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Streamline Simulation of Water Injection in Naturally Fractured Reservoirs

机译:自然裂缝储层中注水的流模拟

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Until recently streamline simulators were limited to single-porosity systems and not suitable for modeling fluid flow and transport in naturally fractured reservoirs. Describing fluid transport in naturally fractured reservoirs entails additional challenge because of the complicated physics arising from matrix-fracture interactions. In this paper thestreamline-based simulation is generalized to describe fluid transport in naturally fractured reservoirs through a dual-media approach. The fractures and matrix are treated as separate continua that are connected through a transfer function, as in conventional finite difference simulators for modeling fractured systems. The transfer functions that describe fluid exchange between the fracture and matrix system can be implemented easily within the framework of the current single-porosity streamline models. In particular, the streamline time of flight concept is utilized to develop a general dual porosity dual permeability system of equations for water injection in naturally fractured reservoirs. We solve the saturations equations using an operator splitting approach that involves ‘convection’ along streamline followed ‘matrix- fracture’ exchange calculations on the grid. Our formulation reduces to the commonly used dual porosity model when the flow in the matrix is considered negligible. We have accounted for the matrix-fracture interactions using two different transfer functions: the conventional transfer function (CTF) and an empirical transfer function (ETF). The ETF allows for analytical solution of the saturation equation for dual porosity systems and is used to validate the numerical implementation. We also compare our results with a commercial finite-difference simulator for waterflooding in five spot and nine-spot patterns. For both dual porosity and dual permeability formulation, the streamline approach shows close agreement in terms of recovery histories and saturation profiles with a marked reduction in numerical dispersion and grid orientation ef fects. An examination of the scaling behavior of the computation time indicates that the streamline approach is likely to result in significant savings for large- scale field applications.
机译:直到最近的简化模拟器局限于单孔隙度系统,不适合于在天然裂缝储层中建模流体流动和运输。描述自然裂缝储层中的流体运输由于基质骨折相互作用而产生的复杂物理而导致额外的挑战。在本文中,基于线的模拟通常通过双媒体方法描述自然碎储层中的流体输送。裂缝和基质被视为通过传递函数连接的单独连续,如在用于建模裂缝系统的传统有限差分模拟器中。描述裂缝和矩阵系统之间的流体交换的传递函数可以容易地在当前单孔隙度流线模型的框架内实现。特别地,利用飞行概念的流线时间来开发一种用于在天然裂缝储层中注射注水方程的一般双孔隙率双渗透系统。我们使用操作员分割方法解决饱和方程,涉及沿着流线“对流”的“对流”遵循“矩阵 - 骨折”交换计算。当认为矩阵中的流动忽略不计时,我们的配方减少了常用的双孔隙度模型。我们已经考虑了使用两种不同传递函数的矩阵 - 断裂相互作用:传统的传递函数(CTF)和经验传递函数(ETF)。 ETF允许双孔隙系统饱和方程的分析解,用于验证数值实现。我们还将结果与商业有限差异模拟器进行了比较,用于在五个斑点和九个点图案中的水上浇灌。对于双孔隙度和双渗透性制剂,流线线方法在回收历史和饱和谱方面显示了密切的协议,并且数值分散和网格取向EF Fects的标记降低。对计算时间的缩放行为的检查表明,流线方法可能会导致大型现场应用程序的显着节省。

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