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Flows Through Real Porous Media: X-Ray Computed Tomography, Experiments, and Numerical Simulations

机译:流过真实的多孔介质:X射线计算机断层扫描,实验和数值模拟

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Two different direct-forcing immersed boundary methods (IBMs) were applied for the purpose of simulating slow flow through a real porous medium: the volume penalization IBM and the stress IBM. The porous medium was a random close packing of about 9000 glass beads in a round tube. The packing geometry was determined from an X-ray computed tomography (CT) scan in terms of the distribution of the truncated solid volume fraction (either 0 or 1) on a three-dimensional Cartesian grid. The scan resolution corresponded to 19.3 grid cells over the mean bead diameter. A facility was built to experimentally determine the permeability of the packing. Numerical simulations were performed for the same packing based on the CT scan data. For both IBMs the numerically determined permeability based on the Richardson extrapolation was just 10% lower than the experimentally found value. As expected, at finite grid resolution the stress IBM appeared to be the most accurate IBM.
机译:为了模拟通过真实多孔介质的缓慢流动,应用了两种不同的直接强制浸入边界方法(IBM):体积损失IBM和压力IBM。多孔介质是在圆管中随机密堆积约9000个玻璃珠。根据X射线计算机断层扫描(CT)扫描,根据三维笛卡尔网格上截断的固体体积分数(0或1)的分布确定填充几何形状。扫描分辨率对应于平均磁珠直径上的19.3个网格单元。建立了一个设施,以实验确定填料的渗透性。根据CT扫描数据对同一包装进行了数值模拟。对于两个IBM而言,基于Richardson外推法的数值确定的渗透率仅比实验发现的值低10%。不出所料,在有限的网格分辨率下,压力IBM似乎是最准确的IBM。

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