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The foam drainage equation for drainage dynamics in unsaturated porous media
Year:
2017
Source of publication :
Water Resources Research
Authors :
Assouline, Shmuel
;
.
Volume :
53
Co-Authors:
Lehmann, P.
Hoogland, F.
Or, D.
Facilitators :
From page:
5706
To page:
5724
(
Total pages:
19
)
Abstract:
Similarity in liquid-phase configuration and drainage dynamics of wet foam and gravity drainage from unsaturated porous media expands modeling capabilities for capillary flows and supplements the standard Richards equation representation. The governing equation for draining foam (or a soil variant termed the soil foam drainage equation—SFDE) obviates the need for macroscopic unsaturated hydraulic conductivity function by an explicit account of diminishing flow pathway sizes as the medium gradually drains. The study provides new and simple analytical expressions for drainage rates and volumes from unsaturated porous media subjected to different boundary conditions. Two novel analytical solutions for saturation profile evolution were derived and tested in good agreement with a numerical solution of the SFDE. The study and the proposed solutions rectify the original formulation of foam drainage dynamics of Or and Assouline (2013). The new framework broadens the scope of methods available for quantifying unsaturated flow in porous media, where the intrinsic conductivity and geometrical representation of capillary drainage could improve understanding of colloid and pathogen transport. The explicit geometrical interpretation of flow pathways underlying the hydraulic functions used by the Richards equation offers new insights that benefit both approaches
Note:
Related Files :
drainage
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More details
DOI :
DOI: 10.1002/2017WR020361
Article number:
0
Affiliations:
Database:
Google Scholar
Publication Type:
article
;
.
Language:
Editors' remarks:
ID:
18360
Last updated date:
02/03/2022 17:27
Creation date:
16/04/2018 23:18
Scientific Publication
The foam drainage equation for drainage dynamics in unsaturated porous media
53
Lehmann, P.
Hoogland, F.
Or, D.
The foam drainage equation for drainage dynamics in unsaturated porous media
Similarity in liquid-phase configuration and drainage dynamics of wet foam and gravity drainage from unsaturated porous media expands modeling capabilities for capillary flows and supplements the standard Richards equation representation. The governing equation for draining foam (or a soil variant termed the soil foam drainage equation—SFDE) obviates the need for macroscopic unsaturated hydraulic conductivity function by an explicit account of diminishing flow pathway sizes as the medium gradually drains. The study provides new and simple analytical expressions for drainage rates and volumes from unsaturated porous media subjected to different boundary conditions. Two novel analytical solutions for saturation profile evolution were derived and tested in good agreement with a numerical solution of the SFDE. The study and the proposed solutions rectify the original formulation of foam drainage dynamics of Or and Assouline (2013). The new framework broadens the scope of methods available for quantifying unsaturated flow in porous media, where the intrinsic conductivity and geometrical representation of capillary drainage could improve understanding of colloid and pathogen transport. The explicit geometrical interpretation of flow pathways underlying the hydraulic functions used by the Richards equation offers new insights that benefit both approaches
Scientific Publication
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