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Numerical Investigation of Influence of In-Situ Stress Ratio, Injection Rate and Fluid Viscosity on Hydraulic Fracture Propagation Using a Distinct Element Approach

机译:离散元法数值模拟地应力比,注入速率和流体黏度对水力压裂扩展的影响

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Numerical simulation is very useful for understanding the hydraulic fracturing mechanism. In this paper, we simulate the hydraulic fracturing using the distinct element approach, to investigate the effect of some critical parameters on hydraulic fracturing characteristics. The breakdown pressure obtained by the distinct element approach is consistent with the analytical solution. This indicates that the distinct element approach is feasible on modeling the hydraulic fracturing. We independently examine the influence of in-situ stress ratio, injection rate and fluid viscosity on hydraulic fracturing. We further emphasize the relationship between these three factors and their contributions to the hydraulic fracturing. With the increase of stress ratio, the fracture aperture increases almost linearly; with the increase of injection rate and fluid viscosity, the fracture aperture and breakdown pressure increase obviously. A low value of product of injection rate and fluid viscosity ( i.e. , Qμ ) will lead to narrow fracture aperture, low breakdown pressure, and complex or dispersional hydraulic fractures. A high value of Qμ would lead wide fracture aperture, high breakdown pressure, and simple hydraulic fractures (e.g., straight or wing shape). With low viscosity fluid, the hydraulic fracture geometry is not sensitive to stress ratio, and thus becomes a complex fracture network.
机译:数值模拟对于理解水力压裂机理非常有用。在本文中,我们使用独特元素方法模拟水力压裂,以研究一些关键参数对水力压裂特征的影响。通过独特元素方法获得的击穿压力与分析解决方案一致。这表明在水力压裂建模中独特单元法是可行的。我们独立研究了地应力比,注入速率和流体粘度对水力压裂的影响。我们进一步强调这三个因素之间的关系及其对水力压裂的贡献。随着应力比的增加,断裂口径几乎呈线性增加。随着注入速率和流体黏度的增加,裂缝孔径和破裂压力明显增加。注入速率和流体粘度(即Qμ)的乘积值低将导致裂缝口狭窄,击穿压力低以及复杂或分散的水力裂缝。 Qμ的高值将导致较大的裂隙孔径,高击穿压力和简单的水力压裂(例如,笔直或机翼形)。对于低粘度流体,水力压裂几何形状对应力比不敏感,因此成为复杂的压裂网络。

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