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Hot Dry Rock Geothermal Energy Development in the USA

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Hot Dry Rock Geothermal Energy Development in the USA ( hot-dry-rock-geothermal-energy-development-the-usa )

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a highly jointed Precambrian plutonic and metamorphic complex. Other than an elevated geothermal gradient (about 64°C/km), the only volcanic association of the reservoir rock is in the contained pore fluids which are high in dissolved carbon dioxide, and contain trace amounts of hydrogen sulfide. While Fenton Hill was selected primarily on the basis of favorable heat flow and the lack of structural complexity in the anticipated reservoir rock, its location on a paved road made it easy to bring in heavy equipment. In addition, although the western flank of the caldera is heavily forested, a fire had destroyed much of the vegetation at the Fenton Hill site. Thus, the environmental impact of the project in this highly scenic area was small. Finally, the Fenton Hill site, as a part of the Santa Fe National Forest, was under the jurisdiction of the US Forest Service. It was therefore a simple matter to arrange an inter-governmental agreement to transfer management (but not ownership) of the land to the DOE. Los Alamos could then operate the site under its role as a contractor to the DOE. For all of these reasons, Fenton Hill appeared to be a good permanent site for carrying out HDR research and development. The Phase I HDR Reservoir. Development of the world's first HDR system was initiated at Fenton Hill in 1974. The first borehole was drilled in granitic rock to a depth of 2900 m where the temperature was 197°C . After a series of hydraulic fracturing experiments, a second wellbore was drilled toward the largest of the near-vertical, stimulated natural joints. A good connection was not immediately achieved, and sidetracking was necessary to establish contact with the initial well via a combination of induced and natural fracture pathways. The Phase I system was evaluated in a series of flow experiments from 1978 to 1980 (Dash et al. 1980). In the first flow test, water was circulated through the reservoir for 75 days in early 1978. The significant thermal drawdown (from 175°C to 85°C ) indicated that only a small heat transfer area existed. A second 28-day test in late 1978 assessed the effects of imposing a high backpressure on the production wellbore. This strategy was found to reduce flow impedance but not to increase the surface area of heat extraction. The reservoir was then enlarged by further hydraulic fracturing and two more flow experiments were conducted: First, a flow test lasting 23 days was carried out to quantify the operating performance of the enlarged reservoir. This was followed by a 286-day heat extraction flow test during which the reservoir temperature declined from an initial value of 156°C to a final level of 149°C . At the end of this series of flow tests, a short stress-unlocking experiment was performed. It entailed applying an elevated pressure to the reservoir in order to facilitate relative movement of joint surfaces and the resulting redistribution of fluid flow and/or the opening of new fluid pathways in the cooled reservoir rock. There were abundant indications of seismic activity within the reservoir during the pressurization experiment, and subsequent flow measurements suggested that the reservoir impedance had indeed been reduced. However, the system was not operated long enough following the stress-unlocking experiment to demonstrate that the improved flow conditions could be maintained for an extended length of time. The pioneering work with the Phase I HDR reservoir proved that heat could be extracted from HDR using the techniques conceived and developed at Los Alamos. In addition, it indicated that issues such as induced seismicity, water consumption, and fluid geochemistry (including its effect on the system components), would not present insurmountable problems in operating an HDR heat mine. This initial field work highlighted the dynamic nature of HDR reservoirs, even under steady- 3

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