Literature DB >> 32056018

Note on the instability mechanism of gravity-driven unsaturated slow flow in porous media.

Zhen-Ting Wang1,2, Ya-Ning Chen3.   

Abstract

A capillary tube model reveals that the surface tension at the air-water interface cannot cause the instability of gravity-driven unsaturated slow flow in sandy soils.

Keywords:  Flowing Matter: Liquids and Complex Fluids

Year:  2020        PMID： 32056018     DOI： 10.1140/epje/i2020-11937-0

Source DB:  PubMed          Journal:  Eur Phys J E Soft Matter        ISSN： 1292-8941            Impact factor:   1.890


  3 in total

1.  Stability analysis of a phase-field model of gravity-driven unsaturated flow through porous media.

Authors:  Luis Cueto-Felgueroso; Ruben Juanes
Journal:  Phys Rev E Stat Nonlin Soft Matter Phys       Date:  2009-03-09

2.  Nonlocal interface dynamics and pattern formation in gravity-driven unsaturated flow through porous media.

Authors:  Luis Cueto-Felgueroso; Ruben Juanes
Journal:  Phys Rev Lett       Date:  2008-12-12       Impact factor: 9.161

3.  Rain water transport and storage in a model sandy soil with hydrogel particle additives.

Authors:  Y Wei; D J Durian
Journal:  Eur Phys J E Soft Matter       Date:  2014-10-27       Impact factor: 1.890
  3 in total

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