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A Non-Local Model for Fluid-Structure Interaction with Applications in Hydraulic Fracturing

机译:流体-结构相互作用的非局部模型及其在水力压裂中的应用

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摘要

Modeling important engineering problems related to flow induced damage (in the context of hydraulic fracturing among others) depends critically on characterizing the interaction of porous media and interstitial fluid flow. This work presents a new formulation for incorporating the effects of pore pressure in a non-local representation of solid mechanics. The result is a framework for modeling fluid-structure interaction problems with the discontinuity capturing advantages of an integral-based formulation. A number of numerical examples are used to show that the proposed formulation can be applied to measure the effect of leak-off during hydraulic fracturing as well as modeling consolidation of fluid saturated rock and surface subsidence caused by fluid extraction from a geologic reservoir. The formulation incorporates the effect of pore pressure in the constitutive description of the porous material in a way that is appropriate for nonlinear materials, easily implemented in existing codes, straightforward in its evaluation (no history dependence), and justifiable from first principles. A mixture theory approach is used (deviating only slightly where necessary) to motivate an alteration to the peridynamic pressure term based on the fluid pore pressure. The resulting formulation has a number of similarities to the effective stress principle developed by Terzaghi and Biot and close correspondence is shown between the proposed method and the classical effective stress principle.
机译:与流动引起的损伤(在水力压裂等情况下)有关的重要工程问题的建模,关键取决于表征多孔介质和间隙流体流动的相互作用。这项工作提出了一种新的公式,可以将孔隙压力的影响纳入固体力学的非局部表示中。结果是一个用于建模流体-结构相互作用问题的框架,其中不连续性体现了基于积分的配方的优点。使用大量数值示例来表明,所提出的公式可用于测量水力压裂过程中的渗漏效果,以及对由于从地质储层中抽出流体而引起的饱和流体的岩石固结和地表沉陷进行建模。该配方以适合非线性材料的方式将孔隙压力的影响纳入多孔材料的本征描述中,该方法易于在现有规范中实现,其评估简单(无历史记录依赖)且可根据第一原理进行论证。使用混合理论方法(在必要时仅略微偏移)以基于流体孔隙压力促使对围动态压力项进行更改。所得的公式与Terzaghi和Biot提出的有效应力原理有许多相似之处,并且在拟议的方法与经典有效应力原理之间显示出紧密的对应关系。

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