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On the simulation of fracking processes in porous media by use of a phase-field approach

机译:利用相场方法模拟多孔介质中的压裂过程

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The theoretical and numerical description of hydraulic fracturing processes in porous soil or rock is a very interesting topic in engineering sciences. Following this, the well-known phase-field approach applied to fracturing solids was recently embedded in the Theory of Porous Media for the description of hydraulic fracturing scenarios. This method has been found very convenient not only for the description of solid deformation and fracture but also for the transition of Darcy-type flow in the saturated porous-media domain towards Navier-Stokes-type flow in fractured zones. However, the monotonic evolution of the phase-field variable as it is used in purely solid-mechanical scenarios does not allow for the description of pre-existing closed fractures or of fractures closing after generation, where either only Darcy-type flow occurs or where Navier-Stokes-type flow turns back to Darcy-type flow. Taking this into account, the present study also concerns the introduction of a crack-opening indicator as an additional variable governed by the current deformation. By use of this procedure, not only opening but also closing fractures as well as pre-fractured domains can easily be included into the numerical simulation of fracking scenarios in saturated porous media. Proceeding from the finite-element analysis, the numerical results are found consistent with experimental observations presented in the literature.
机译:在多孔土壤或岩石中水力压裂过程的理论和数值描述是工程科学中非常有趣的主题。此后,最近在多孔介质理论中嵌入了用于压裂固体的众所周知的相场方法,以描述水力压裂情况。已经发现该方法非常方便,不仅用于描述固体变形和断裂,而且还用于使饱和多孔介质域中的达西类型的流向断裂区域中的纳维-斯托克斯类型的流过渡。但是,在纯固体力学情况下使用的相场变量的单调演变无法描述既存的闭合裂缝或生成后闭合裂缝的描述,其中仅发生达西流或Navier-Stokes型流变回Darcy型流。考虑到这一点,本研究还涉及引入裂缝指示器作为由当前变形控制的附加变量。通过使用该程序,不仅可以轻松地将裂缝闭合,而且可以将闭合裂缝以及预裂缝区域纳入饱和多孔介质中的压裂场景的数值模拟中。从有限元分析出发,发现数值结果与文献中的实验观察结果一致。

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