DEEP PERMEABLE STRATA GEOTHERMAL ENERGY A Means To Extend Geothermal Energy Production To Deep Sedimentary Basins Dr. Richard J. Erdlac, Jr. The University of Texas of the Permian Basin Center for Energy & Economic Diversification Douglas B. Swift Petroleum Consultant Concept Devised & Initiated By: Mr. Douglas B. Swift Dr. Richard J. Erdlac, Jr. West Texas Earth Resources Institute World Geothermal Provinces U.S. Geothermal Provinces United States Geothermal Electric Power Generation Potential (GeoPowering The West - DOE, 2000) Top 3 States: Nevada, California, Utah Other High Potential States: Idaho, Hawaii, New Mexico, Oregon, South Dakota, Texas, and Wyoming “Texas does not have the sort of readily accessible high-temperature hydrothermal resource that can be used to generate electricity.” “Geysers, hot springs, volcanoes, and seismic activity, all of which are noticeably absent in Texas, mark such regions.” Texas Renewable Energy Resource Assessment, 1995 Statement did not envision DPSGE. Deep sedimentary basins, (e.g the Delaware, Val Verde, Anadarko, Appalachian) contain high thermal reservoirs which can be tapped for geothermal power generation. Structures in the Delaware and Val Verde Basins have been prolific for natural gas production. These wells demonstrate extensive, highly porous and permeable strata. Geothermal grade temperatures are readily apparent from DST data, BHT tests, and less reliable electric log measurements. Potential U.S. DPSGE Sedimentary Basins Texas Oil And Gas District Boundaries Deep wells (Ellen>15,000’) in central Delaware Basin. Well control courtesy of GDS; Mapped with Geographix. - 1 50 00 - 15000 - 15 000 -1 0 00 - 50 0 00 0 - 15000 - 10 00 0 -1 50 00 00 0 - 20 00 5 - -1 00 00 -1 Subsurface map of borehole temperature (BHT) data from oil and gas wells in the Permian Basin. Black dots: BHT 150oF (65oC). Blue dots: BHT = 151oF to 179oF (66oC to 81oC). Green dots: BHT = 180oF to 280oF (82oC to 142oC). Red dots: BHT 290oF (143oC). Isotherm contours are in thousands of feet below surface. The dark gray area represents the 150oF isotherm. Adapted from Subsurface Temperature Map of North America (1976). The basic requirements for an exploitable DPSGE geothermal region are similar to those for oil and gas exploration: 1) a sufficiently high geothermal gradient; 2) A significantly large, porous and permeable reservoir to receive and heat injection fluids; 3) A seal to contain the system. 120 100 80 60 40 20 0 0. 60 0. 66 0. 72 0. 78 0. 84 0. 90 0. 96 1. 02 1. 08 1. 14 1. 20 1. 26 1. 32 1. 38 1. 44 1. 50 1. 56 Wells Total Permian Basin Temp. Grad. Distribution of temperature gradient for wells within the Permian Basin (New Mexico and Texas). Values given in degrees F/100 feet. Data source from the Geothermal Survey of North America. AAPG, 1976. Delaware - Val Verde Basins 10 6 4 2 0 0. 60 0. 66 0. 72 0. 78 0. 84 0. 90 0. 96 1. 02 1. 08 1. 14 1. 20 1. 26 1. 32 1. 38 1. 44 1. 50 1. 56 Wells 8 Temp. Grad. Distribution of temperature gradient for wells within the Delaware and Val Verde Basins. Values given in degrees F/100 feet. Data source from the Geothermal Survey of North America. AAPG, 1976. Deep Ellenburger Formation gas fields with BHTs ranging from 115o to > 160oC (239o to >320oF) are well documented. These temperatures are sufficiently high to generate live steam. A number of the fields studied are prospective for flash power generation. Most are particularly attractive as sources for fueling binary systems. 5 4 3 2 1 0 0. 60 0. 66 0. 72 0. 78 0. 84 0. 90 0. 96 1. 02 1. 08 1. 14 1. 20 1. 26 1. 32 1. 38 1. 44 1. 50 1. 56 Wells Trans-Pecos Temp. Grad. Distribution of temperature gradient for wells within the Trans-Pecos region of Texas. Values given in degrees F/100 feet. Data source from the Geothermal Survey of North America. AAPG, 1976. Geothermal Delivery Systems Existing Plant Designs Dry Steam Power Plants – use steam directly. Flash Steam Power Plants – hot water under pressure (most common). Binary Cycle Power Plants – hot water through heat exchanger. Feedstock Systems – incremental heat in elevated water temperatures. New Plant Designs Power Tube – iso-pentane & iso-butane into subsurface. Water temperature (optimum range) 230o to 380o F (110o to 193o C) Construction costs ~ $1500 per kW including exploration and drilling. 10 Mw plant $15,000,000 (National Renewable Energy Laboratory, 1999) Canyon Diablo Binary Geothermal Plant Mammoth, California Alternate Geothermal Technology – Power Tube DEEP >4 KM (>13,000’) PERMEABLE STRATA GEOTHERMAL ENERGY A NEW DAWN!