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Simulation of multiphase flow in fractured reservoirs using a fracture-only model with transfer functions

机译:使用带传递函数的仅裂缝模型模拟裂缝储层中的多相流

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We present a fracture-only reservoir simulator for multiphase flow: the fracture geometry is modeled explicitly, while fluid movement between fracture and matrix is accommodated using empirical transfer functions. This is a hybrid between discrete fracture discrete matrix modeling where both the fracture and matrix are gridded and dual-porosity or dual-permeability simulation where both fracture and matrix continua are upscaled. The advantage of this approach is that the complex fracture geometry that controls the main flow paths is retained. The use of transfer functions, however, simplifies meshing and makes the simulation method considerably more efficient than discrete fracture discrete matrix models. The transfer functions accommodate capillary- and gravity-mediated flow between fracture and matrix and have been shown to be accurate for simple fracture geometries, capturing both the early- and late-time average behavior. We verify our simulator by comparing its predictions with simulation results where the fracture and matrix are explicitly modeled. We then show the utility of the approach by simulating multiphase flow in a geologicallyrnrealistic fracture network. Waterflooding runs reveal the fraction of the fracture-matrix interface area that is infiltrated by water so that matrix imbibition can occur. The evolving fraction of the fracture-matrix interface area turns out to be an important characteristic of any particular fracture system to be used as a scaling parameter for capillary driven fracture-matrix transfer.
机译:我们为多相流提供了一个仅裂缝的油藏模拟器:裂缝的几何形状是明确建模的,而裂缝和基质之间的流体运动是使用经验传递函数来适应的。这是离散裂缝离散矩阵建模(其中裂缝和矩阵都网格化)与双孔隙率或双重渗透率仿真(其中裂缝和矩阵连续性都按比例放大)之间的混合。这种方法的优点是保留了控制主要流动路径的复杂裂缝几何形状。但是,传递函数的使用简化了网格划分,并使模拟方法比离散裂缝离散矩阵模型有效得多。传递函数可适应裂缝和基质之间的毛细作用和重力作用,并且已被证明对于简单的裂缝几何形状是准确的,可以捕获早期和晚期的平均行为。我们通过将仿真器的预测结果与模拟结果进行比较,从而对仿真器进行了验证,其中明确地模拟了裂缝和基质。然后,我们通过模拟地质现实裂缝网络中的多相流来显示该方法的实用性。注水运行揭示出裂缝-基质界面区域的一部分被水渗透,从而可能发生基质吸收。事实证明,裂缝-基质界面区域的演化分数是任何特定裂缝系统的重要特征,可用作毛细管驱动裂缝-基质转移的定标参数。

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