2018
DOI: 10.1007/s10661-018-7021-8
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Hydrochemistry and groundwater quality in a semiarid calcareous area: an evaluation of major ion chemistry using a stoichiometric approach

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Cited by 25 publications
(6 citation statements)
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“…This varied distribution of HCO 3 and Clin groundwater of the study area might be due to the dissolution of minerals from the sedimentary rocks and the weathering of calcite in the parental mineral rock most commonly found in local geology [53]. The results of the current study for HCO 3 and Clare in line with other similar studies conducted in other parts of the country [54].…”
Section: Discussionsupporting
confidence: 86%
“…This varied distribution of HCO 3 and Clin groundwater of the study area might be due to the dissolution of minerals from the sedimentary rocks and the weathering of calcite in the parental mineral rock most commonly found in local geology [53]. The results of the current study for HCO 3 and Clare in line with other similar studies conducted in other parts of the country [54].…”
Section: Discussionsupporting
confidence: 86%
“…Both Ca and Mg are important micronutrients which are essential for the human body and mainly originate from dissolution of CO 3 minerals and dolomitic rocks, respectively. Na and K generally originate from dissolution of clay minerals and evaporates and silicates (Avci et al 2018 ). The order of abundance of LM is Ca > Mg > Na > K, which is in accordance with the study conducted by Sánchez et al ( 2017 ) in water–rock interactions in the urban area of Puebla Valley aquifer (Mexico).…”
Section: Resultsmentioning
confidence: 99%
“…Water is the most limited and countable resource, and only a small fraction (2.5%) of surface water is fresh and suitable for various purposes (household activities, agriculture practices, aquatic biochemical processes, and industrial maneuver) to humans and other living beings (Avci et al 2018 ; Xiao et al 2019 ). The investigation of water quality and its resources is essential for understanding the current state of water and the main threats that have occurred over the past decades.…”
Section: Introductionmentioning
confidence: 99%
“…This cumulation results in the precipitation of some less soluble minerals, and these precipitates eventually invade the saturated zone, increasing groundwater salinity. In general, the groundwater body and geology were found to be the main drivers of the hydrochemical characteristics of shallow groundwater in the study area [6,46,47].…”
Section: Hydrogeochemical Faciesmentioning
confidence: 93%