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Image-based simulations of absolute permeability with massively parallel pseudo-compressible stabilised finite element solver

机译:大规模并行拟可压缩稳定有限元求解器基于图像的绝对渗透率模拟

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We apply an accurate parallel stabilised finite element method to solve for Navier-Stokes equations directly on a binarised three-dimensional rock image, obtained by micro-CT imaging. The proposed algorithm has several advantages. First, the linear equal-order finite element space for velocity and pressure is ideal for presenting the pixel images. Second, the algorithm is fully explicit and versatile for describing complex boundary conditions. Third, the fully explicit matrix-free finite element implementation is ideal for parallelism on high-performance computers, similar to lattice Boltzmann. In the last, the memory usage is low compared with lattice Boltzmann or implicit finite volume. We compute the permeability of a range of rock images. The stabilisation parameter may affect the velocity, and an optimal parameter is chosen from the numerical tests. The steady state results are comparable with lattice Boltzmann method and implicit finite volume. The transient behaviour of pseudo-compressible stabilised finite element and lattice Boltzmann method is very similar. Our analysis shows that the stabilised finite element is an accurate and efficient method with low memory cost for the image-based simulations of flow in the pore scale up to 1 billion voxels on 128-GB ram workstation and on distributed clusters.
机译:我们应用精确的并行稳定有限元方法直接在通过微CT成像获得的二值化三维岩石图像上求解Navier-Stokes方程。所提出的算法具有几个优点。首先,速度和压力的线性等阶有限元空间非常适合呈现像素图像。其次,该算法是完全显式的,可用于描述复杂边界条件。第三,与晶格玻尔兹曼相似,完全明确的无矩阵有限元实现是高性能计算机上并行性的理想选择。最后,与格子Boltzmann或隐式有限体积相比,内存使用率较低。我们计算一系列岩石图像的渗透率。稳定参数可能会影响速度,并从数值测试中选择最佳参数。稳态结果与格子玻尔兹曼方法和隐式有限体积相当。拟可压缩稳定有限元的瞬态行为与晶格玻尔兹曼方法非常相似。我们的分析表明,稳定的有限元是一种精确有效的方法,具有低内存成本,可用于基于图像的128 GB内存工作站和分布式簇上的孔尺度高达10亿体素的流动模拟。

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