1983
DOI: 10.1016/0009-2541(83)90033-5
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Geochemistry of saline minerals separated from Lake Qarun brine

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Cited by 12 publications
(4 citation statements)
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“…Therefore, during the movement of groundwater towards Lake Qarun, the dominant anion changes from HCO 3 -to SO 4 2-. Since gypsum is abundant in the Faiyum (Rasmy & Estefan, 1983;Aref, 2003), this increase in sulphate concentration, and the transformation from HCO 3 --Na ? brine to SO 4 2--Na ?…”
Section: Discussionmentioning
confidence: 98%
See 1 more Smart Citation
“…Therefore, during the movement of groundwater towards Lake Qarun, the dominant anion changes from HCO 3 -to SO 4 2-. Since gypsum is abundant in the Faiyum (Rasmy & Estefan, 1983;Aref, 2003), this increase in sulphate concentration, and the transformation from HCO 3 --Na ? brine to SO 4 2--Na ?…”
Section: Discussionmentioning
confidence: 98%
“…brine, may have been brought about by the action of the HCO 3 --Na ? solution on gypsum deposits in the following way (Rasmy & Estefan, 1983).…”
Section: Discussionmentioning
confidence: 99%
“…The agricultural activities in the Fayoum Depression depend mainly on Nile water. The agriculture drainage water annually carries 470 × 10 6 kg of dissolved salts to Lake Qarun [16]. Since the lake has no outlet and the climatic conditions are warm and dry almost all the year, the lake brine gradually evaporates and its salinity increases.…”
Section: Introductionmentioning
confidence: 99%
“…Nowadays, 3,822,836 people inhabit the Fayum depression (CAMPAS 2020b). Owing to the steep downward slope of Fayum land towards Lake Qaroun (Donia 2013), the lake annually receives 470*10 6 kg dissolved salts from the agricultural drainage (Rasmy and Estefan 1983). Since the lake is regarded as an endorheic lake without outlets (Williams and Mann 2014), the continuous increase of agricultural discharge and evaporation rate had raised the lake's salinity.…”
mentioning
confidence: 99%