2012
DOI: 10.4028/www.scientific.net/amm.212-213.362
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Chemistry of Groundwater from Two Aquifers in Liuyi Coal Mine, Northern Anhui Province, China: a Comparative Study

Abstract: Major ion concentrations of twenty groundwater samples from two deep seated aquifers (coal bearing-GC and limestone-LC) are analyzed for identify the differences between them and the source of ions. The results suggest that they are moderate to highly mineralized water with their average TDS values are 2444 (GC) and 1178 (LC) mg/L. LCs show lower Na but much higher Ca and Mg concentrations relative to GCs. Saturation indexes and principle component analysis, as well as mole ratios between Na and Cl, Ca and SO4… Show more

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Cited by 2 publications
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“…However, in some places of China, the excessive occurrence of dissolved solids in the groundwater, primarily due to geological causes, though not classified as brackish, restricts its usage for drinking water production. A notable example is the relatively high concentrations of sodium, fluoride and sulfate in the groundwater of the Huaibei Plain [2,3]. The maximum allowable concentrations for sodium, fluoride and sulfate are 200, 1 and 250 mg•L -1 , respectively, according to the Chinese Standards for Drinking Water Quality [4].…”
Section: Introductionmentioning
confidence: 99%
“…However, in some places of China, the excessive occurrence of dissolved solids in the groundwater, primarily due to geological causes, though not classified as brackish, restricts its usage for drinking water production. A notable example is the relatively high concentrations of sodium, fluoride and sulfate in the groundwater of the Huaibei Plain [2,3]. The maximum allowable concentrations for sodium, fluoride and sulfate are 200, 1 and 250 mg•L -1 , respectively, according to the Chinese Standards for Drinking Water Quality [4].…”
Section: Introductionmentioning
confidence: 99%