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DOI10.1016/j.geothermics.2016.01.002
Desert Peak EGS: Mechanisms influencing permeability evolution investigated using dual-porosity simulator TFReact
Benato, Stefano1; Taron, Joshua2
通讯作者Benato, Stefano
来源期刊GEOTHERMICS
ISSN0375-6505
EISSN1879-3576
出版年2016
卷号63页码:157-181
英文摘要

The reservoir response associated with selected phases of the hydraulic stimulation conducted as part of the 2010-2013 Desert Peak Enhanced Geothermal System (EGS) project was investigated using the dual porosity numerical simulator TFReact. The code couples the solid mechanics (M) analyses of FLAC3D with the multiphase, non-isothermal and reactive capabilities (THC) of TOUGHREACT, and allows for a comprehensive investigation of the major thermal-hydraulic-mechanical-chemical (THMC) physical processes occurring in deep, tight rock masses subject to circulation of pressurized fluids. Numerical simulations were performed to determine: (a) pore pressure diffusion and stress field modifications, (b) development of mechanical deformation, and, above all, (c) relative impact of tensile vs. shear deformation on the evolution of the reservoir permeability. A three-well reservoir model was implemented to account for the combined influence of concurrent injection in wells 27-15 (EGS well), 22-22 and 21-2 (active injectors). This study simulated selected stimulation treatments carried out from 914 to 1067 m depth (shallow stimulation interval) and from 914 to 1771 m depth (extended stimulation interval). Alternative hydraulic stimulation schemes/scenarios (by assuming diverse varying injectate properties and injection durations) were modeled over the two stimulation intervals to test if and how the final permeability could have been further improved. Simulated permeability modifications appear to be predominantly governed by thermo-hydro-mechanical dilation (elastic) during stimulation of the shallow interval and by hydro-mechanical deformation (inelastic shear) during stimulation of the extended interval. Inelastic shear deformation delivers higher permeability gains, and in the shortest time, when hydraulically conductive and well-oriented features are targeted with the stimulation treatment. TFReact simulations combined with a detailed site conceptualization and microseismicity interpretation, provide further understanding of injection-induced mechanisms. (C) 2016 Elsevier Ltd. All rights reserved.


英文关键词Desert Peak Enhanced Geothermal Systems THMC Permeability evolution Hydraulic stimulation modeling
类型Article
语种英语
国家USA
收录类别SCI-E
WOS记录号WOS:000379630900012
WOS关键词FLUID INJECTION ; ROCK ; MICROSEISMICITY ; FRICTION ; SHEAR ; STIFFNESS ; BEHAVIOR ; GEYSERS ; STRESS ; FLOW
WOS类目Energy & Fuels ; Geosciences, Multidisciplinary
WOS研究方向Energy & Fuels ; Geology
来源机构United States Geological Survey ; Desert Research Institute
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/193298
作者单位1.Desert Res Inst, Div Hydrol Sci, Reno, NV 89512 USA;
2.US Geol Survey, 345 Middlefield Rd, Menlo Pk, CA 94025 USA
推荐引用方式
GB/T 7714
Benato, Stefano,Taron, Joshua. Desert Peak EGS: Mechanisms influencing permeability evolution investigated using dual-porosity simulator TFReact[J]. United States Geological Survey, Desert Research Institute,2016,63:157-181.
APA Benato, Stefano,&Taron, Joshua.(2016).Desert Peak EGS: Mechanisms influencing permeability evolution investigated using dual-porosity simulator TFReact.GEOTHERMICS,63,157-181.
MLA Benato, Stefano,et al."Desert Peak EGS: Mechanisms influencing permeability evolution investigated using dual-porosity simulator TFReact".GEOTHERMICS 63(2016):157-181.
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