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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Format: | conferenceObject biblioteca |
Language: | eng |
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2013
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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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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 |
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Biblioteca 'Ing. Agrónomo Moisés Farber' de la Facultad de Ciencias Agropecuarias |
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Suelos no saturados Geofísica Suelo colapsables Mapeo de agua Concentración de sal Suelos no saturados Geofísica Suelo colapsables Mapeo de agua Concentración de sal |
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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. |
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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 |
_version_ |
1756010463827591168 |