Application of electrical resistivity for the control of water content and density in loess

Argentinean loess is a typical collapsible soil which strength and stiffness are mainly governed by water content and unit weight. Electrical resistivity of soils depends fundamentally from water content, porosity, and salt concentration in the pore fluid. The interest of this work is to discuss the applicability of electrical resistivity survey to predict variations in density and water content in loess. Samples of loess were prepared in laboratory at varied densities and water contents. The results show that loess resistivity depends mainly on water content and that soil density has little influence. Mapping water content distribution by means of resistivity measurements is possible if salt concentration in pore fluid is known in advance and assumed uniformly distributed in the whole soil mass. A real scale work is described here for which resistivity mapping was used successfully to evaluate distribution of water content in loess formation.

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Bibliographic Details
Main Author: Rinaldi, V.
Format: conferenceObject biblioteca
Language:eng
Published: 2013
Subjects:Suelos no saturados, Geofísica, Suelo colapsables, Mapeo de agua, Concentración de sal,
Online Access:http://hdl.handle.net/11086/29647
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spelling dig-unc-ar-11086-296472022-11-20T09:52:38Z Application of electrical resistivity for the control of water content and density in loess Rinaldi, V. Suelos no saturados Geofísica Suelo colapsables Mapeo de agua Concentración de sal Argentinean loess is a typical collapsible soil which strength and stiffness are mainly governed by water content and unit weight. Electrical resistivity of soils depends fundamentally from water content, porosity, and salt concentration in the pore fluid. The interest of this work is to discuss the applicability of electrical resistivity survey to predict variations in density and water content in loess. Samples of loess were prepared in laboratory at varied densities and water contents. The results show that loess resistivity depends mainly on water content and that soil density has little influence. Mapping water content distribution by means of resistivity measurements is possible if salt concentration in pore fluid is known in advance and assumed uniformly distributed in the whole soil mass. A real scale work is described here for which resistivity mapping was used successfully to evaluate distribution of water content in loess formation. Fil: Rinaldi, V. Universidad Nacional de Córdoba; Argentina. Ingeniería de la Construcción 2022-11-14T16:31:02Z 2022-11-14T16:31:02Z 2013 conferenceObject 978-0-415-62095-6 http://hdl.handle.net/11086/29647 eng Attribution-NonCommercial-ShareAlike 4.0 International https://creativecommons.org/licenses/by-nc-sa/4.0/ Impreso; Electrónico y/o Digital
institution UNC AR
collection DSpace
country Argentina
countrycode AR
component Bibliográfico
access En linea
databasecode dig-unc-ar
tag biblioteca
region America del Sur
libraryname Biblioteca 'Ing. Agrónomo Moisés Farber' de la Facultad de Ciencias Agropecuarias
language eng
topic Suelos no saturados
Geofísica
Suelo colapsables
Mapeo de agua
Concentración de sal
Suelos no saturados
Geofísica
Suelo colapsables
Mapeo de agua
Concentración de sal
spellingShingle Suelos no saturados
Geofísica
Suelo colapsables
Mapeo de agua
Concentración de sal
Suelos no saturados
Geofísica
Suelo colapsables
Mapeo de agua
Concentración de sal
Rinaldi, V.
Application of electrical resistivity for the control of water content and density in loess
description Argentinean loess is a typical collapsible soil which strength and stiffness are mainly governed by water content and unit weight. Electrical resistivity of soils depends fundamentally from water content, porosity, and salt concentration in the pore fluid. The interest of this work is to discuss the applicability of electrical resistivity survey to predict variations in density and water content in loess. Samples of loess were prepared in laboratory at varied densities and water contents. The results show that loess resistivity depends mainly on water content and that soil density has little influence. Mapping water content distribution by means of resistivity measurements is possible if salt concentration in pore fluid is known in advance and assumed uniformly distributed in the whole soil mass. A real scale work is described here for which resistivity mapping was used successfully to evaluate distribution of water content in loess formation.
format conferenceObject
topic_facet Suelos no saturados
Geofísica
Suelo colapsables
Mapeo de agua
Concentración de sal
author Rinaldi, V.
author_facet Rinaldi, V.
author_sort Rinaldi, V.
title Application of electrical resistivity for the control of water content and density in loess
title_short Application of electrical resistivity for the control of water content and density in loess
title_full Application of electrical resistivity for the control of water content and density in loess
title_fullStr Application of electrical resistivity for the control of water content and density in loess
title_full_unstemmed Application of electrical resistivity for the control of water content and density in loess
title_sort application of electrical resistivity for the control of water content and density in loess
publishDate 2013
url http://hdl.handle.net/11086/29647
work_keys_str_mv AT rinaldiv applicationofelectricalresistivityforthecontrolofwatercontentanddensityinloess
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