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Unstructured-Coarse-Grid Generation Using Background-Grid Approach

机译:使用背景网格方法生成非结构化粗网格

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Reservoir flow simulation involves subdivision of the physical domain into a number of gridblocks. This is best accomplished with optimized gridpoint density and a minimized number of gridblocks, especially for coarse-grid generation from a fine-grid geological model.rnIn any coarse-grid generation, proper distribution of gridpoints, which form the basis of numerical gridblocks, is a challenging task. We show that this can be achieved effectively by a novel grid-generation approach based on a background grid that stores gridpoint spacing parameters.rnSpacing parameter (L) can be described by Poisson's equation (▽~2L = G), where the local density of gridpoints is controlled by a variable source term (G); see Eq. 1. This source term can be based on different gridpoint density indicators, such as permeability variations, fluid velocity, or their combination (e.g., vorticity) where they can be extracted from the reference fine grid. Once a background grid is generated, advancing-front triangulation (AFT) and then Delaunay tessellation are invoked to form the final (coarse) gridblocks. The algorithm produces grids varying smoothly from high- to low-density gridpoints, thus minimizing use of grid-smoothing and -optimization techniques. This algorithm is quite flexible, allowing choice of the gridding indicator, hence providing the possibility of comparing the grids generated with different indicators and selecting the best.rnIn this paper, the capabilities of approach in generation of unstructured coarse grids from fine geological models are illustrated using 2D highly heterogeneous test cases. Flexibility of algorithm to gridding indicator is demonstrated using vorticity, permeability variation, and velocity. Quality of the coarse grids is evaluated by comparing their two-phase-flow simulation results to those of fine grid and uniform coarse grid. Results demonstrate the robustness and attractiveness of the approach, as well as relative quality/performance of grids generated by using different indicators.
机译:储层流动模拟涉及将物理域细分为多个网格块。这是通过优化网格点密度和最少数量的网格块来实现的,特别是对于从细网格地质模型生成粗网格的情况。rn在任何粗网格生成中,网格点的适当分布是数字网格块的基础,一项艰巨的任务。我们表明,这可以通过基于存储栅格点间距参数的背景栅格的新颖栅格生成方法有效地实现。rn间距参数(L)可用泊松方程(▽〜2L = G)描述,其中局部密度为网格点由可变源项(G)控制;参见式1.此源项可以基于不同的网格点密度指标,例如渗透率变化,流体速度或其组合(例如,涡度),可以从参考精细网格中提取它们。生成背景网格后,将调用前向三角剖分(AFT),然后调用Delaunay细分,以形成最终的(粗略)网格块。该算法可生成从高到低密度网格点平滑变化的网格,从而最大程度地减少了网格平滑和优化技术的使用。该算法非常灵活,可以选择网格指示符,因此可以比较使用不同指示符生成的网格并选择最佳网格。rn本文说明了从精细地质模型生成非结构化粗网格的方法的功能。使用2D高度异构的测试用例。使用涡度,渗透率变化和速度来证明算法对网格指示器的灵活性。通过比较粗网格的两相流模拟结果与细网格和均匀粗网格的仿真结果,可以评估粗网格的质量。结果证明了该方法的鲁棒性和吸引力,以及使用不同指标生成的网格的相对质量/性能。

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