arXivDaily arXiv每日学术速递 周一至周五更新
arXiv周末暂无论文更新,休息一下吧,周末愉快~~
arXiv 1902.08233physics.flu-dyn
收藏

多孔介质中水对惯性颗粒输运的孔隙尺度研究

A pore-scale study of transport of inertial particles by water in porous media

Max A. Endo Kokubun, Adrian Muntean, Florin A. Radu, Kundan Kumar, Iuliu S. Pop, Eirik Keilegavlen, Kristine Spildo

摘要:

本文研究了多孔介质中水流中惯性颗粒的输运问题。我们的兴趣在于了解颗粒的积聚,包括堵塞的可能性。我们建议,积累可以是流体动力学效应的结果:多孔介质的曲折路径产生的主导应变/涡度,这有利于积累/分散的惯性粒子的区域。数值模拟表明,基本上有两个积累制度确定:低和高流速。当颗粒聚集在高速区域时,在孔喉的入口处,形成堵塞。堵塞物的形成显著地改变了流动,因为孔隙的部分堵塞导致局部压力重新分布。这种重新分布可以将上游水流转移到邻近的孔隙中。此外,我们表明,在高速区域的积累发生在非均质介质中,但不是在均匀介质中,在那里我们指的是均匀性相对于孔喉直径的分布。

英文摘要:

We study the transport of inertial particles in water flow in porous media. Our interest lies in understanding the accumulation of particles including the possibility of clogging. We propose that accumulation can be a result of hydrodynamic effects: the tortuous paths of the porous medium generate regions of dominating strain/vorticity, which favour the accumulation/dispersion of the inertial particles. Numerical simulations show that essentially two accumulation regimes are identified: for low and for high flow velocities. When particles accumulate in high-velocity regions, at the entrance of a pore throat, a clog is formed. The formation of a clog significantly modifies the flow, as the partial blockage of the pore causes a local redistribution of pressure. This redistribution can divert the upstream water flow into neighbouring pores. Moreover, we show that accumulation in high velocity regions occurs in heterogeneous media, but not in homogeneous media, where we refer to homogeneity with respect to the distribution of the pore throat diameters.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑