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三维多孔介质中两相流的有效流变学:实验与模拟

Effective Rheology of Two-Phase Flow in Three-Dimensional Porous Media: Experiment and Simulation.

作者信息

Sinha Santanu, Bender Andrew T, Danczyk Matthew, Keepseagle Kayla, Prather Cody A, Bray Joshua M, Thrane Linn W, Seymour Joseph D, Codd Sarah L, Hansen Alex

机构信息

Beijing Computational Science Research Center, 10 East Xibeiwang Road, Haidian District, Beijing, 100193 China.

Department of Mechanical and Industrial Engineering, Montana State University, Bozeman, MT USA.

出版信息

Transp Porous Media. 2017;119(1):77-94. doi: 10.1007/s11242-017-0874-4. Epub 2017 Jun 13.

Abstract

We present an experimental and numerical study of immiscible two-phase flow of Newtonian fluids in three-dimensional (3D) porous media to find the relationship between the volumetric flow rate () and the total pressure difference ([Formula: see text]) in the steady state. We show that in the regime where capillary forces compete with the viscous forces, the distribution of capillary barriers at the interfaces effectively creates a yield threshold ([Formula: see text]), making the fluids reminiscent of a Bingham viscoplastic fluid in the porous medium. In this regime, depends quadratically on an excess pressure drop ([Formula: see text]). While increasing the flow rate, there is a transition, beyond which the overall flow is Newtonian and the relationship is linear. In our experiments, we build a model porous medium using a column of glass beads transporting two fluids, deionized water and air. For the numerical study, reconstructed 3D pore networks from real core samples are considered and the transport of wetting and non-wetting fluids through the network is modeled by tracking the fluid interfaces with time. We find agreement between our numerical and experimental results. Our results match with the mean-field results reported earlier.

摘要

我们对牛顿流体在三维(3D)多孔介质中的不混溶两相流进行了实验和数值研究,以找出稳态下体积流量()与总压差([公式:见正文])之间的关系。我们表明,在毛细力与粘性力相互竞争的区域,界面处毛细屏障的分布有效地产生了一个屈服阈值([公式:见正文]),使得流体在多孔介质中类似于宾汉粘塑性流体。在这个区域, 与过剩压降([公式:见正文])呈二次方关系。当增加流量时,会有一个转变,超过这个转变后,整体流动变为牛顿流体,且关系呈线性。在我们的实验中,我们使用一列玻璃珠构建了一个模型多孔介质,用于输送去离子水和空气这两种流体。对于数值研究,考虑了从真实岩心样本重建的三维孔隙网络,并通过随时间跟踪流体界面来模拟润湿流体和非润湿流体在网络中的传输。我们发现数值结果与实验结果一致。我们的结果与先前报道的平均场结果相符。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3c06/5522531/d57177893cf9/11242_2017_874_Fig1_HTML.jpg

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