2014
DOI: 10.14419/ijag.v2i2.2213
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Mapping of groundwater quality using GIS technique in the east coast of Tamilnadu state and Pondicherry union territory, India

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Cited by 5 publications
(3 citation statements)
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References 15 publications
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“…CO 2 penetrates through earth and rocks and dissolves CO 3 2− to produce HCO 3 − ions (Flood, ; Balathandayutham et al, ). The presence of Ca 2+ in the water, which is dissolved from earth and rocks leading to the hardness of water, originates from geological units, and agricultural and industrial waste (Deshpande and Aher, ; Kumaravel et al, ). Aside from TDS and TH, the most dominant ion in the research area in the wet and dry seasons is SO 4 2− , and the one with the lowest concentration is K + .…”
Section: Resultsmentioning
confidence: 99%
“…CO 2 penetrates through earth and rocks and dissolves CO 3 2− to produce HCO 3 − ions (Flood, ; Balathandayutham et al, ). The presence of Ca 2+ in the water, which is dissolved from earth and rocks leading to the hardness of water, originates from geological units, and agricultural and industrial waste (Deshpande and Aher, ; Kumaravel et al, ). Aside from TDS and TH, the most dominant ion in the research area in the wet and dry seasons is SO 4 2− , and the one with the lowest concentration is K + .…”
Section: Resultsmentioning
confidence: 99%
“…Similarly, the majority of samples (86%) from all aquifers in the Nawab Shah district, the plot fell into the rock dominance zone, while (14%) of the samples fell into the evaporation dominance zones (see Supplementary Figures S1C,D), indicating that rock-forming weathered minerals and infiltration of precipitation were the primary factors that influenced groundwater chemistry (Kumaravel et al, 2014). Some groundwater samples from the Nawab Shah fall in the evaporation dominance zone, demonstrating the impact of surface river water on the groundwater system, which could be possibly trapped during the sedimentation process (Mani et al, 2008), as well as the importance of evaporation in the depth zone of shallow groundwater.…”
Section: Factors Controlling the Groundwater Chemistry In The Ghotki ...mentioning
confidence: 92%
“…As compared to the analytical results with BIS (2012), ~ 14% of groundwater samples are located above the threshold limit. The main sources of Ca 2+ in drinking water come from geological units, agricultural wastes, and industrial wastes (Kumaravel et al 2014). Moreover, magnesium (Mg 2+ ) is another important contributor to water hardness and its contribution remarkably influences the chemistry of groundwater (Ahada and Suthar 2018).…”
Section: Spatial Variation Of Groundwater Parametersmentioning
confidence: 99%