多孔介质中含毛细滞后的弹塑性地质力学与两相流耦合建模

H. C. Yoon, J. Kim
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摘要

本文运用弹塑性基本理论研究了两个耦合不可逆过程的新本构关系:弹塑性地质力学和带毛细滞后的两相流。将流体加性分解为弹塑性两部分,并假定其变换为无穷小。具体而言,塑性流体含量,即总残余(或不可恢复)饱和度,由于地质力学塑性和毛细滞后这两个不可逆过程,也被加性分解成组分。塑性流体含量的加性分解有助于将现有的两个单独的模拟器组合起来,例如,通过使用固定应力顺序法。对于多相流体与地质力学耦合的孔隙压力,采用等效孔隙压力,得到了多相流体与地质力学耦合的完备性,而不考虑毛细作用。我们进行了能量分析,以证明所提出模型的适定性。并通过数值算例验证了循环吸/排水和加载/卸载过程的稳定解。分别采用van Genuchten和Drucker Prager毛细管和塑性模型,我们证明了多相流和弹塑性地质力学中毛细管滞后模型的鲁棒性。
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The Modeling for Coupled Elastoplastic Geomechanics and Two-Phase Flow With Capillary Hysteresis in Porous Media
We study new constitutive relations employing the fundamental theory of elastoplasticity for two coupled irreversible processes: elastoplastic geomechanics and two-phase flow with capillary hysteresis. The fluid content is additively decomposed into elastic and plastic parts with infinitesimal transformation assumed. Specifically, the plastic fluid content, i.e., the total residual (or irrecoverable) saturation, is also additively decomposed into constituents due to the two irreversible processes: the geomechanical plasticity and the capillary hysteresis. The additive decomposition of the plastic fluid content facilitates combining the existing two individual simulators easily, for example, by using the fixed-stress sequential method. For pore pressure of the fluid in multi-phase which is coupled with the geomechanics, the equivalent pore pressure is employed, which yields the well-posedness of coupled multi-phase flow and geomechanics, regardless of the capillarity. We perform an energy analysis to show the well-posedness of the proposed model. And numerical examples demonstrate stable solutions for cyclic imbibition/drainage and loading/unloading processes. Employing the van Genuchten and the Drucker Prager models for capillary and the plasticity, respectively, we show the robustness of the model for capillary hysteresis in multiphase flow and elastoplastic geomechanics.
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