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Handling domain discontinuity in a subsurface grid model with the help of grid optimization techniques

机译:借助网格优化技术处理地下网格模型中的区域不连续性

摘要

Method for mapping a 3D grid or mesh from a faulted subsurface domain to a continuous design domain, wherein the grid may be used to represent a discrete model of a subsurface material property (such as permeability) to use, for example, in a reservoir simulator. The mapping is geometry-based, not physics-based. The mapping is determined by an iterative optimization procedure designed to penalize deformation of tessellated mesh cells (703) in the design domain compared to their geometric quality in the faulted domain (701), but subject to stitching constraints (702) appearing as a penalty term or Lagrange multiplier term in the optimization objective function to influence the final mesh to co-locate pairs of points identified on opposite sides of a fault as having been located together before the fault occurred.
机译:用于将3D网格或网格从有缺陷的地下区域映射到连续设计区域的方法,其中网格可用于表示地下材料属性(例如渗透率)的离散模型,以用于例如储层模拟器。映射是基于几何的,而不是基于物理的。映射是通过迭代优化过程确定的,该迭代优化过程旨在与在故障域(701)中的几何质量相比,在设计域中对棋盘形网格(703)的变形进行惩罚,但是受到作为约束项出现的缝合约束(702)的影响优化目标函数中的“拉格朗日”乘数项或“拉格朗日乘数”项,以影响最终网格,以共同定位在故障的相对侧确定为在故障发生之前已经在一起的点对。

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