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A Technique for Averaging Matrix-Fracture Fluid Transfer Rates for Multiple Displacement Processes in a Naturally Fractured Reservoir Model

机译:一种用于在天然裂缝储层模型中进行多个位移过程的矩阵断裂流体传递速率的技术

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A common method of modeling naturally fractured reservoirs is a dual porosity approach that uses two identical grids superimposed on each other. Porosity in one grid represents pore space within matrix rock. In the other it represents fracture space between blocks of matrix rock. Fluid transfer rates between corresponding fracture and matrix grid nodes due to capillary pressure and gravity effects are determined from the results of independent simulations that model displacement of fluids in the matrix by fluids from the fracture. This paper presents details of a technique for averaging results of these independent simulations when multiple displacement processes are expected in the reservoir. Motivation came from the need to model a naturally fractured field in which water was first injected below the oil zone in a peripheral waterflood. At the end of the waterflood, gas was injected at the top of the oil zone as the second part of a double displacement process. Fluids in the matrix rock were expected to be displaced by fluids from the fracture network with the following processes: water displacing oil, oil displacing water, and gas displacing oil and water.
机译:一种普遍的模拟自然裂缝储层的方法是一种双孔隙率方法,其使用彼此叠加的两个相同的网格。一个网格中的孔隙率代表了基质岩石内的孔隙空间。在另一个中,它代表了矩阵岩石块之间的裂缝空间。由于毛细管压力和重力效应导致的相应裂缝和基质网格节点之间的流体传递速率由独立模拟的结果确定通过裂缝的流体在基质中的流体位移。本文介绍了在储层中预期多个位移过程时,用于平均这些独立模拟的结果的细节。动机来自需要模拟一种自然裂缝的领域,其中在外周水料中首先在油区下方注入水。在水泡的末端,作为双位移过程的第二部分,在油区的顶部注入气体。预期基质岩石中的流体通过来自裂缝网络的流体流离失所程,下列方法:水位油,油置换水和气体置换油和水。

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