由流体注入触发的故障再激活建模

D. Tran, V. Shrivastava, L. Nghiem
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摘要

近年来,随着人们越来越关注二氧化碳封存、水力压裂和注汽作业,对流体诱发地震活动的理解引起了研究人员和实践工程师的广泛关注。由于注入作业而重新激活现有的休眠断层,可能导致流体从储层流过或沿着断层流向不需要的区域。这是一个严重的挑战,需要仔细研究,以便采取措施避免这种情况的发生。本文提出了一种利用地质力学响应来计算储层因注入流体而发生应力变化时的滑移趋势的方法。滑移倾向被认为是决定断层是否重新激活的主要变量。它是根据断层表面法向的有效应力和切向应力计算的。当断层附近格块孔隙压力增大导致断层表面有效应力减小时,有可能使断层滑动趋势超过临界极限。在这种情况下,断层两侧的栅格块的透射率增加,以允许流体流入断层并随后沿断层流动。当流体从储层经断层向另一层渗漏时,断层附近的栅格块体有效应力增大,而栅格块体孔隙压力减小。这反过来又会减少打滑的倾向。因此,这种情况下的传输率也会降低到小于故障重新激活时的传输率。该算法允许断层重新激活或停用,以应对储层压力变化。并对断层的滑动位移进行了估计。该方法在多维多相流模拟器中实现,以证明利用地质力学预测断层再激活的优势,断层再激活可能导致流体从储层泄漏到其他区域或地面。给出了两个合成场和一个场三个实例来说明该方法的应用。所提出的断层再激活建模方法适用于任何具有地质力学能力的流体流动模拟器。它旨在研究和设计安全注入策略,以避免意外的故障重新激活。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Modeling Fault Reactivation Triggered by Fluid Injection
With increased focus on CO2 storage, hydraulic fracturing, and steam injection operations in recent years, understanding of fluid induced seismicity has drawn a lot of attention amongst researchers and practicing engineers. Reactivation of existing dormant faults due to injection operations can lead to flow through or along the fault from the reservoir to undesirable zones. It poses a serious challenge that requires careful study so that measures could be taken to avoid such occurrence. In this paper, a method is presented where geomechanical response is used to compute the slip tendency when the stress changes in a reservoir due to fluid injection. The slip tendency is considered as the main variable to determine whether the fault is reactivated or not. It is computed based on the effective stress normal to the fault surface, and the tangential stress. When the effective stress on a fault surface is reduced due to the increase of pore pressure in grid-blocks adjacent to the fault, it can potentially make the slip tendency exceed the critical limit. In such a case, the transmissibility of grid-blocks on both sides of the fault are increased to allow the fluid to flow into the fault and subsequently along the fault. When the fluid leaks from the reservoir to another zone through the fault, the effective stress on grid-blocks adjacent to the fault increases as the pore pressures in those grid-blocks decrease. This will in turn reduce the slip tendency. Therefore, the transmissibility in this case will also decrease to a value smaller than the one when the fault reactivated. The algorithm allows the fault to be reactivated or deactivated to cope with the pressure change in the reservoir. The slip displacement at the fault is also estimated. The method is implemented in a multidimensional, multiphase flow simulator to demonstrate the advantages of using geomechanics for predicting fault reactivation, which can lead to leakage of fluids from the reservoir to other zones or to the surface. Three examples, two synthetic and one field, are presented to illustrate application of the procedure. The proposed method of fault reactivation modeling is suitable for implementing in any fluid flow simulator with geomechanics capability. It is intended for studying and designing of safe injection strategies that avoid undesirable fault reactivation.
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