Estimating soil suction from electrical resistivity

Soil suction and resistivity strongly depend on the degree of soil saturation and, therefore, both are used for estimating water content variations. The main difference between them is that soil suction is measured using tensiometers, which give point information, while resistivity is obtained by to...

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Main Authors: E. Piegari, R. Di Maio
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/13/2369/2013/nhess-13-2369-2013.pdf
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spelling doaj-eb0c7e2e8e9b4ed9b7fc4f299db489662020-11-25T00:47:53ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812013-09-011392369237910.5194/nhess-13-2369-2013Estimating soil suction from electrical resistivityE. PiegariR. Di MaioSoil suction and resistivity strongly depend on the degree of soil saturation and, therefore, both are used for estimating water content variations. The main difference between them is that soil suction is measured using tensiometers, which give point information, while resistivity is obtained by tomography surveys, which provide distributions of resistivity values in large volumes, although with less accuracy. In this paper, we have related soil suction to electrical resistivity with the aim of obtaining information about soil suction changes in large volumes, and not only for small areas around soil suction probes. We derived analytical relationships between soil matric suction and electrical resistivity by combining the empirical laws of van Genuchten and Archie. The obtained relationships were used to evaluate maps of soil suction values in different ashy layers originating in the explosive activity of the Mt Somma-Vesuvius volcano (southern Italy). Our findings provided a further example of the high potential of geophysical methods in contributing to more effective monitoring of soil stress conditions; this is of primary importance in areas where rainfall-induced landslides occur periodically.http://www.nat-hazards-earth-syst-sci.net/13/2369/2013/nhess-13-2369-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Piegari
R. Di Maio
spellingShingle E. Piegari
R. Di Maio
Estimating soil suction from electrical resistivity
Natural Hazards and Earth System Sciences
author_facet E. Piegari
R. Di Maio
author_sort E. Piegari
title Estimating soil suction from electrical resistivity
title_short Estimating soil suction from electrical resistivity
title_full Estimating soil suction from electrical resistivity
title_fullStr Estimating soil suction from electrical resistivity
title_full_unstemmed Estimating soil suction from electrical resistivity
title_sort estimating soil suction from electrical resistivity
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2013-09-01
description Soil suction and resistivity strongly depend on the degree of soil saturation and, therefore, both are used for estimating water content variations. The main difference between them is that soil suction is measured using tensiometers, which give point information, while resistivity is obtained by tomography surveys, which provide distributions of resistivity values in large volumes, although with less accuracy. In this paper, we have related soil suction to electrical resistivity with the aim of obtaining information about soil suction changes in large volumes, and not only for small areas around soil suction probes. We derived analytical relationships between soil matric suction and electrical resistivity by combining the empirical laws of van Genuchten and Archie. The obtained relationships were used to evaluate maps of soil suction values in different ashy layers originating in the explosive activity of the Mt Somma-Vesuvius volcano (southern Italy). Our findings provided a further example of the high potential of geophysical methods in contributing to more effective monitoring of soil stress conditions; this is of primary importance in areas where rainfall-induced landslides occur periodically.
url http://www.nat-hazards-earth-syst-sci.net/13/2369/2013/nhess-13-2369-2013.pdf
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