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Analytical solution for propagation of hydraulic fracture with Barenblatt's cohesive tip zone

机译:Barenblatt黏性尖端区域在水力压裂扩展中的解析解

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In the paper, a model of a hydraulic fracture with a tip cohesive zone according to the Barenblatt's approach is considered. The particular case of inviscid fracturing fluid and impermeable rock is studied analytically. Dependencies on time of the fracture length, injection pressure, and fracture opening at the well-bore are obtained, and compared with the corresponding dependencies for a brittle (elliptic-tip) hydraulic fracture. It is proved that on the assumption of finite-ness of the cohesive stresses action range, the cohesive zone length cannot also exceed a certain limit value. The limit form of the cohesive zone is obtained, and the limit fracture toughness is evaluated. It is shown that effective fracture toughness tends to the limit value as power function of fracture length with index -1/2.
机译:在本文中,根据Barenblatt的方法,考虑了具有尖端粘性区域的水力压裂模型。通过分析研究了无粘性压裂液和不渗透岩石的特殊情况。获得了裂缝长度,注入压力和井眼裂缝开度对时间的依赖性,并将其与脆性(椭圆尖端)水力裂缝的相应依赖性进行了比较。已经证明,在内聚应力作用范围的有限性的假设下,内聚区长度也不能超过一定的极限值。获得内聚区的极限形式,并评估极限断裂韧性。结果表明,有效的断裂韧性随着断裂长度的幂函数趋向于极限值,为-1/2。

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