2015
DOI: 10.1007/s12665-015-4327-5
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Total vulnerability estimation for the Tabriz aquifer (Iran) by combining a new model with DRASTIC

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Cited by 21 publications
(13 citation statements)
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“…This layer was generated using DEM of the area. Impact of vadose zone is a layer located between groundwater table and unsaturated soil, which controls the passage of contaminant into the groundwater (Vaezihir and Tabarmayeh 2015). With respect to many physical and chemical reactions occurring in this zone such as mechanical filtration, volatilization, dispersion, biodegradation, and neutralization, this layer is potential for filtering the contaminants (Wu et al 2016).…”
Section: Structure Of Each Model For Evaluating Drastic Indicesmentioning
confidence: 99%
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“…This layer was generated using DEM of the area. Impact of vadose zone is a layer located between groundwater table and unsaturated soil, which controls the passage of contaminant into the groundwater (Vaezihir and Tabarmayeh 2015). With respect to many physical and chemical reactions occurring in this zone such as mechanical filtration, volatilization, dispersion, biodegradation, and neutralization, this layer is potential for filtering the contaminants (Wu et al 2016).…”
Section: Structure Of Each Model For Evaluating Drastic Indicesmentioning
confidence: 99%
“…Hydraulic conductivity controls contaminant migration and dispersion within the aquifer media and consequently, the concentration of the plume in the groundwater (Vaezihir and Tabarmayeh 2015). The hydraulic conductivity was calculated by the following equation: k = T b −1 , where k (m/d) is the hydraulic conductivity, T (m 2 /d) and b −1 (m) are transmissivity and thickness of the aquifer, respectively.…”
Section: Structure Of Each Model For Evaluating Drastic Indicesmentioning
confidence: 99%
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