What is the True Cost of Hydraulic Fracturing? Incorporating Negative Externalities into the Cost of America’s Latest Energy Alternative. Katie Phillips Environmental Science Program, Appalachian State University, Boone, NC [email protected] Abstract Decreased technological costs and increased efficiency of horizontal drilling has made obtaining natural gas from shale deposits through hydraulic fracturing a viable economic option. However, current estimates of per kWh costs to obtain natural gas through this method do not account for increased environmental risks. By incorporating damages from air and water pollution, the true cost of hydraulic fracturing can be assessed. Results indicate air pollution from volatile organic compounds (VOCs) is higher for unconventional natural gas versus conventional natural gas. Without potential water pollution taken into account, the best estimate levelized cost of electricity for unconventional natural gas is $13.99/kWh, $1.87/kWh lower than that of conventional natural gas and $0.80/kWh higher than the best estimate for wind energy. Difference in cost between conventional and unconventional natural gas is largely due to funds spent procuring and protecting natural gas from other countries. The water pollution externality is estimated by comparing the total cost of replacing the water of all of the citizens in the water basin overlying the shale play to the total possible number of kWh energy that could be extracted from that shale for five shale plays. Replacement of water for 10 years results in an externality larger than the security cost for the Eagle Ford shale, and about half of the security cost for the Marcellus and Barnett shales. The water externality for the same period is smaller than the security externality for the Fayetteville and Green River shales. More studies are needed to determine the cause of the excess air pollution and to limit the range of water externalities. 1.0 Introduction Shale gas, also referred to as unconventional natural gas, is natural gas stored in shale deposits [1]. Shale has an extremely low permeability (about 1 microdarcy versus 1000 microdarcy of typical conventional natural gas storage rocks), which, until recently, prevented large scale natural gas extraction [2]. Advancements in horizontal drilling technology, in combination with hydraulic fracturing, have made shale gas production a viable option [3]. To extract natural gas from shale, wells are drilled vertically to the depth of the shale deposit. From there, horizontal drills are used to increase access to the shale. High-pressure injection of water and chemicals is then used to hydraulically fracture the rock, increasing the 40 permeability of the shale [3]. Both methods have been used in oil and gas extraction for many years, but decreased technological costs, waning conventional natural gas reserves, and increased oil prices have driven a shale boom over the last few years [4]. Shale gas deposits exist all over the Earth [3]; it is estimated that the United States has 1,836 trillion cubic feet of recoverable natural gas, possibly enough to supply our energy needs for the next hundred years [5]. Natural gas also produces less greenhouse gas emissions than coal [6]. Replacing coal and imported natural gas with domestic natural gas could reduce our greenhouse gas emissions from energy production and fuel transport, respectively. However, other environmental concerns Journal of Student Research in Environmental Science at Appalachian PR O O F #2 have dampened enthusiasm for increased unconventional natural gas production. Enormous amounts of water are needed in hydraulic fracturing, and much of that water flows back to the surface or requires treatment before it can be reinjected into the subsurface [2]. Most states do not require companies to report what chemicals are used in their drilling processes, raising questions about the potential for chemical contamination of soil and groundwater. Recent work has indicated higher levels of air contaminants surrounding hydraulic fracturing systems than is usually found in conventional gas fields [7,8]. In addition, there is the concern that increased unconventional natural gas production will take away from renewable energy exploitation, further delaying the inevitable switch from nonrenewable resources [9]. In order to properly assess the potential benefits and costs of increased hydraulic fracturing, negative externalities to production such as government subsidies, environmental remediation efforts, and health care costs that are eventually paid for by the taxpayers should be incorporated into the calculation of the true cost per kWh of energy for comparison to different forms of alternative energy (wind, solar, coal, biomass, etc.). Until now, unconventional and conventional natural gas costs have been lumped together. However, increased environmental concerns indicate that there may be a significant difference between the true cost of natural gas derived through conventional and unconventional means. Using a method developed by Roth and Ambs (2004) [10], with additional parameters for water externalities, the real cost of unconventional natural gas was assessed and compared with the levelized cost of wind power. (see Table 1 for nomenclature). Different types of power plants have different levels of efficiency and environmental externalities. For the purposes of this study, both types of natural gas - unconventional and conventional – are assumed to have been fired in an Advanced Combined Cycle facility, which has the lowest levelized cost of energy of any natural gas burning power plant, according to Roth and Amb’s [10]. The fixed charge rate (12%), discount rate (5.5%), and operations and maintenance levelization factor (0.3865 for gas and 0.199 for wind) were obtained from Roth and Ambs [10]. Other plant parameters can be found in Table 2. Externality costs were determined using the Roth and Ambs’s [10] formula: XC=DC*EF*C1*HR*C2 (3) Table 1. Variable Definitions, Equation 2. Variable Definition LCOE Levelized cost of energy, $/kWh FCR Fixed charge rate, % PC Plant cost, $/kWyear HY Hours per year, 8760 hr/yr CF Capacity factor, % OLF Operations and maintenance levelization factor, % FOM Fixed operations and maintenance cost, $/kWyear VOM Variable operations and maintenance cost, $/kW FLF Fuel levelization factor, % FC Fuel cost, $/MMBtu HR Heat rate, Btu/kWh XC Externality cost, $/kWh e Escalation rate, % r Real discount rate, % The levelized cost of energy (LCOE) was determined using a formula developed by the California Energy Commission [11] : PL Plant life, years n Percentage NOx removed via scrubbing, % p Percentage particulate matter removed by scrubbing, % LCOE= [FCR*PC/HY/CF]+ [OLF*(FOM/HY/CF+VOM)]+ [FLF*FC*HR]+XC where FLF is defined as: DC Damage cost, $/tonpollutant EF Emission factor, lbpollutant/MMBtu C1 Conversion factor, 1 ton/2000 lbs C2 Conversion factor, 106 MMBtu/Btu C3 Conversion factor, 1 lb/ 453.59 g 2.0 Methods FLF=[r*(1+r)PL/((1+r)PL-1)] * (1+e)/(r-e) * [1-[(1+e)/(1+r)]PL] (1) (2) Volume 2, 1st Edition • Spring 2012 41 PR O O F #2 Table 2. Plant Parameters Obtained from the EIA Annual Energy Outlook 2011 Advanced Combined Cycle (Natural Gas) Plant Cost ($) Capacity Factor (%) Table 3. Externality Damage Costs for Air Pollution Utility Scale Wind Turbine $1003 $2438 0.87 0.34 Levelization Factor (%) 0.3865 0.199 Fixed Operating and $14.62 Maintenance Cost ($/ kWyear) $28.07 Variable Operating $3.11 and Maintenance Cost ($/kWh) $0 Fuel Cost ($/MMBtu) 0.0395* $0 Heat Rate (Btu/kWh) 6430 n/a Lower Range ($/ton) Best Estimate ($/ton) Upper Range ($/ton) CO2 13.36 35.63 56.14 CO 683.17 1424.93 3366.07 SO2 2207.80 2523.31 6658.56 NOX 1416.02 10686.95 13536.80 PM 4222.06 6530.92 18375.61 VOC 1502.10 7106.33 8757.35 Petron et al. [8] found increased levels of VOCs in areas where hydraulic fracturing had occurred. Using data from their study, the amount of each VOC (recorded in ppm) was converted to lb/MMBtu VOC (see Table 5). The conversion for ppm to lb/MMBtu used is: For greenhouse gas emissions, a global warming potential (GWP) term was multiplied to the formula above [10]. XC=DC*EF*C1*HR*C2*GWP (4) One-hundred-year IPCC global warming potentials were used for CO2 and N2O [12]. One-hundred-year global warming potentials for CO and CH4 were taken from Shindell et al. (2009) [13]. Additional terms were added to compensate for technology that can remove NOx and particulate matter in Advanced Combined Cycle facilities [10]: XC=[DC*EF*(1-n)]NOx * C1 * HR * C2 (5) XC=[DC*EF*(1-p)]PM * C1 * HR * C2 (6) Damage costs for externalities were taken from Roth and Ambs [10], but updated from 1999 to 2010 dollars (see Table 3). With the exception of CH4 and volatile organic compounds (VOCs), emission factors were also taken from Roth and Ambs [10]. Howarth et al. [14] found fugitive CH4 emissions to be 30% to 50% higher over the lifetime of an unconventional shale well as opposed to a conventional gas well. To incorporate this finding, unconventional natural gas was given a CH4 emission factor 30% higher than conventional natural gas (see Table 4). 42 Pollutant lb/MMBtu = ppmmeasured * [(21-0)/(21-%O2 measured)] * (MW)* Fd /VM (7) where VM is molar volume (385 dscf/mol), Fd is the ratio of the volume of dry flue gas to the heat of the fuel (8,710 dscf/MMBtu), and MW is the molecular weight of the VOC [15]. Increased VOCs could be due to exposed produced water or the well drilling process. Air samples were taken from the surrounding area, not directly from flue gas, so the percentage of O2 was ignored, leaving the formula: lb/MMBtu = ppmmeasured * (MW)* Fd /VM (8) The lb/MMBtu for each VOC was calculated and added together to give a total VOC emission factor. The VOC emission factor for unconventional shale gas was altered appropriately. All other air pollutant emission factors were obtained from Roth and Ambs [10]. Roth and Ambs [10] noted three other externalities for natural gas production: energy supply, energy depletion, and energy loss due to distributed production. Energy supply or energy security cost is a valuation determined by Coiante and Barra [16] of the military cost per kWh to obtain, protect, and transport fuel from overseas. The energy depletion externality is the cost of depleting finite resources per kWh Journal of Student Research in Environmental Science at Appalachian PR O O F #2 Table 4. Emission Factors and Global Warming Potentials for Natural Gas Global Warming Potential Pollutant Conventional Natural Gas Unconventional Natural Gas Low Best High CO2 117 117 1 1 1 CH4 0.0169 0.01352 26 34 41 N2O 0.00018 0.00018 320 320 320 Upstream 24.5 24.5 1 1 1 CO 0.082 0.082 3 5 7.5 SO2 0.00058 0.00058 - - - NOx 0.4 0.4 - - - PM 0.0066 0.0066 - - - VOC 0.0066 0.30633 - - - Table 5. Total VOC from Petron et al. Converted from ppm to lb/MMBtu. Chemical lb/MMBtu Ethane 7.50 x 10-2 Propane 8.80 x 10-2 n-Butane 5.80 x 10-2 i-Butane 2.32 x 10-2 n-Pentane 2.52 x 10-2 i-Pentane 2.16 x 10-2 n-Hexane 4.30 x 10-3 n-Heptane 2.50 x 10-3 Cyclopentane 1.05 x 10-3 n-Octane 5.70 x 10-4 n-Nonane 3.20 x 10-4 n-Decane 2.13 x 10-4 n-Undecane 1.56 x 10-4 Toluene 1.38 x 10-3 Benzene 1.17 x 10-3 m&p-Xylenes 5.30 x 10-4 o-Xylene 2.65 x 10-4 Benzene_1ethyl 2.12 x 10-4 Benzene_135trimethyl 5.99 x 10-5 Ethene 1.12 x 10-3 Propene 2.10 x 10-4 Styrene 4.68 x 10-5 Isoprene 1.70 x 10-5 Ethyne 1.30 x 10-3 Total 3.06 x 10-1 [17]. The distribution externality is a valuation of downstream emissions and energy loss due to transport of energy to consumers over large distances [18]. Assuming all unconventional natural gas used in the U.S. would be produced in the U.S., the energy security externality was removed from the unconventional natural gas cost. All of the values for these externalities were obtained from Roth and Ambs [10] and updated to 2010 dollars. For wind production, only the distribution externality was applied. Another externality, labeled “other”, incorporates land, visual impact, and noise externalities associated with wind [19]. 2.1 Water Externality The amount of money to buy extra water for hydraulic fracturing is negligible per kWh of unconventional natural gas extracted. However, the threat that leaky cement casings and unknown fractures in the shale pose to surrounding water supplies needs to be accounted for. To estimate possible water damage, the amount of technically recoverable resources for five shale plays (the Marcellus, Eagle Ford, Fayetteville, Green River, and Barnett) was obtained from the EIA [20] (except the Marcellus shale, which was obtained from EIA [21]) and compared to the amount of water that could be polluted and would have to be replaced. Since the amount of water in most aquifers is not known, the water pollution externality was estimated by comparing the total cost of replacing the water of all of the citizens in the water basin overlying the shale play to the total possible Volume 2, 1st Edition • Spring 2012 43 PR O O F #2 Table 6. Lower, Best Estimate and Upper Values for Other Externalities, in ¢/kWh Conventional Natural Gas Unconventional Natural Gas Utility Scale Wind Turbine Low Best Upper Low Best Upper Low Best Upper Energy Security Supply 2.481 2.553 5.341 - - - - - - Energy Security Depletion 0.769 1.543 3.090 0.769 1.543 3.090 - - - Distribution 0.945 2.699 9.447 0.945 2.699 9.447 0.9447 2.699 9.447 - - - - - - 0.1184 0.1754 0.1754 Other number of kWh energy that could be extracted from that shale for five shale plays. Population estimates for the Marcellus shale and the Eagle Ford shale were obtained from Arthur et al. [22] and the National Wildlife Federation [23], respectively. For the other shale plays, water basin populations were estimated using county data from the U.S. Census Bureau [24], which was then multiplied by the average number of gallons of water used per year per person in the U.S. and the average cost of the water per gallon [25]. The number of years the water would need to be replaced before the pollution was remediated was given a base estimate of ten years. tance traveled roundtrip by trucks to adjoining water basins for all the shale plays investigated was 300 miles. The price per gallon of diesel was estimated based on current diesel costs at $4.00. The gallons of H2O per truck was estimated based on an 18-wheel transfer truck carrying capacity of 44,000 lbs., divided by the number of lbs. per gallon of water for 5282.11 lb. H2O/per truck, which corroborates well with Chesapeake Energy’s 2008 estimate of truck water carrying capacity of 5,040 - 6,300 gallons of water per truck. Other variables used in the water externality equation are shown in Table 7. Table 7. Water Externality Variable Values $H2O replacement=(# of people)* (gal H2O/person/year)* ($H2O/gal)*year kWh=tcf gas * (1000 bcf/1 tcf )* (1.03 x 109 Btu/1 bcf) * (1012 Btu/ 1.03 x 109 Btu)* (1kWh/3413 Btu) (9) Variable Value lb diesel/gal 7.3 gal diesel/mil 0.2 lb/truckload 44000 gal H20/(person*year) 32850 lb/gal water 8.33 (10) The ten-year water replacement cost only includes the cost of the water, not the cost of transporting it from another water basin. To estimate the cost of transport, a second equation was used: Diesel combustion produces CO2, CH4, and N2O. To account for the additional greenhouse gas emissions, the following equations were used: $ Transport=(miles/truck)* (11) (gal diesel/mile)* ($/gal diesel)* (gal H2O per year/gal H2O per truck)* years The number of miles from the center of the Marcellus shale to the nearest unaffiliated water basin is 150 miles. Trucks transporting water would therefore travel 300 miles to deliver water to this location. For the sake of comparison, the dis44 $ CO2=gal diesel* (lb CO2/gal diesel)* DC* C1 (12) $ CH4=(g CH4/lb diesel)* (13) (gal H2O per year/gal H2O per truck)* years*(miles/truck)*DC*GWP*C1*C2* ($/gal diesel)*(lb diesel/gal) Journal of Student Research in Environmental Science at Appalachian PR O O F #2 $ N2O=(g N2O/lb diesel)* (14) (gal H2O per year/gal H2O per truck)* years*(miles/truck)*DC*GWP*C1*C2* ($/gal diesel)*(lb diesel/gal) Emission factors for diesel fuel were obtained from the EPA (2007) [26]. A water externality estimate was calculated by adding the replacement, transport, and greenhouse gas costs together and dividing by the total number of kWh energy the shale play could produce. The number of years of water replacement needed for the total cost of replacing the water to equal the total profit that could be obtained extracting the natural gas was also determined. The profit per kWh of natural gas was estimated to be $ 0.04/kWh by subtracting the levelized cost of electricity without externalities ($ 0.058/ kWh) from the average retail price of electricity per kWh ($ 0.098/kWh [19]). It was then multiplied by the number of kWh of energy the shale play could produce to determine the total potential profit of each play. 2.2 Unquantified Externalities Studies have shown that injecting hydraulic fracturing water into the ground can cause earthquakes; however, there has been no reported damage related to these earthquakes [27]. Increased cancer risk due to air pollution is also an issue, but is highly variable and dependent upon proximity to a well [28]. In addition, federal and state subsidies are also part of the true cost of the electricity. These externalities are noted but not quantified in this study. 3.0 Results and Discussion Based on the Petron (2012) [8] study, the emission factor for volatile organic compounds from unconventional shale gas extraction is more than 145 times higher than that for conventional gas (0.30633 lb/MMBtu vs. 0.0021 lb/MMBtu). Associated best estimate externality costs vary from 0.0048 ¢/kWh (emission factor of 0.0021 lb/MMBtu) to 0.700 ¢/kWh (emission factor of 0.30633 lb/MMBtu). Levelized costs of unconventional natural gas without incorporating the water externality vary from 8.83 – 25.36 $/ kWh, while levelized costs of conventional natural gas vary from 11.16 – 29.84 Table 8. Levelized Cost of Energy for Conventional, Unconventional and Wind Power Without Water Externality. Conventional Unconventional Natural Gas Natural Gas Wind Best Estimate ($/kWh) 15.86 13.99 13.19 Lower ($/kWh) 11.16 8.827 11.58 Upper ($/kWh) 29.63 25.14 19.94 $/ kWh (see Table 8). All estimates for the levelized cost of electricity are lower for wind than conventional natural gas, but the lower range of wind energy cost is more than that of unconventional natural gas. Water externalities vary between shale plays due to differences in the ratio between the possible amount of energy that could be extracted from the shale play and the number of people dependent upon connected water supplies. Costs for water replacement alone are substantially lower than costs due to water transport and greenhouse gas externalities from burning diesel. Water externalities, including replacement, transport, and greenhouse gas emission costs, with an assumption of 10 years of water replacement, vary from 0.100 ¢/kWh in the Fayetteville shale to 4.167 ¢/kWh in the Eagle Ford shale play. With a value of 10 years of water replacement, the water externality for the Eagle Ford shale play is larger than the conventional gas security externality, but is smaller in the other four shale plays. The number of years for the water externality to equal the conventional natural gas security externality varies from 6.47 to 250. The number of years for the price of replacing the water to equal the profits gained from the energy extraction ranges from 9.60 to 371 years (see Table 9). Increases in air pollution externalities (methane and volatile organic compounds) for unconventional natural gas are not equal to the security cost of securing and purchasing conventional natural gas abroad. However, the cost of replacing polluted water for ten to twenty years could equal or exceed the cost of energy security in most shale plays. The data show a large gap between the Marcellus, Barnett, and Eagle Ford shale plays that are all heavily populated and Volume 2, 1st Edition • Spring 2012 45 PR O O F #2 Table 9. Estimated Water Externality by Shale Play Marcellus Barnett Green River Eagle Ford Fayetteville 141 43 4 21 32 Total Profit ($) 1.412 x 1012 5.191 x 1011 4.829 x 1010 2.535 x 1011 3.863 x 1011 Population 2 .000 x 107 1.000 x 107 6.028 x 104 1.200 x 107 4.734 x 105 Replacement ($) 1.314 x 1010 6.570 x 109 3.961 x 107 7.884 x 109 3.110 x 108 Transport ($) 2.985 x 1011 1.493 x 1011 8.998 x 108 1.791 x 1011 7.065 x 109 Air Pollution ($) 1.284 x 1011 6.422 x 1010 3.872 x 108 7.707 x 1010 3.040 x 109 $ water damage/kWh (10 year estimate) 1.246 1.696 0.110 4.167 0.108 Years for water externality = security externality 28.08 15.92 245.6 6.478 250.2 Years water damage = profit 41.61 23.59 364.0 9.600 370.8 Technically recoverable gas (tcf ) have large water externalities versus the Green River and Fayetteville shale plays, which have small populations and small water externalities. 4.0 Conclusion To more accurately estimate the water pollution associated with unconventional shale gas, the amount of water in nearby basins would need to be approximated and the amount of additional water stress to surrounding aquifers incorporated. Water stress due to hydraulic fracturing itself may already be problematic in some areas, so water stress due to the need for replacement from adjoining aquifers may be substantial. Contaminant flow models of each shale play may also aid in determining potential costs of water pollution. By determining the amount of dispersal chemicals hydraulic fracturing fluid could possibly attain, the amount of fluid that could be pumped into the subsurface without causing tremendous damage due to leaking could be assessed. Obtaining better estimates of the amount of recoverable shale gas is also key to determining the relative weight of potential water pollution costs to potential energy gains. In the EIA’s Annual Energy Outlook Early Release 2012 [21], the amount of technically recoverable cubic feet of natural gas dropped in the Marcellus shale from 410 tcf to 141 tcf. Such differences create large changes in the ratio of potential profits to potential water losses. It would take 81.7 years of water replacement to equal the conventional security externality in the Marcellus shale, if the shale could produce 410 tcf versus 28.08 years 46 with 141 tcf of recoverable gas. Research on the source of the increased volatile organic compound levels is needed. Increased methane from hydraulic fracturing wells is due to leaks and flowback, but where the excess volatile organic compounds originate is unknown. Is it a result of evaporation of hydraulic fluid during flow back or treatment? Or is it a property of the shale itself? Unless the excess air pollution is solely due to shale play geochemistry, taking air quality samples is unlikely to solve this issue. Hydraulic fracturing fluids vary in formula from company to company and likely from shale to shale. Only by combining shale geochemistry and hydraulic fracturing fluid data can a likely cause of the air pollution be determined and a remediation solution proposed. Although renewable energy costs more per kWh when externalities are not considered, the best estimate levelized cost of wind is less than that of conventional or unconventional natural gas with and without water externality considerations. Policy makers should consider levelized energy costs when making value assessments of unconventional natural gas. When externalities are considered, short- and long-term costs of wind energy are less than that of conventional natural gas. Like unconventional natural gas, wind energy does not need to be secured abroad, but wind energy also has negligible air and water pollution concerns without any worry of increased prices due to energy depletion. Although not available everywhere, wind power is not currently being used to its full potential. In allocating subsidies and zoning per- Journal of Student Research in Environmental Science at Appalachian PR O O F #2 mits, lawmakers should take into consideration the full cost of energy technology, not just the price on an electric bill. This can be done by creating a polluter-pays-system or by simply acknowledging taxpayer cost for pollution externalities. The security cost of obtaining conventional natural gas is large, but the water externality cost may be larger still. More studies are needed to determine potential environmental harm of large scale hydraulic fracturing and horizontal drilling before implementing any more largescale unconventional shale gas extraction projects. References [1] U.S. Department of Energy and the National Energy Technology Laboratory (2011), Shale Gas: Applying Technology to Solve America’s Energy Challenges, http://www. netl.doe.gov/technologies/oil-gas/publications/brochures/Shale_Gas_March_2011. pdf. [2]Stephenson, T., J. E. Valle, and X. Riera-Palou (2011), Modeling the relative GHG emissions of conventional and shale gas production, Environ. Sci. Tech., 45, 10757-10764, dx.doi.org/10.1021/es2024115. [3] Sakmar, S. L. (2011), The global shale gas initiative: will the United States be the role model for the development of shale gas around the world?, Houston Journal of International Law, 33(2),369-416. [4]Rahm, D. (2011), Regulating hydraulic fracturing in shale gas plays: the case of Texas, Energy Policy, 39, 2974-2981, doi:10.1016/j. enpol.2011.03.009. [5]Verrastro, F., and C. Branch (2010), Developing America’s unconventional gas resources: benefits and challenges, Center for Strategic and International Studies, Washington, DC. [6] Jiang, M., W. M. Griffin, C. Hendrickson, P. Jaramillo, J. VanBriesen, and A. Venkatesh (2011), Life cycle greenhouse gas emissions of Marcellus shale gas, Env. Res. Lett., 6, 1-9, doi:10.1088/1748-9326/6/3/034014. [7] Kemball-Cook, S., A. Bar-Ilan, J. Grant, L. Parker, J. Jung, W. Santamaria, J. Mathews, and G. Yarwood (2010), Ozone impacts of natural gas development in the Haynesville shale, Environ. Sci. Technol., 44, 9357-9363. [8]Pétron, G., G. Frost, B. R. Miller, A. I. Hirsch, S. A.Montzka, A. Karion, M. Trainer, C. Sweeney, A. E. Andrews, L. Miller, J. Kofler, A. Bar-Ilan, E. J. Dlugokencky, L. Patrick, C. T. Moore Jr., T. B. Ryerson, C. Siso, W. Kolodzey, P. M. Lang, T. Conway, P. Novelli, K. Masarie, B. Hall, D. Guenther, D. Kitzis, J. Miller, D. Welsh, D. Wolfe, W. Neff, and P. Tans (2012), Hydrocarbon Emissions Characterization in the Colorado Front Range: A Pilot Study, J. Geophys. Res., 117, D04304, doi:10.1029/2011JD016360. [9]Paltsev, S., H. D. Jacoby, J. M. Reilly, Q. J. Ejaz, J. Morris, F. O’Sullivan, S. Rausch, N. Winchester, and O. Kragha (2011), The future of U.S. natural gas production, use, and trade, Energy Policy, 39, 5309-5321. [10]Roth, I. F., and L. L. Ambs (2004), Incorporating externalities into a full cost approach to electric power generation life-cycle costing, Energy, 29, 2125-2144. [11] California Energy Commission (1998). Energy technology status report, 1996. California Energy Commision, Sacramento, CA. [12] Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (2007), Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, 2007, http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch2s2-10-2. html. [13] Shindell, D.T., G. Faluvegi, D. M. Koch, G. A. Schmidt, N. Unger, and S. E. Bauer (2009), Improved Attribution of Climate Forcing to Emissions, Science, 326, 716-718. [14]Howarth, R. W., R. Santoro and A. Ingraffea (2011), Methane and the greenhouse-gas footprint of natural gas from shale formations, Climate Change, 106, 679-690. [15]Lee, M. K. C. (2008), Source Specific Permit Handbook, http://www.baaqmd.gov/~/ media/Files/Engineering/Permit%20Handbook/PH_00_05.ashx [16] Coiante D, Barra L (1995), Practical method for evaluating the real cost of electrical energy, International Journal of Energy Research, 19(2), 159–68. [17]Vollebergh H (1997), Environmental externalities and social optimality in biomass markets: waste-to-energy in the Netherlands and biofuels in France, Energy Policy, 25(6), 605–21. [18] Distributed Power Coalition of America Volume 2, 1st Edition • Spring 2012 47 PR O O F #2 (1999), Benefits of distributed power,http:// www.dpc.org/utilities.html. [19]Pace University Center for Environmental Legal Studies (1990), Environmental costs of electricity, Oceana Publications, New York. [20]Energy Information Agency (2010), Annual Energy Outlook 2010 with Projections to 2035, U.S. Department of Energy, Washington, D.C. [21]Energy Information Agency (2011), Review of Emerging Resources: U.S. Shale Gas and Shale Oil Plays, U.S. Department of Energy, Washington, D.C. [22] Arthur, J. D., M. Uretsky, and P. Wilson (2010), Water Resources and Use for Hydraulic Fracturing in the Marcellus Shale Region, http://fracfocus.org/sites/default/files/ publications/water_resources_and_use_ for_hydraulic_fracturing_in_the_marcellus_shale_region.PDF. [23]National Wildlife Federation, Environmental Defense, and Lone Star Chapter of the Sierra Club (2006), The 16 water regions of Texas, http://www.texaswatermatters.org/ regions.htm. [24] U.S. Census Bureau (2010), State and County Quick Facts, http://quickfacts.census. gov/qfd/index.html. [25]Environmental Protection Agency (2009), Water on tap: what you need to know, http://water.epa.gov/drink/guide/upload/ book_waterontap_full.pdf. [26]Environmental Protection Agency (2007), Inventory of U.S. Greenhouse Gas Emissions and Sinks: 1990-2005, http://www.epa.gov/ climatechange/emissions/usinventoryreport.html. [27] Shampton, J. F., and D. Ritter (2011), Making the earth move: liability for earthquake damage associated with oil and gas production activities, Southern Law Journal, 21, 91-100. [28] McKenzie, Lisa M.; Witter, Roxana Z.; Newman, Lee S. (2012), Human health risk assessment of air emissions from development of unconventional natural gas resources, Science of the Total Environment, 424: 79-87 48 Journal of Student Research in Environmental Science at Appalachian PR O O F #2 Volume 2, 1st Edition • Spring 2012 49 PR O O F #2
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