2012
DOI: 10.1016/j.jhydrol.2012.06.044
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Towards a better estimate of storage properties of aquifer with magnetic resonance sounding

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Cited by 34 publications
(53 citation statements)
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“…Pumping durations lasted between 72 and 120 h and pumping yields ranged between 1.3 and 9.4 m 3 /h. Pumping tests were interpreted by Vouillamoz et al (2012a) using analytical solutions and drawdown log-derivative analysis (Renard et al 2009) implemented in AQTESOLV/Pro v4.5 software.…”
Section: Estimation and Supplementation Of Aquifer Productivity And Smentioning
confidence: 99%
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“…Pumping durations lasted between 72 and 120 h and pumping yields ranged between 1.3 and 9.4 m 3 /h. Pumping tests were interpreted by Vouillamoz et al (2012a) using analytical solutions and drawdown log-derivative analysis (Renard et al 2009) implemented in AQTESOLV/Pro v4.5 software.…”
Section: Estimation and Supplementation Of Aquifer Productivity And Smentioning
confidence: 99%
“…water-table mapping, drilling boreholes, setting up pumping tests, monitoring groundwater levels and rainfall, analysis of water isotopes-together with the geophysical magnetic resonance sounding (MRS) method. Based on new developments in the application of MRS for assessing aquifer specific yield (Vouillamoz et al 2012a(Vouillamoz et al , 2014a, a sizable MRS survey has been conducted for quantifying aquifer storage and recharge. From the unrivalled data set obtained, the groundwater resource of shallow sandstones that are targeted by local drillers has been estimated for the first time in the Oddar Meanchey province.…”
Section: Introductionmentioning
confidence: 99%
“…The relationship between MRS parameters and groundwater storage parameters is still not well established (Vouillamoz et al, 2012b). The computing of extractable groundwater storage in unconfined aquifers requires the specific yield (S y ) while in confined aquifers the elastic storativity (S e ).…”
Section: Magnetic Resonance Sounding Methodsmentioning
confidence: 99%
“…The MRS survey provides θ MRS , which is an estimate of the free water content (θ f ) that is composed of both extractable, gravitational water and immobile, non-extractable capillary water (Lubczynski and Roy, 2007). Thus neither S y nor S e are equivalent to θ MRS although there are empirical relations between them Roy, 2004, 2007;Vouillamoz et al, 2007;Boucher et al, 2009b;Vouillamoz et al, 2012b). In this study, to calculate unconfined and confined storage parameters we used the empirical Equations (4.6) and (4.7) respectively (Vouillamoz et al, 2007):…”
Section: Magnetic Resonance Sounding Methodsmentioning
confidence: 99%
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