流-地-力耦合双三维网格中具有多弯曲和相交断层的储层建模新方法

Abdulrahman Bubshait, B. Jha
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摘要

本文采用一种新颖的网格划分方法,建立了盖层-储层-基底系统注采耦合流动-地质力学模型,该系统具有类似于地堑-地堑或合成-反断裂的共轭弯曲断裂结构。该例程以CMG网格文件格式提供网格中每个角的3D坐标。我们的工作流程使我们能够将两个故障表示为3D对象,并为其分配实际的物理属性和故障的尺寸。这是非常有利的,因为传统的结构网格不能在不牺牲其几何形状或流体力学特性的情况下表示弯曲断层、连接断层或断层交叉点。牺牲断层的弯曲几何形状会导致计算基底区诱发应力的准确性下降,而基底区是美国已知的大多数诱发地震事件的发生地。生成的网格用于孔隙弹塑性模拟,以研究位于两个共轭断层边界的上盘块(地堑)区域的油藏生产后产生的应力变化。生产过程中孔隙压力的变化引起了储层和基底的总应力和有效应力的变化。根据断层流变学和摩擦参数的不同,断层上的剪应力和有效正应力的演化可能导致断层破坏和滑动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Novel Meshing Routine for Modeling Reservoirs with Multiple Curved and Intersecting Faults in Coupled Flow-Geomechanical Dual 3D Grids
We use a novel meshing routine to build a coupled flow-geomechanical model of injection and production in a caprock-reservoir-basement system with two conjugate curved faults that resemble a horst-graben or a synthetic-antithetic fault structure. The routine provides the 3D coordinates of each corner in the grid in a CMG grid file format. Our workflow enables us to represent the two faults as 3D objects to which we assign actual physical properties and dimensions of the faults. This is highly advantageous because traditional structured grids cannot represent curved faults, connected faults, or fault intersections without sacrificing either their geometry or their hydromechanical properties. Sacrificing the curved geometry of faults results in a loss of accuracy in computing the induced stresses in the basement region, which is known to host most of the recorded induced seismic events in US. The generated grid was used in a poro-elastoplastic simulation to examine stress changes resulting after production from a reservoir located in the hanging wall block (graben) region bounded by the two conjugate faults. The change in pore pressure due to production causes changes in both the total stress and the effective stress in the reservoir and the basement. The evolution of the shear and effective normal stresses on the faults may induce fault failure and slip depending on the fault rheology and friction parameters.
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