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DOI | 10.1016/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
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ISSN | 0375-6505 |
EISSN | 1879-3576 |
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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