2011
DOI: 10.1155/2011/632968
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Study on the Significance of Temporal Ion Chemistry in Groundwater of Dindigul District, Tamilnadu, India

Abstract: The demand of water supply is increasing day by day to meet the pace of developments in domestic, agricultural and industrial sectors especially in developing countries like India. Groundwater being a scarce commodity in a hard rock terrain like Dindigul district an attempt has been made in this study brings out the significance of temporal ion chemistry in groundwater by collecting groundwater from 43 different location of the district and analysed for major and minor ions. These ions were then used for the i… Show more

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Cited by 10 publications
(3 citation statements)
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“…The pH increases from 6 to 9.4 (Fig. 6) type (Manivannan et al 2010;Singaraja et al 2014). These imply that higher pCO 2 leads to higher bicarbonate concentrations in the groundwater, which in turn enhances the release of F − due to higher rock-water interactions under long residence time.…”
Section: Relationship Between Pco 2 and Hco −mentioning
confidence: 97%
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“…The pH increases from 6 to 9.4 (Fig. 6) type (Manivannan et al 2010;Singaraja et al 2014). These imply that higher pCO 2 leads to higher bicarbonate concentrations in the groundwater, which in turn enhances the release of F − due to higher rock-water interactions under long residence time.…”
Section: Relationship Between Pco 2 and Hco −mentioning
confidence: 97%
“…9). Lithologically, the highest F − and HCO contents in groundwater occur in the northern part of the Tuticorin District due to HBG and charnockites geology (Manivannan et al 2010;Manikandan et al 2014). In the northern part of the Tuticorin District, the groundwater flow paths are longer and hence will have longer residence time and higher degree of rock-water interactions.…”
Section: Relationship Between Pco 2 and Hco −mentioning
confidence: 99%
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