Numerical investigation of a novel hypothesis for fracture termination and crossing, with applications to lost circulation mitigation and hydraulic fracturing

Mayowa Oyedere, Ken Gray, Mark W. McClure
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引用次数: 4

Abstract

We investigate a novel hypothesis regarding the process of hydraulic fracture termination against a preexisting frictional interface. According to current understanding, crossing occurs when small tensile fractures form ahead of the crack tip, on the other side of the frictional interface, before the concentration of stress at the crack tip causes slip along the interface. Slip blunts the concentration of stress at the crack tip and causes termination. Existing crossing criteria assume that the incipient fractures ahead of the crack tip form instantaneously once the effective stress is sufficiently tensile. However, there is a poroelastic response that causes a reduction in pressure in response to opening. This is counteracted by flow into the crack from the surrounding matrix. In very low matrix permeability formations (shale, coalbed methane, etc.), flow of fluid inward from the matrix is slow, and the opening of these incipient fractures may require a non-negligible amount of time. Using the hydro-mechanical discrete fracture network simulator CFRAC, we performed a series of numerical simulations to qualitatively investigate this process. The simulations confirm that poroelastic response could affect incipient fracture initiation and hydraulic fracture crossing. Based on this mechanism, we developed a heuristic modification to an existing crossing criterion. We applied the new criterion to investigate an injection sequence for prevention of lost circulation in fractured, low matrix permeability formations. Lost circulation occurs if wellbore fluid pressure exceeds the minimum principal stress, causing fluid loss due to propagation of a hydraulic fracture. In our proposed injection sequence: (1) injection is performed at high rate to create near wellbore fracture network complexity and then (2) viscous fluid is injected into the newly formed fractures to create resistance to flow. The simulations show that this sequence may be able to mitigate lost circulation and create a stress cage around the wellbore.

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一种新的裂缝终止和交叉假设的数值研究,及其在减少漏失和水力压裂中的应用
我们研究了一个关于水力压裂终止过程的新假设,反对预先存在的摩擦界面。根据目前的理解,在裂纹尖端的应力集中导致沿界面滑动之前,在摩擦界面的另一侧,在裂纹尖端前面形成小的拉伸断裂,就会发生交叉。滑移使裂纹尖端的应力集中钝化并导致终止。现有的交叉准则假设,一旦有效应力足够大,裂纹尖端之前的初始断裂就会立即形成。然而,有一个孔隙弹性响应,导致压力的减少,以响应打开。这被从周围基质流入裂纹的流体所抵消。在基质渗透率非常低的地层(页岩、煤层气等)中,流体从基质向内流动缓慢,这些早期裂缝的打开可能需要不可忽略的时间。利用流体力学离散裂缝网络模拟器CFRAC,我们进行了一系列数值模拟来定性研究这一过程。模拟结果表明,孔隙弹性响应影响水力裂缝初期起裂和水力裂缝穿越。基于这种机制,我们开发了一种启发式修改现有的交叉准则。我们应用新标准研究了在裂缝性、低基质渗透率地层中防止漏失的注入顺序。如果井筒流体压力超过最小主应力,则会发生漏失,导致水力裂缝扩展导致流体漏失。在我们提出的注入顺序中:(1)高速注入以增加近井裂缝网络的复杂性,然后(2)将粘性流体注入新形成的裂缝中以产生流动阻力。模拟结果表明,该顺序可以减少漏失,并在井筒周围形成应力笼。
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