Geoelectrical investigation for the assessment of groundwater conditions: a case study

An electrical resistivity survey involving Vertical Electrical Soundings (VES) was carried out in the Shooro
 Basin in Southeast Iran in order to study groundwater conditions such as depth, thickness and aquifer boundaries.
 Vertical electrical soundings by Schlumberger array were co...

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Main Authors: M. Nakhaei, G. R. Lashkaripour
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2005-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3244
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spelling doaj-64cbc79ef3b54d56b2dadd9d58db097e2020-11-24T23:23:15ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2005-06-0148610.4401/ag-3244Geoelectrical investigation for the assessment of groundwater conditions: a case studyM. NakhaeiG. R. LashkaripourAn electrical resistivity survey involving Vertical Electrical Soundings (VES) was carried out in the Shooro
 Basin in Southeast Iran in order to study groundwater conditions such as depth, thickness and aquifer boundaries.
 Vertical electrical soundings by Schlumberger array were conducted in this area. The resistivity Schlumberger
 soundings which have a maximum current electrode spacing (AB) ranging from 200 m to 600 m were
 carried out at 207 positions in 19 profiles. Interpretation of these soundings indicates the presence of an alluvial
 aquifer. This aquifer is divided into eastern and western parts by the Shooro River, which comprises a variable
 thickness and resistivity of deposits. The average permeability coefficient and resistivity in the western part, especially
 southwest is higher than the eastern part of the aquifer. Therefore, it seems that Shooro River follows a
 fault zone in the region. The high resistivity of west part is due to the water quality and the existence of alluvial
 fan with coarse grain materials. Low aquifer resistivities in the east are associated with finer materials and also
 brackish water infiltration from the adjacent basin mainly in the central part of the aquifer. Furthermore, zones
 with high yield potential have been determined in this research based on the resistivity data.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3244electrical resistivitysoundingroundwater conditionShooroIran
collection DOAJ
language English
format Article
sources DOAJ
author M. Nakhaei
G. R. Lashkaripour
spellingShingle M. Nakhaei
G. R. Lashkaripour
Geoelectrical investigation for the assessment of groundwater conditions: a case study
Annals of Geophysics
electrical resistivity
sounding
roundwater condition
Shooro
Iran
author_facet M. Nakhaei
G. R. Lashkaripour
author_sort M. Nakhaei
title Geoelectrical investigation for the assessment of groundwater conditions: a case study
title_short Geoelectrical investigation for the assessment of groundwater conditions: a case study
title_full Geoelectrical investigation for the assessment of groundwater conditions: a case study
title_fullStr Geoelectrical investigation for the assessment of groundwater conditions: a case study
title_full_unstemmed Geoelectrical investigation for the assessment of groundwater conditions: a case study
title_sort geoelectrical investigation for the assessment of groundwater conditions: a case study
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2005-06-01
description An electrical resistivity survey involving Vertical Electrical Soundings (VES) was carried out in the Shooro
 Basin in Southeast Iran in order to study groundwater conditions such as depth, thickness and aquifer boundaries.
 Vertical electrical soundings by Schlumberger array were conducted in this area. The resistivity Schlumberger
 soundings which have a maximum current electrode spacing (AB) ranging from 200 m to 600 m were
 carried out at 207 positions in 19 profiles. Interpretation of these soundings indicates the presence of an alluvial
 aquifer. This aquifer is divided into eastern and western parts by the Shooro River, which comprises a variable
 thickness and resistivity of deposits. The average permeability coefficient and resistivity in the western part, especially
 southwest is higher than the eastern part of the aquifer. Therefore, it seems that Shooro River follows a
 fault zone in the region. The high resistivity of west part is due to the water quality and the existence of alluvial
 fan with coarse grain materials. Low aquifer resistivities in the east are associated with finer materials and also
 brackish water infiltration from the adjacent basin mainly in the central part of the aquifer. Furthermore, zones
 with high yield potential have been determined in this research based on the resistivity data.
topic electrical resistivity
sounding
roundwater condition
Shooro
Iran
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3244
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AT grlashkaripour geoelectricalinvestigationfortheassessmentofgroundwaterconditionsacasestudy
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