T153 Enhanced Geothermal Systems (EGS): Sustainable, Carbon-Free Energy
Tuesday, 2 November 2010
8:00 AM - 12:00 PM
Room 612
ENGINEERING GEOTHERMAL SYSTEMS IN SEDIMENTARY BASINS: EXAMPLES OF POTENTIAL IN COLORADO
Paper number: T153-6
Program: Technical Sessions
Time: 9:25 AM – 9:40 AM
Authors
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Matthew SaresColorado Geological Survey, Denver, CO
Abstract
An alternative to hydraulic fracturing to produce connectivity between two wells would be to use natural permeability. This natural connectivity has been successfully used at several locations in Germany, two of which produce >3 MW of electricity each from a pair of wells. Geothermal gradients in sedimentary basins in Colorado are above average for continental crust, ranging from 35 to 70°C/km. Temperatures of 150°C are indicated from bottom-hole temperature data in some basins as shallow as 2-3 km. There are probably permeable aquifers at these depths. Many hydrocarbon wells penetrate to these depths, so permeability testing either in situ or with core samples should be possible. Abandoned wells may even be available for a pilot project to test connectivity and heat extraction through a natural aquifer. Colorado is ready to engineer sedimentary geothermal systems with natural permeability.