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A 2D fully coupled hydro-mechanical finite-discrete element model with real pore seepage for simulating the deformation and fracture of porous medium driven by fluid

机译:具有真实孔隙渗流的二维全耦合水力机械有限元模型,用于模拟流体驱动的多孔介质的变形和破裂

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摘要

Based on the finite-discrete element method (FDEM), a 2D fully coupled model with real pore seepage is proposed. This model can solve the problem of the deformation and fracture of porous medium driven by fluid. In this model, the fluid flow in the fracture is expressed by the cubic law, while the fluid flow in the rock matrix is characterized by Darcy's law and solved by the finite volume method. The interaction between pore seepage and fracture seepage is realized at the fracture. Three analytical solutions are presented to verify the correctness of the proposed model. The results show that the numerical solutions agree well with the analytical solutions. In addition, a hydraulic fracturing problem with a complex fracture network is studied using this model. The simulation results show that the model can capture the fracture initiation, propagation, and intersection, the interaction of natural fractures and newly generated fractures, and the evolution of fluid pressure during hydraulic fracturing. The model can be used not only to simulate hydraulic fracturing in shale gas and geothermal mining but also to solve a series of geomechanical problems related to the effect of fluid. Thus, this model has broad application prospects. (C) 2017 Elsevier Ltd. All rights reserved.
机译:基于有限元法,提出了一种具有真实孔隙渗流的二维全耦合模型。该模型可以解决流体驱动的多孔介质变形和破裂的问题。在该模型中,裂缝中的流体流动用三次定律表示,而岩石基体中的流体流动用达西定律表征,并通过有限体积法求解。在裂缝处实现了孔隙渗流与裂缝渗漏之间的相互作用。提出了三种分析解决方案,以验证所提出模型的正确性。结果表明,数值解与解析解吻合良好。此外,使用该模型研究了具有复杂裂缝网络的水力压裂问题。仿真结果表明,该模型可以捕获裂缝的萌生,扩展和相交,自然裂缝与新裂缝的相互作用以及水力压裂过程中流体压力的变化。该模型不仅可以用来模拟页岩气和地热开采中的水力压裂,而且可以解决一系列与流体作用有关的地质力学问题。因此,该模型具有广阔的应用前景。 (C)2017 Elsevier Ltd.保留所有权利。

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