2022
DOI: 10.1016/j.pce.2022.103109
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Impact of anthropogenic and geological factors on groundwater hydrochemistry in the unconfined aquifers of Indo-Gangetic plain

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Cited by 20 publications
(6 citation statements)
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“…Also, pollutants that enter groundwater under the influence of waste washing help to disperse pollutants in an aquifer and after being infected, aquifer recovery is not easy. 12 One way to compensate for water shortages is to reuse contaminated water. Water pollution varies in terms of quantity and type of pollutants based on the source of water consumption.…”
Section: Introductionmentioning
confidence: 99%
“…Also, pollutants that enter groundwater under the influence of waste washing help to disperse pollutants in an aquifer and after being infected, aquifer recovery is not easy. 12 One way to compensate for water shortages is to reuse contaminated water. Water pollution varies in terms of quantity and type of pollutants based on the source of water consumption.…”
Section: Introductionmentioning
confidence: 99%
“…Calcium and magnesium are two essential minerals that can be obtained from various sources. The presence of ferromagnesium minerals in the natural surroundings, dolomite weathering and dissolution of calcite are some of the processes to acquire these essential minerals (Gautam et al, 2022;Goswami et al, 2022;Gugulothu et al, 2022). The Palaeozoic substratum of the Anti-Atlas, as well as the limestone and dolomitic rocks of the Jurassic Mountains in the High-Atlas region, are considered potential sources of calcium and magnesium minerals.…”
Section: Assessment Of Water Quality 421 Adequacy Of Water For Human ...mentioning
confidence: 99%
“…Nowadays, hydrogeochemical processes have garnered increased attention [17] due to their valuable insights into the interaction between groundwater and the environment. The groundwater's hydrochemical properties, including both anions and cations, are predominantly dictated by the surrounding area's geology and the aquifer's characteristics [18,19]. Anions such as chloride (Cl − ), sulfate (SO 4 2− ), and bicarbonate (HCO 3 − ) may derive from the dissolution of minerals rich in these ions, such as halite, gypsum, and calcite, respectively.…”
Section: Introductionmentioning
confidence: 99%