Date of Award:
5-2014
Document Type:
Dissertation
Degree Name:
Doctor of Philosophy (PhD)
Department:
Geosciences
Department name when degree awarded
Geology
Committee Chair(s)
James P. Evans
Committee
James P. Evans
Committee
John W. Shervais
Committee
Douglas R. Schmitt
Committee
Anthony R. Lowry
Committee
Thomas E. Lachmar
Abstract
Geothermal energy is being explored as a supplement to traditional fossil fuel resources to meet growing energy demand and reduce carbon emissions. Geothermal energy plants harvest heat stored in the Earth’s subsurface by bringing high temperature fluids to the surface and generating steam to produce electricity. Development of geothermal resources is often inhibited by large upfront risk and expense. Successful mitigation of those costs and risks begins with efficient characterization of the resource before development. A typically successful geothermal reservoir consists of a fractured reservoir that conducts hydrothermal fluids and a cap rock seal to limit convective heat loss through fluid leakage. The controls on the system include the density and orientation of fractures, mechanical rock properties, and the local stress field acting on those rocks.
The research presented in this dissertation utilizes diverse data sets to characterize core, wireline borehole logs, and laboratory data to describe the distribution of fractures, rock properties, and the orientation and magnitude of stresses acting on the borehole. The research demonstrates there is a potential resource in the region and describes the controls on the vertical extent of the hydrothermal fluids. The distribution of fractures is controlled by the distribution of elastic rock properties and rock strength. A cap rock seal is present that limits hydrothermal fluid loss from a fractured artesian reservoir at 1,745 m (5,726 ft). In addition to characterization of the resource, this research demonstrates that an equivalent characterization can be used in future exploration wells without the expense and risk of collecting core. It also demonstrates that multiple methods of analysis can be utilized simultaneously when some data are not available. Data collection from deep wellbores involves risk and data loss or tool failure is a possibility. In these cases, our methods show that successful characterization is still possible, saving time and money, and minimizing the financial risk of exploration
Checksum
cb0a9c51479a56a9a72e8a481587c262
Recommended Citation
Kessler, James Andrew, "In Situ Stress and Geology from the MH-2 Borehole, Mountain Home, Idaho: Implications for Geothermal Exploration from Fractures, Rock Properties, and Geomechanics" (2014). All Graduate Theses and Dissertations, Spring 1920 to Summer 2023. 3966.
https://digitalcommons.usu.edu/etd/3966
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