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TOUGH2Biot: A Coupled Thermal-Hydrodynamic-Mechanical Model for Geothermal Development

机译:TOUGH2Biot:地热发育的热-水力-力学耦合模型

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Geothermal development and exploitation involve coupled thermal-hydrodynamic-mechanical (THM) processes. Amechani-cal module based on the extended Biot consolidation model is developed and incorporated into the well-established thermal-hydrodynamic simulator T0UGH2, resulting in an integral numerical THM simulation program TOUGH2Biot. A finite element method is employed to discretize space for rock mechanical calculation and the Mohr-Coulomb failure criterion is used to determine if rock undergoes shear-slip failure. Mechanics is partly coupled with the thermal-hydrodynamic processes and gives feedback to flow through stress-dependent porosity and permeability. TOUGH2Biot is verified against an analytical solution for the 1D Terzaghi consolidation and cooling-induced subsidence. TOUGH2Biot has been applied to evaluate thermal, hydrodynamic and mechanical responses of geothermal exploitation at the Geysers geothermal field, California. The results demonstrate that change in effective stress due to temperature decrease is greater than that due to pressure decrease near the production. The most likely shear-slip occurs near the injection because of an increase in shear stress. The formations are compressed and the maximum vertical displacement is up to 0.6m after 40 years of production, half of which is contributed from temperature decline. At the same time, TOUGH2Biot is proved to have the capability of analyzing change in pressure and temperature, displacement, stress and potential shear-slip failure for geothermal exploitation.
机译:地热开发和开采涉及热-水动力-机械(THM)耦合过程。开发了基于扩展的Biot固结模型的Amechani-cal模块,并将其结合到完善的热液动力学模拟器T0UGH2中,从而生成了完整的THM数值模拟程序TOUGH2Biot。采用有限元方法离散化空间以进行岩石力学计算,并使用Mohr-Coulomb破坏准则确定岩石是否经历了剪切滑移破坏。力学部分与热流体动力学过程耦合,并提供反馈,使其流经应力相关的孔隙率和渗透率。 TOUGH2Biot已针对一维Terzaghi固结和冷却引起的沉陷的分析解决方案进行了验证。 TOUGH2Biot已用于评估加利福尼亚州Geysers地热田的地热开采的热,水动力和机械响应。结果表明,温度降低引起的有效应力变化大于生产附近压力降低引起的有效应力变化。由于剪切应力增加,最可能发生的剪切滑移发生在注入附近。生产40年后,地层被压缩,最大垂直位移高达0.6m,其中一半是温度下降引起的。同时,TOUGH2Biot被证明具有分析地热开采压力和温度,位移,应力和潜在剪切滑移破坏的能力。

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