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THE CRACK TIP SOLUTION FOR HYDRAULIC FRACTURING IN A PERMEABLE SOLID

机译:渗透固体中水力压裂的裂缝提示解决方案

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This paper extends previous work on self-similar analytical solutions fora hydraulically driven fracture propagating in a solid which is in a state of plane strain. In particular, we examine the effect of fluid loss to the formation modelled by the Carter leak-off mechanism. Our main new results are asymptotic solutions for arbitrary rock permeability; it is shown how these may be represented by an expansion whose leading term is the near-tip solution in the high permeability limit. This term gives an integrable singularity in the near-tip fluid pressure which is slightly stronger than the singularity which arises in the impermeable case; it follows that there is always a region immediately adjacent to the fluid front where the solution is dominated by fluid loss. Our most important conclusion for applications is that the solution in the practical case of intermediate permeability may be constructed as a series which starts from the loss dominated limit. We also provide a detailed comparison of our predictions with results from a numerical model which includes a fluid lag zone. The results are found to be in good agreement in all of the various permeability regimes. [References: 15]
机译:本文扩展了以前的工作,这些工作是针对在平面应变状态下以固体传播的水力驱动裂缝的自相似解析解。特别是,我们检查了流体损失对卡特泄漏机制模拟的地层的影响。我们的主要新结果是任意岩石渗透率的渐近解。它显示了如何用扩展来表示这些扩展,其扩展项是高磁导率极限中的近端解。该术语在近端流体压力中给出可积分的奇点,该奇点比在不渗透情况下出现的奇点略强。因此,总有一个紧邻流体前沿的区域,在该区域中,溶液主要受流体损失的影响。我们对应用程序最重要的结论是,在中等渗透率的实际情况下,该解决方案可以构造为一系列以损耗为主的极限值。我们还将提供的预测结果与包含流体滞后区的数值模型的结果进行详细的比较。发现结果在所有各种渗透率方案中都吻合良好。 [参考:15]

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