2017
DOI: 10.1016/j.jafrearsci.2017.02.009
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Geophysical and hydrogeological investigation to study groundwater occurrences in the Taref Formation, south Mut area – Dakhla Oasis - Egypt

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Cited by 16 publications
(4 citation statements)
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“…The aquifer layer had a range of resistivity values that vary from 682 to 1347 Ωm, where the aquifer was found in the fissure and fracture of schist and sandstone rocks as revealed by Sukrisna (2004). High aquifer values are common in aged rocks such as schist and sandstone [21,39]. Apart from being a limited aquifer, schist can also act as an aquifuge layer, that is, a layer that cannot hold or drain water [28,40].…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The aquifer layer had a range of resistivity values that vary from 682 to 1347 Ωm, where the aquifer was found in the fissure and fracture of schist and sandstone rocks as revealed by Sukrisna (2004). High aquifer values are common in aged rocks such as schist and sandstone [21,39]. Apart from being a limited aquifer, schist can also act as an aquifuge layer, that is, a layer that cannot hold or drain water [28,40].…”
Section: Resultsmentioning
confidence: 99%
“…It is also widely used in research on aquifer susceptibility [20]. Vertical electrical sounding is a data collection technique widely used in geoelectrical research [21]. Schlumberger arrays are electrode configuration techniques in vertical electrical sounding that are widely used in hydrogeological investigations [22].…”
Section: Introductionmentioning
confidence: 99%
“…Electrical resistivity tomography allowed us to distinguish the distribution of electrical resistivity of the subsoil by relating the solid constituents of the soil, water tent, and temperature with respect to the electrical resistivity. This can be considered way to interpret the variability in the physical properties of the soil [10,14,15]. The res of this study are from a distance-depth stratigraphic section with a distribution of surface resistivity, which is easily understandable in geological terms, in which the e trical resistivity of the medium depends on the amount of water in the subsurface [16] determine the electrical resistivity of the structures, Equation (1) is used [17]: The methodology used was developed based on national and regional geological information [13] to determine the areas of hydrogeological interest in the Langos sector.…”
Section: Electrical Resistivity Tomography (Ert)mentioning
confidence: 99%
“…However, the complexity of studying groundwater due to the cost of traditional methods, such as drilling, means that there is a shortage of hydrogeological data in the country [8]. In this context, geophysical methods are a solution to this problem because they are widely used worldwide and provide acceptable results, which allow an understanding of the behavior of groundwater in the subsurface strata [9][10][11].…”
Section: Introductionmentioning
confidence: 99%