2020
DOI: 10.1007/s13146-020-00602-8
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Hydrogeochemical characteristics of karst groundwater in Jinci spring area, north China

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Cited by 7 publications
(3 citation statements)
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“…This reflects the contribution of these components to the groundwater salinity. A strong positive correlation between Ca 2+ and SO4 Gibbs diagrams are the primary means of illustrating water-rock interactions in groundwater [33,34]. In general, the relative relationship between Na + /(Na + + Ca 2+ ), Cl − /(Cl − + HCO 3 − ), and TDS can reveal the dominant factors in the evolution of groundwater chemistry, i.e., atmospheric precipitation, rock weathering, and evaporative crystallization [35].…”
Section: Correlation Analysismentioning
confidence: 99%
“…This reflects the contribution of these components to the groundwater salinity. A strong positive correlation between Ca 2+ and SO4 Gibbs diagrams are the primary means of illustrating water-rock interactions in groundwater [33,34]. In general, the relative relationship between Na + /(Na + + Ca 2+ ), Cl − /(Cl − + HCO 3 − ), and TDS can reveal the dominant factors in the evolution of groundwater chemistry, i.e., atmospheric precipitation, rock weathering, and evaporative crystallization [35].…”
Section: Correlation Analysismentioning
confidence: 99%
“…Currently, there is limited research on groundwater in the western karst region. The vulnerability of karst water to contamination is determined by the fragile karst environment in the northern and southern karst regions, the multiple recharge of karst water, the openness of the system, and the fragility of the karst environment [4]. The high permeability of the aquifers and the poor antifouling performance of the karst groundwater systems are key factors that make them susceptible to contamination [5,6].…”
Section: Introductionmentioning
confidence: 99%
“…This research will contribute to a deeper understanding of the migration patterns of elements in the entire karst environment and their correlation with karst ecology. 4.…”
mentioning
confidence: 99%