2022
DOI: 10.3390/app12052271
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Integrated Geophysical Methods for Shallow Aquifers Characterization and Modelling

Abstract: Aquifers stock about 31 [...]

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Cited by 4 publications
(2 citation statements)
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“…GPR for hydrogeological studies has mainly embraced the definition of near-surface aquifer geometries and stratigraphic information [177][178][179][180][181], as well as the determination of the water table depth and volumetric water content [182][183][184][185]. While the determination of the subsurface geometry is a well-established procedure and can be quantitatively extracted from traditional radargrams, the estimation of soil dielectric properties is performed through the solution of specific petrophysical relationships, which link the measured permittivity properties to the material porosity and moisture content.…”
Section: Gpr Applications In Environmental Investigationsmentioning
confidence: 99%
“…GPR for hydrogeological studies has mainly embraced the definition of near-surface aquifer geometries and stratigraphic information [177][178][179][180][181], as well as the determination of the water table depth and volumetric water content [182][183][184][185]. While the determination of the subsurface geometry is a well-established procedure and can be quantitatively extracted from traditional radargrams, the estimation of soil dielectric properties is performed through the solution of specific petrophysical relationships, which link the measured permittivity properties to the material porosity and moisture content.…”
Section: Gpr Applications In Environmental Investigationsmentioning
confidence: 99%
“…The electrical resistivity tomography (ERT) method is a geophysical technique with many applications, including marine [11], geotechnical, environmental [12], and composition of the soil, including building foundation prospecting, archaeological prospecting [13], landfill delineation [14], contamination [15], and chemical tracer studies [16,17]. This technique is based on measuring the electrical resistivity of soil [18], which is dependent on the geometry, pore size, and total porosity of the soil [19].…”
Section: Introductionmentioning
confidence: 99%