Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid

Soil-water retention curve (SWRC) has a wide application in geoenvironmental engineering from the predication of unsaturated shear strength to transient two-phase flow and stability analyses. Although various SWRC models have been proposed to take into account some influencing factors, less attentio...

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Main Authors: Sadeghi Hamed, Golaghaei Darzi Ali
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:MATEC Web of Conferences
Online Access:https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_02001.pdf
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spelling doaj-f8cad6540e7141fcabed66ba66169b472021-05-04T12:21:53ZengEDP SciencesMATEC Web of Conferences2261-236X2021-01-013370200110.1051/matecconf/202133702001matecconf_PanAm-Unsat2021_02001Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluidSadeghi Hamed0Golaghaei Darzi Ali1Assistant Professor, Department of Civil Engineering, Sharif University of TechnologyM.Sc. Student, Department of Civil Engineering, Sharif University of TechnologySoil-water retention curve (SWRC) has a wide application in geoenvironmental engineering from the predication of unsaturated shear strength to transient two-phase flow and stability analyses. Although various SWRC models have been proposed to take into account some influencing factors, less attention has been given to consider the effects of pore fluid osmotic potential. Therefore, the key objective of this study is to extend van Genchten’s model so that osmotic potential is considered as an independent factor governing the SWRC behavior. The new model comprises only six variables, which can be calibrated through minimal experimental measurements. More importantly, most of the model parameters have physical meaning by correlating macroscopic volumetric behavior and general trends of SWRC to osmotic potential. The results of validation tests revealed that the new osmotic-dependent SWRC model can predict the retention data in terms of both total and matric suction for two different soils and various molar concentrations very good. The proposed modeling approach does not require any advanced mercury intrusion porosimetry (MIP) tests, yet it can deliver excellent predictions by calibrating only six parameters which are far less than those incorporated into similar models for saline water permeating through the pore structure.https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_02001.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Sadeghi Hamed
Golaghaei Darzi Ali
spellingShingle Sadeghi Hamed
Golaghaei Darzi Ali
Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
MATEC Web of Conferences
author_facet Sadeghi Hamed
Golaghaei Darzi Ali
author_sort Sadeghi Hamed
title Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
title_short Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
title_full Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
title_fullStr Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
title_full_unstemmed Modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
title_sort modelling of soil-water retention curve considering the effects of existing salt solution in the pore fluid
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2021-01-01
description Soil-water retention curve (SWRC) has a wide application in geoenvironmental engineering from the predication of unsaturated shear strength to transient two-phase flow and stability analyses. Although various SWRC models have been proposed to take into account some influencing factors, less attention has been given to consider the effects of pore fluid osmotic potential. Therefore, the key objective of this study is to extend van Genchten’s model so that osmotic potential is considered as an independent factor governing the SWRC behavior. The new model comprises only six variables, which can be calibrated through minimal experimental measurements. More importantly, most of the model parameters have physical meaning by correlating macroscopic volumetric behavior and general trends of SWRC to osmotic potential. The results of validation tests revealed that the new osmotic-dependent SWRC model can predict the retention data in terms of both total and matric suction for two different soils and various molar concentrations very good. The proposed modeling approach does not require any advanced mercury intrusion porosimetry (MIP) tests, yet it can deliver excellent predictions by calibrating only six parameters which are far less than those incorporated into similar models for saline water permeating through the pore structure.
url https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_02001.pdf
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