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Use of Improved Gridding Technique in Coupled Geomechanics and Compositional Reservoir Flow Simulation

机译:改进的网格技术在耦合地质力学和组成储层流动模拟中的使用

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Coupled reservoir flow and geomechanics simulations are important in many compositional fluid flow processes like water- alternating-miscible gas injection and CO2 storage. The intention in these models is to understand the effect of stress and deformation consequent to changes in reservoir flow and fluid phase behavior. Safe CO2 storage in deep saline aquifers calls for evaluation of cap-rock and seal integrity via stress responses so that undesired leakage through the seals could be avoided. In the geomechanics calculations unknowns at a large number of finite element nodes need to be solved at each coupling step, which can lead to overwhelmingly large computation time for the coupled simulations. Recently an improved gridding technique was applied to model coupled geomechanics and reservoir flow in a thermal simulator. In this technique, a dual grid system consisting of separate grids for the reservoir flow and the geomechanics calculations is used. The exchange of information of the variables between reservoir and geomechanics simulators was accomplished in an iteratively coupled fashion. This method showed significant reduction in CPU time compared to single grid coupled simulation. This paper presents an extension of the above method wherein the geomechanics model is coupled with an equation-of-state compositional simulator in place of a thermal simulator. Use of the dual grid system is demonstrated through simulation models for two compositional processes. Comparison between a dual grid system and a single grid system is presented. The results show that there is substantial saving in computation time and memory requirement without significant loss in the quality of flow or geomechanical results. The dual grid system presented in the paper can be used to model compositional processes in stress-sensitive reservoirs to yield satisfactory results in considerably less time than would be possible through a conventional single grid system for coupled flow and deformation simulation.
机译:耦合储层流量和地质力学模拟在许多组成流体流程过程中是重要的,如水交交流气体注射和CO 2储存。这些模型中的意图是了解压力和变形的影响,从而改变储层流动和流体相位行为。安全的CO2储存在深盐含水层中,通过应力响应来评估帽岩和密封完整性,从而可以避免通过密封件的不期望的泄漏。在每个耦合步骤中需要在每个耦合步骤中解决大量有限元节点的GeoMencharics计算,这可能导致耦合模拟的压倒性地增加了大量的计算时间。最近,将改进的网格技术应用于热模拟器中的模型耦合地质力学和储存器流。在该技术中,使用由用于储存流的单独网格和地质力学计算组成的双电网系统。储层和地质力学模拟器之间的变量的信息交换以迭代耦合的方式完成。与单网格耦合仿真相比,该方法显示CPU时间显着降低。本文介绍了上述方法的扩展,其中地质力学模型与状态 - 状态方程式模拟器耦合到代替热模拟器。通过模拟模型来证明双电网系统的使用,用于两个组成过程。提出了双电网系统和单个网格系统之间的比较。结果表明,计算时间和内存要求存在显着节省,而流或地质力学效果的质量造成显着损失。本文中提出的双电网系统可用于在应力敏感储存器中模拟组成过程,以产生令人满意的结果,其时间比传统的单个网格系统可以耦合流动和变形模拟。

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