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The influence of the cohesive process zone in hydraulic fracturing modelling

机译:内聚过程区对水力压裂建模的影响

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This paper studies the importance of the cohesive zone in the modelling of a fluid driven fracture under plain strain conditions. The fracture is driven by pumping of an incompressible viscous fluid at the fracture inlet. Rock deformation is modeled for linear elastic and poroelastic solids. Fluid flow in the fracture is modeled by lubrication theory. The cohesive zone approach is used as the fracture propagation criterion.Finite element analysis was used to compute the solution for the crack length, the fracture opening and propagation pressure as a function of the time and distance from the wellbore. It is demonstrated that the crack profiles and the propagation pressures are larger in the case of elastic-softening cohesive model compared to the results of the rigid-softening cohesive model for both elastic and poroelastic cohesive solids. It is found that the results are affected by the slope of the loading branch of the cohesive model and they are nearly unaffected from the exact form of the softening branch.Furthermore, the size of the process zone, the fracture geometry and the propagation pressure increase with increasing confining stresses. These results may explain partially the discrepancies in net-pressures between field measurements and conventional model predictions.
机译:本文研究了粘性区域在平原应变条件下流体驱动裂缝建模中的重要性。裂缝是通过在裂缝入口处泵入不可压缩的粘性流体来驱动的。岩石变形针对线性弹性和多孔弹性固体建模。裂缝中的流体流动是通过润滑理论建模的。内聚区方法被用作裂缝扩展准则。有限元分析被用来计算裂缝长度,裂缝开度和扩展压力随时间和距井眼距离的函数。结果表明,与弹性和多孔弹性内聚固体的刚性软化内聚模型相比,弹性软化内聚模型的裂纹轮廓和扩展压力更大。结果表明,结果受内聚模型加载分支斜率的影响,几乎不受软化分支确切形式的影响。此外,过程区的大小,裂缝的几何形状和传播压力增加随着围压的增加。这些结果可能部分解释了现场测量和常规模型预测之间的净压力差异。

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