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Note on the instability mechanism of gravity-driven unsaturated slow flow in porous media.
The European Physical Journal E ( IF 1.8 ) Pub Date : 2020-02-17 , DOI: 10.1140/epje/i2020-11937-0 Zhen-Ting Wang 1, 2 , Ya-Ning Chen 1
中文翻译：
注意多孔介质中重力驱动的非饱和慢流的失稳机理。
The European Physical Journal E ( IF 1.8 ) Pub Date : 2020-02-17 , DOI: 10.1140/epje/i2020-11937-0 Zhen-Ting Wang 1, 2 , Ya-Ning Chen 1
Affiliation
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.Graphical abstract
中文翻译：
注意多孔介质中重力驱动的非饱和慢流的失稳机理。
摘要。
毛细管模型表明，空气-水界面的表面张力不会引起砂土中重力驱动的非饱和慢流的不稳定性。图形概要
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