Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands

Electrical resistivity of soils can be used to evaluate the level of contamination in soils in geophysical prospection tests. The chemical composition of pore fluid also corresponds to a given water potential, named as osmotic suction. Therefore both electrical resistivity and osmotic suction can be...

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Main Authors: Borges Inês, Gingine Vikas, Cardoso Rafaela
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03019.pdf
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spelling doaj-8e33b530ea644a62be8d70ba70ef4e6d2021-04-02T12:22:41ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011950301910.1051/e3sconf/202019503019e3sconf_e-unsat2020_03019Preliminary study on the contribution of osmotic effects for the electrical resistivity of sandsBorges InêsGingine Vikas0Cardoso RafaelaKLS Gogte Institute of TechnologyElectrical resistivity of soils can be used to evaluate the level of contamination in soils in geophysical prospection tests. The chemical composition of pore fluid also corresponds to a given water potential, named as osmotic suction. Therefore both electrical resistivity and osmotic suction can be related when soil is saturated. This paper investigates their relationship when the soil is not saturated. The osmotic suction and electrical resistivity were measured for uniform grading size samples of sand prepared with different concentrations of an ionic leachate from a real landfield. Both were measured also for the fluid with the different concentrations. Suction was measured for different degrees of saturation using the ionic fluid for the different concentrations. The soil osmotic suction is similar to the osmotic suction of the pore fluid independently from the degree of saturation, and the differences in electrical resistivity in the saturated samples and pore fluid alone as function of osmotic suction are related by a constant. Although pore fluid composition affects electrical resistivity, when evaluating the electrical resistivity considering the degree of saturation one should pay attention to factors that are related with matric suction instead of osmotic suction.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Borges Inês
Gingine Vikas
Cardoso Rafaela
spellingShingle Borges Inês
Gingine Vikas
Cardoso Rafaela
Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
E3S Web of Conferences
author_facet Borges Inês
Gingine Vikas
Cardoso Rafaela
author_sort Borges Inês
title Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
title_short Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
title_full Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
title_fullStr Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
title_full_unstemmed Preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
title_sort preliminary study on the contribution of osmotic effects for the electrical resistivity of sands
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Electrical resistivity of soils can be used to evaluate the level of contamination in soils in geophysical prospection tests. The chemical composition of pore fluid also corresponds to a given water potential, named as osmotic suction. Therefore both electrical resistivity and osmotic suction can be related when soil is saturated. This paper investigates their relationship when the soil is not saturated. The osmotic suction and electrical resistivity were measured for uniform grading size samples of sand prepared with different concentrations of an ionic leachate from a real landfield. Both were measured also for the fluid with the different concentrations. Suction was measured for different degrees of saturation using the ionic fluid for the different concentrations. The soil osmotic suction is similar to the osmotic suction of the pore fluid independently from the degree of saturation, and the differences in electrical resistivity in the saturated samples and pore fluid alone as function of osmotic suction are related by a constant. Although pore fluid composition affects electrical resistivity, when evaluating the electrical resistivity considering the degree of saturation one should pay attention to factors that are related with matric suction instead of osmotic suction.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03019.pdf
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AT cardosorafaela preliminarystudyonthecontributionofosmoticeffectsfortheelectricalresistivityofsands
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