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A two-dimensional coupled hydro-mechanical finite-discrete model considering porous media flow for simulating hydraulic fracturing

机译:考虑多孔介质流动的水力压裂二维水力耦合有限元模型

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In this study, we propose a new coupled hydro-mechanical model considering porous media flow (FDEM-flow) for simulating hydraulic fracturing, which makes full use of the unique topological connection between joint elements and solid elements in the combined finite-discrete element method (FDEM). The joint elements form the flow channel for fluid, through which flow obeys the cubic law. In addition, viscous forces of fluid are taken into account in FDEM-flow. A simple example with analytical solution is given to verify the model. Then, the effects of fluid viscosity on hydraulic fracturing are investigated by this model. The simulated results show that when a low viscosity fluid is injected, the fluid infiltrates the fracture rapidly. The initiation pressure is lower than the theoretical value and the breakdown pressure is slightly larger than the initiation pressure. When high viscosity fluid is injected, fluid infiltrate into the cracks very slowly. The initiation pressure is close to the theoretical value and the breakdown pressure is much larger than the initiation pressure. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在这项研究中,我们提出了一种新的考虑多孔介质流动(FDEM-flow)的耦合水力力学模型来模拟水力压裂,它在有限元组合法中充分利用了节理单元和实体单元之间独特的拓扑联系。 (FDEM)。接头元件形成了流体的流道,流经该流道遵循三次定律。此外,在FDEM流动中考虑了流体的粘性力。给出了带有解析解的简单示例来验证模型。然后,通过该模型研究了流体黏度对水力压裂的影响。模拟结果表明,当注入低粘度流体时,流体会迅速渗透到裂缝中。起始压力低于理论值,击穿压力略大于起始压力。当注入高粘度流体时,流体非常缓慢地渗透到裂缝中。初始压力接近理论值,击穿压力远大于初始压力。 (C)2016 Elsevier Ltd.保留所有权利。

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