGS study estimated that the United States has geothermal resources sufficient to supply half of the nation's electric generation needs, assuming enhanced geothermal systems could be successfully developed and deployed at a commercial scale.81 That is, much of the geothermal potential shown on maps of geothermal resources82 requires water to be injected (and therefore consumed) to exploit the geothermal energy. Enhanced geothermal power plants require relatively little land and can be used in coproduction with enhanced oil recovery to lengthen the lifespan of oil fields.83 These enhanced systems are an emerging technology, so more research and development are needed for large-scale commercial deployment. Current research is investigating the possibility of replacing water with carbon dioxide as the working fluid, which would significantly reduce water usage and would be a means of carbon sequestration.

Acknowledgments

Ashlynn Stillwell and Kelly Twomey contributed to the writing of this report during their tenure as visiting CRS researchers.

Footnotes

1.

Thermoelectric power plants burn or react fuel to generate steam, which turns a turbine connected to a generator that produces electricity. Cooling water is used to condense the steam into boiler feed water, so the process can be repeated. See Appendix C for more information on thermoelectric cooling technologies and water use.

2.

U.S. Geological Survey, Estimated Use of Water in the United States in 2005 (Circular 1344: 2009).

3.

D. Elcock, "Future U.S. Water Consumption: The Role of Energy Production," Journal of the American Water Resources Association, vol. 46, no. 3 (June 2010), pp. 447-480, hereafter referred to as Elcock 2010.

4.

See CRS Report RS21421, Mountaintop Mining: Background on Current Controversies, by [author name scrubbed]

5.

See CRS Report R41311, The Deepwater Horizon Oil Spill: Coastal Wetland and Wildlife Impacts and Response, by [author name scrubbed] and [author name scrubbed].

6.

DOE, National Energy Technology Laboratory (NETL), Estimating Freshwater Needs to Meet Future Thermoelectric Generation Requirements (2009 Update), p. 64, http://www.netl.doe.gov/energy-analyses/pubs/2009%20Water%20Needs%20Analysis%20-%20Final%20(9-30-2009).pdf, hereafter referred to as NETL 2009.

7.

EIA, Annual Energy Outlook 2010 Early Release, Washington, DC, http://www.eia.doe.gov/oiaf/aeo/aeoref_tab.html.

8.

For more on oil shale and water rights, see CRS Report RS22986, Water Rights Related to Oil Shale Development in the Upper Colorado River Basin, by Cynthia Brougher.

9.

U.S. Department of Agriculture (USDA) Forest Service, 2000 RPA Assessment of Forest and Range Lands, FS-687, February 2001, p. 14.

10.

See U.S. Climate Change Science Program and the Subcommittee on Global Change Research, Effects of Climate Change on Energy Production and Use in the United States, Synthesis and Assessment Product 4.5, February 2008, pp. 31-32, hereafter referred to as U.S. Climate Science Program 2008.

11.

M. Hightower and S.A. Pierce, "The Energy Challenge," Nature, vol. 452, no. 7185 (March 20, 2008), pp. 285-286.

12.

Tennessee Valley Authority, "President's Report" presentation, Nov. 2010, p. 88, http://www.tva.gov/abouttva/board/pdf/11-4-2010_board_final.pdf.

13.

Ibid, p. 89.

14.

U.S. Climate Science Program 2008, p. 45, found that "hydroelectric power generation can be expected to be directly and significantly affected by climate change…with potential for production decreases in key areas such as the Columbia River Basin and Northern California." Hydroelectric generation also may decrease if dams are reoperated to maximize stored water and minimize losses to evaporation, in areas where conserving available freshwater supplies may become more critical.

15.

M. Furniss et al., Water, Climate Change and Forests: Watershed Stewardship for a Changing Climate, U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, PNW-GTR-812, Portland, OR, June 2010, http://www.fs.fed.us/pnw/pubs/pnw_gtr812.pdf, hereafter referred to as Forest Service 2010.

16.

U.S. Climate Science Program 2008, p. 38.

17.

For a discussion of data gaps related to thermoelectric power plants, see U.S. Government Accountability Office (GAO), Energy-Water Nexus: Improvements to Federal Water Use Data Would Increase Understanding of Trends in Power Plant Water Use, GAO-10-23, Oct.16, 2009.

18.

Past forecasts of national water use have proven highly inaccurate. The draft report cited below includes a graph showing a wide variation of previously projected freshwater withdrawals. It further illustrates that all but one overestimated actual water withdrawals: U.S. Army Corps of Engineers, Institute of Water Resources, Plan of Study: National Water Demand and Availability Assessment, DRAFT, Alexandria, VA, Feb. 1995, p. 7. Some recent reports, like Forest Service 2010, indicate a role for scenario-based forecasts.

19.

W. B. Solley et al., Estimated Use of Water in the United States in 1995 (USGS Circular 1200, 1998), http://water.usgs.gov/watuse/pdf1995/html/. Hereafter referred to as USGS 1998.

20.

The Forest Service 2010 water assessment is anticipated to assess the vulnerability of the coterminus United States to water supply shortages over the next 50 years, including alternative scenarios for climate change. It is not breaking out energy's water use or evaluating the sensitivity of the assessments to various policy and technology choices. For more information on this assessment, see http://www.fs.fed.us/rm/human-dimensions/staff/2010_rpa_assessment.shtml.

21.

Elcock 2010; D. Elcock, Baseline and Projected Water Demand Data for Energy and Competing Water Use Sectors, Argonne National Laboratory, Environmental Science Division, November 2008.

22.

U.S. Dept of the Interior, "Secretary Salazar Launches New Regional Climate Science Center and Water Census at Meeting of Colorado River Basin Water Leaders," press release, Oct. 20, 2010, http://www.doi.gov/news/pressreleases/Secretary-Salazar-Launches-New-Regional-Climate-Science-Center-and-Water-Census-at-Meeting-of-Colorado-River-Basin-Water-Leaders.cfm.

23.

For more information see, the Western Governors' Association, Regional Transmission Expansion Project, http://www.westgov.org/index.php?option=com_content&view=article&id=311&Itemid=81.

24.

USDA Forest Service, Past and Future Freshwater Use in the United States: A Technical Document Supporting the 2000 USDA Forest Service RPA Assessment, RMRS-GTR-39, Sept. 1999, p. 44.

25.

The extent to which increased water use for bioenergy results in a net increase in national water consumption remains the subject of debate.

26.

Calculated using data tables for Yi-Wen Chiu, Brian Walseth, and Sangwon Suh, "Water Embodied in Bioethanol in the United States," Environmental Science & Technology, vol. 43, no. 8 (2009), pp. 2688-2692, hereafter referred to as Chiu 2009; and Kansas Department of Agriculture, Division of Water Resources, Water Use in Kansas, http://www.ksda.gov/appropriation/content/116. Insufficient data are available to analyze more local effects on water use (e.g., county level water use). Chiu 2010 includes water used for irrigation and for converting the feedstock into fuel; it does not include precipitation, soil moisture, and other water indirectly consumed by the feedstock.

27.

Forest Service 2010, pp. 15-16, and 24.

28.

Ibid.

29.

DOE, 20% Wind Energy by 2030: Increasing Wind Energy's Contribution to U.S. Electricity Supply, July 2008, p. 185, http://www1.eere.energy.gov/windandhydro/pdfs/41869.pdf, hereafter referred to as DOE 2008. In the report, the Midwest/Great Plains region included Illinois, Indiana, Iowa, Kansas, Michigan, Minnesota, Missouri, Nebraska, North Dakota, Ohio, Oklahoma, South Dakota, Texas, and Wisconsin.

30.

EIA, Table 1.1, Net Generation by Energy Source, http://www.eia.gov/cneaf/electricity/epm/table1_1.html.

31.

For more on carbon capture, see CRS Report R41325, Carbon Capture: A Technology Assessment, by [author name scrubbed]

32.

NETL 2009, p. 64.

33.

USGS 1998, p. 54.

34.

NREL 2003.

35.

The NREL 2003 report included data on the average water consumption per unit of hydroelectric generation by state; the water consumption intensity for the hydroelectric produced at these facilities, according to the study, can vary from a low of 2,000 gallons/megawatt-hour (MWh)(Nebraska) to a high of 154,000 gallons/MWh (Kentucky). The report calculated the weighted average rate of water consumption per MWh at 18,000 gallons, with the variation in the rates across states being significant; the report calculated the national weighted average for thermoelectric generation at 470 gal/MWh.

36.

DOE, Office of Fossil Energy, Modern Shale Gas Development in the United States: A Primer, April 2009, p. ES-2, http://www.netl.doe.gov/technologies/oil-gas/publications/EPreports/Shale_Gas_Primer_2009.pdf.

37.

Ibid, p. 64. An Army Corps of Engineers draft report put the lower end of water use at 0.8 million gallons, with the lower end dominated by the shorter vertical wells. U.S. Army Corps of Engineers, Omaha District, Garrison/Lake Sakakawea Project, North Dakota, Draft Surplus Water Report, Omaha, NE, Dec. 2010, p 3-2.

38.

M. Mantell, "Abundant, Affordable, and Surprisingly Water Efficient," presented at 2009 GWCP Water/Energy Sustainability Symposium in Salt Lake City, September 13-16, 2009, available at http://www.energyindepth.org/wp-content/uploads/2009/03/MMantell_GWPC_Water_Energy_Paper_Final.pdf; and EIA, Average Heat Rates by Prime Mover and Energy Source, January 2010, http://www.eia.doe.gov/cneaf/electricity/epa/epat5p4.html.

39.

DOE, Energy Demands on Water Resources: Report to Congress on the Interdependency of Energy and Water, Dec. 2006, http://www.sandia.gov/energy-water/docs/121-RptToCongress-EWwEIAcomments-FINAL.pdf, hereafter referred to as DOE 2006.

40.

L. P. Galusky, An Update and Prognosis on the Use of Fresh Water Resources in the Development of Fort Worth Basin Barnett Shale Natural Gas Reserves, Texerra Engineering, prepared for Barnett Shale Education Council and Barnett Shale Water Conservation and Management Committee, Midland, TX, Nov. 4, 2009.

41.

Ibid.

42.

C.J. Vavra, "Desalination of Oil Brine," presentation, http://www.pe.tamu.edu/gpri-new/home/BrineDesal/MembraneWkshpAug06/Burnett8-06.pdf

43.

CRS Report R40631, Water Issues of Concentrating Solar Power (CSP) Electricity in the U.S. Southwest, by [author name scrubbed] and [author name scrubbed].

44.

Ibid.

45.

Dish engine CSP facilities employ engines instead of steam turbines. Mirrors concentrate sunlight to produce heat in a gas chamber connected to a piston and drive shaft. The drive shaft powers an electricity generator. Because of the high operating temperature and high efficiency of the motor, air cooling can be used with little compromise of overall electricity generation efficiency. This significantly reduces the water used to generate electricity compared to other CSP technologies. One dish engine facility with a capacity of 2 MW was put into operation in 2010 in Arizona; dish engine facilities of 750 MW and 850 MW are under development in southern California.

46.

This section on biofuels was written by [author name scrubbed], Analyst in Agricultural Conservation and Natural Resources Policy, Resources, Science and Industry Division ([phone number scrubbed]).

47.

For more on and a map of the aquifer, see V. L. McGuire, Changes in Water Levels and Storage in the High Plains Aquifer, Predevelopment to 2005, USGS, USGS Face Sheet 2007-3029, 2007, http://pubs.usgs.gov/fs/2007/3029/.

48.

Calculated using supplementary data tables from Chiu 2009, and City of Fort Collins, Water Supply and Demand, Fort Collins, CO, http://www.fcgov.com/water/supply.php.

49.

S. E. Powers, R. Domingues-Faus, and P. J. J. Alvarez, "The Water Footprint of Biofuel Production in the USA," Biofuels, vol. 1, no. 2 (2010), pp. 255-260.

50.

GAO, Energy Water Nexus: Many Uncertainties Remain about National and Regional Effects of Increased Biofuel Production on Water Resources (GAO 10-116, Nov. 2009), p. 10. Agricultural runoff with excess nutrients from fertilizers used in the Mississippi River basin contributes significantly to hypoxic "dead zones" in the Gulf of Mexico. For more information on dead zones, see CRS Report 98-869, Marine Dead Zones: Understanding the Problem, by [author name scrubbed].

51.

C.W. King,, M. E. Webber, and I.J. Duncan, "The Water Needs for LDV Transportation in the United States," Energy Policy, vol. 38 (2010), p. 1161, hereafter referred to as King 2010.

52.

In particular, the renewable fuels standard (RFS), a major federal incentive established in the Energy Independence and Security Act of 2007 (EISA, P.L. 110-140), establishes a goal of 36 billion gallons of biofuel production by 2022, including 16 billion gallons of cellulosic biofuels. For more information on the RFS, see CRS Report R40155, Renewable Fuel Standard (RFS): Overview and Issues. Also, the Food, Conservation, and Energy Act of 2008 (the 2008 farm bill, P.L. 110-246) supports the growth of the cellulosic industry through research programs, grants, loans, and tax credits. For more information on energy provisions in the 2008 farm bill, see CRS Report RL34130, Renewable Energy Programs in the 2008 Farm Bill, by [author name scrubbed].

53.

K.R. Fingerman et al., "Accounting for the Water Impacts of Ethanol Production," Environmental Resources. Letters, vol. 5 (2010), http://iopscience.iop.org/1748-9326/5/1/014020/pdf/1748-9326_5_1_014020.pdf. Others also have raised concerns that large-scale deployment of open pond algae systems in arid areas may have a freshwater footprint if impaired waters are not used (C. Harto, R. Meyers, and E. Williams, "Life Cycle Water Use of Low-Carbon Transport Fuels," Energy Policy, vol. 38 (2010), pp. 4933-4944).

54.

For more information, see CRS Report R41460, Cellulosic Ethanol: Feedstocks, Conversion Technologies, Economics, and Policy Options, by [author name scrubbed].

55.

For example, dry cooling is not equally effective for power plant cooling in locations with temperatures above 100°F, or substituting municipal wastewater may not be an option for remote facilities.

56.

J. Leshy, "Notes on a Progressive National Water Policy," Harvard Law & Policy Review, vol. 3, no. 1 (Winter 2009), pp. 133-159.

57.

D. H. Getches, "The Metamorphosis of Western Water Policy: Have Federal Laws and Local Decisions Eclipsed the States' Role?," Stanford Environmental Law Journal, vol. 20 (2001), pp. 3-72.

58.

For more on rare minerals in the energy sector, CRS Report R41347, Rare Earth Elements: The Global Supply Chain, by [author name scrubbed].

59.

Elcock 2010.

60.

Elcock 2010 considered that only energy crops would generate an increase in water consumption. The study's projections for water consumption were based on projections for different biofuels, including corn-based ethanol, cellulosic ethanol, and biodiesel.

61.

King 2010, p. 1162.

62.

NETL, Estimating Freshwater Needs to Meet Future Thermoelectric Generation Requirements, 2007.

63.

Elcock 2010, p. 451. For more, see CRS Report RL34738, Cellulosic Biofuels: Analysis of Policy Issues for Congress, by [author name scrubbed] et al.

64.

Argonne National Laboratory released for comment the following report: ANL, DRAFT Water Use in the Development and Operation of Geothermal Power Plants, September 2010, http://www1.eere.energy.gov/geothermal/pdfs/geothermal_water_use_draft.pdf, hereafter referred to as Argonne 2010. The draft links its geothermal water use findings with water intensities of other electricity generation. The report cited references from the early 1990s for fuel processing, and those references cited materials from the late 1970s to the early 1990s. Other articles also use data from these sources (e.g., V. Fthenakis and H.C. Kim, "Life-cycle Uses of Water in U.S. Electricity Generation," Renewable and Sustainable Energy Reviews, vol. 14 (2010), pp. 2039-2048). Continued reliance on older sources demonstrates a knowledge gap on current water use in fuel acquisition and preparation. Changes in the U.S. fossil fuel practices (e.g., natural gas extraction through fracturing) in recent decades may have significantly altered water use for fuel.

65.

Chemicals added to the water at a thermoelectric facility to extend equipment life and improve operational efficiency (e.g., demineralize regenerants and rinses to prevent biological growth) can degrade water quality when discharged into the environment. To comply with water quality regulations promulgated under the Clean Water Act, thermoelectric facilities constructed after January 17, 2002, generally use evaporative cooling. EPA has begun revising these rules, which were issued in 1982. Separately under the Clean Water Act, EPA regulates cooling water intake structures, which protect fish from entrainment at the intake point. EPA is developing a rule to address water intake structures for some existing thermoelectric facilities, which is expected to be proposed in 2011; the rule may affect decisions about power plan retirements and cooling technology.

66.

DOE, Concentrating Solar Power Commercial Application Study: Reducing Water Consumption of Concentrating Solar Power Electricity Generation, no date,: http://www1.eere.energy.gov/solar/pdfs/csp_water_study.pdf.

67.

The Hewlett Foundation and The Energy Foundation, The Last Straw: Water Use by Power Plants in the Arid West, April 2003, pg. 12, http://www.catf.us/publications/reports/The_Last_Straw.pdf. Another source estimates that dry cooling and hybrid wet-dry cooling have capital costs 1.1 to 5 times higher than wet cooling (California Energy Commission, Comparison of Alternate Cooling Technologies for California Power Plants: Economic, Environmental and Other Tradeoffs, Consultant Report 500-02-079F, Sacramento, CA, Feb. 2002, p. 1-9, http://www.energy.ca.gov/reports/2002-07-09_500-02-079F.PDF). This same source provides an example of the cooling system capital costs for a 500 MW combined-cycle power plant ─ $3.6 million for a wet cooling tower versus $25.5 million for a dry cooling system (ibid., p. 5-16 and p. 5-39).

68.

Turchi, C.S., M.J. Wagner, and C.F. Kutscher, Water Use in Parabolic Trough Power Plants: Summary Results from WorleyParsons' Analyses, NREL, Golden, CA, Dec. 2010, http://www.nrel.gov/docs/fy11osti/49468.pdf. See also, letter from Ric O'Connell, Renewable Energy Consultant, Black & Veatch, to Environmental Working Group, Renewable Energy Transmission Initiative, June 25, 2008, which found a 10% increase in the cost of electricity.

69.

The loss in generation efficiency is from insufficient cooling of the turbine exhaust steam, increasing steam turbine back pressure. While efficiency losses also are typical of wet-cooled systems when inlet water temperatures exceed design temperatures, the lower cooling capacity of air versus water makes dry cooling more sensitive to temperature changes and efficiency losses than wet cooling. A power plant with dry cooling can experience a 1% loss in efficiency for each 1°F increase of the condenser, which is limited by ambient temperatures (C. Kutscher, A. Buys, and C. Gladden, Hybrid Wet/Dry Cooling for Power Plants, NREL, presented at Parabolic Trough Technology Workshop, Incline Village, NV, Feb. 14, 2006, http://www.nrel.gov/docs/fy06osti/40026.pdf.). Electricity output is also decreased by the additional electricity requirement of running the fans and pumps of the air cooling system.

70.

Turchi, C.S., M.J. Wagner, and C.F. Kutscher, Water Use in Parabolic Trough Power Plants: Summary Results from WorleyParsons' Analyses, NREL, Golden, CA, Dec. 2010.

71.

While there is interest in using alternative water sources such as coastal waters for cooling, there is concern about harm to marine ecosystems.

72.

For example, the Palo Verde Nuclear Generating Station near Phoenix, AZ, uses wastewater effluent for cooling.

73.

D. Lawrence et al., Power Plant Engineering – Design and Construction, (Black & Veatch, Chapman & Hall: New York, 1996).

74.

J. A. Veil., J. M. Kupar, and M. G. Puder, Argonne National Laboratory, Use of Mine Pool Water for Power Plant Cooling, September 2003, http://www.ipd.anl.gov/anlpubs/2006/11/57830.pdf.

75.

Whether hydroelectric power generation is a renewable is a subject of debate largely because of the environmental impacts of dams and their reservoirs. For more information on small-scale and low-head hydropower, see CRS Report R41089, Small Hydro and Low-Head Hydro Power Technologies and Prospects, by [author name scrubbed].

76.

EPRI, Assessment of Waterpower Potential and Development Needs (Palo Alto, CA: 2007), http://mydocs.epri.com/docs/public/000000000001014762.pdf.

77.

Idaho National Laboratory, Feasibility Assessment of the Water Energy Resources of the United States for New Low Power and Small Hydro Classes of Hydroelectric Plants, (DOE, Washington, DC: 2006), http://hydropower.inel.gov/resourceassessment/pdfs/main_report_appendix_a_final.pdf. This study estimated preliminarily feasible opportunities for increasing U.S. hydroelectric generation with a total potential of 30 MW.

78.

DOE, National Electric Transmission Congestion Study, December 2009, http://congestion09.anl.gov/documents/docs/Congestion_Study_2009.pdf, presents areas where renewable energy development using existing technologies is constrained by transmission, and other areas where development would be constrained if technologies mature (e.g., offshore wind). The areas renewable energy transmission constrained areas are shown in the report on page 23.

79.

Intermittent electricity sources can be used to meet electricity demand for activities that can be ramped up or down (e.g., hydrogen generation via electrolysis, though this technology is still developing commercially) and to reduce generation from other sources when they are available.

80.

DOE, How an Enhanced Geothermal System Works, Washington, DC, March 31, 2006, http://www1.eere.energy.gov/geothermal/printable_versions/egs_animation.html

81.

USGS, Substantial Power Generation from Domestic Geothermal Resources, Reston, VA, Sept. 29, 2008, http://www.usgs.gov/newsroom/article.asp?ID=2027&from=rss_home, pg. 5.

82.

For examples of a geothermal potential map, see the following websites: http://www.nrel.gov/gis/images/geothermal_resource2009-final.jpg, and http://www.azgs.state.az.us/images/geothermal_6b.jpg.

83.

B.D. Green and G. Nix, Geothermal - Energy Under Our Feet, NREL, NREL/TP-840-40665, Nov. 2008.