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Gaye, C.B. |
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Title |
Isotope techniques for monitoring groundwater salinization |
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Journal Article |
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2001 |
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Hydrogeology Journal |
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9 |
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217-218 |
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THL @ christoph.kuells @ article |
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83 |
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Ghabayen, S.; McKee, M.; Kemblowski, M. |
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Title |
Ionic and Isotopic Ratios for Identification of Salinity Sources and Missing Data in the Gaza Aquifer |
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Journal Article |
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2006 |
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Journal of Hydrology |
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318 |
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360-373 |
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THL @ christoph.kuells @ article |
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87 |
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Glavas, S.; Moschonas, N. |
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Title |
Origin of observed acidic–alkaline rains in a wet-only precipitation study in a Mediterranean coastal site, Patras, Greece |
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Journal Article |
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2002 |
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Atmospheric Environment |
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36 |
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19 |
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3089-3099 |
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Elsevier |
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THL @ luqianxue.zhang @ glavas2002origin |
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91 |
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Author |
Goovaerts*, P. |
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Title |
Geostatistics for natural resources evaluation |
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1997 |
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Oxford University Press |
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Applied geostatistics series |
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9780195115383 |
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CUT @ phaedon.kyriakidis @ Goovaerts1997 |
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168 |
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Gopinath, S.; Srinivasamoorthy, K.; Saravanan, K.; Prakash, R. |
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Title |
Tracing groundwater salinization using geochemical and isotopic signature in Southeastern coastal Tamilnadu, India |
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Journal Article |
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Year |
2019 |
Publication |
Chemosphere |
Abbreviated Journal |
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236 |
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124305 |
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Coastal groundwater, Hydrochemistry, Isotopes, Thermodynamics, Statistical analysis |
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Abstract |
Attempt has been made to discriminate groundwater salinity causes along the east coast of India. A total of 122 groundwater samples (61/season) were collected for two diverse seasons (Pre Monsoon and Post Monsoon) and analyzed for physical and chemical components along with stable isotopes. The Piper diagram proposes samples along the coast predisposed by saltwater incursion. Ionic ratio plots recommend groundwater discriminatory by changing geochemical signatures. The statistical correlation suggests impact of saltwater incursion, anthropogenic and rock water interaction as sources for dissolved constituents in groundwater. The thermodynamic stability plot suggests higher silicate dissolution, weathering and ion exchange prompting water chemistry nevertheless of seasons. The δ 18O and δ 2H increases towards the sea suggesting enrichment attributed to the sea water influence and rainfall influences along the southwestern parts of the study area. |
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0045-6535 |
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THL @ christoph.kuells @ Gopinath2019124305 |
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176 |
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