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Modeling of coupled liquid-gas-solid three-phase processes due to fluid injection

机译:流体注入引起的气固两相耦合过程的建模

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摘要

A coupled liquid-gas-solid three-phase model, linking two numerical codes (TOUGH2/EOS3 and FLAC(3D)), was firstly established and validated by simulating an in-situ air flow test in Essen. Then the coupled model was employed to investigate responses of multiphase flow and soil skeleton deformation to compressed air or freshwater injection using the same simulation conditions in an aquifer of Tianjin, China. The simulation results show that with injecting pressurized fluids, the vertical effective stress in some area decreases owing to the pore pressure increasing, an expansion of soil skeleton appears, and land uplift occurs due to support actions from lower deformed soils. After fluids injection stops, soil deformation decreases overall due to injecting fluids dissipating. With the same applied pressure, changes in multiphase flow and geo-mechanical deformation caused by compressed air injection are relatively greater than those by freshwater injection. Furthermore, the expansion of soil skeleton induced by compressed air injection transfers upward and laterally continuously with time, while during and after freshwater injection, this expansion reaches rapidly a quasi-steady state. These differences induced by two fluids injection are mainly because air could spread upward and laterally easily for its lower density and phase state transition appears for compressed air injection.
机译:首先建立了耦合两个数字代码(TOUGH2 / EOS3和FLAC(3D))的液-气-固三相耦合模型,并通过模拟埃森的原位空气流动试验进行了验证。然后,在相同的模拟条件下,采用耦合模型研究了多相流和土壤骨架变形对压缩空气或淡水注入的响应。仿真结果表明,随着压力的增加,孔隙压力的增加使某些区域的竖向有效应力减小,土壤骨架出现扩张,低变形土的支护作用引起了陆地隆起。注入流体停止后,由于注入流体的耗散,土壤变形总体上减少了。在相同的施加压力下,由压缩空气注入引起的多相流变化和岩土力学变形的变化相对大于由淡水注入引起的变化。此外,由压缩空气注入引起的土壤骨架的膨胀随时间向上和横向连续地转移,而在注入淡水期间和之后,该膨胀迅速达到准稳态。由两种流体注入引起的这些差异主要是因为空气由于其较低的密度而易于向上和横向扩散,并且对于压缩空气注入出现了相态转变。

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