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Author Cary, L.; Petelet-Giraud, E.; Bertrand, G.; Kloppmann, W.; Aquilina, L.; Martins, V.; Hirata, R.; Montenegro, S.M.G.L.; Pauwels, H.; Chatton, E.; Franzen, Melissa; Aurouet, A.; Lasseur, E.; Picot-Colbeaux, G.; Guerrot, C.; Fléhoc, C.; Labasque, T.; Santos, Jeane Glaucia; Paiva, Anderson L.R.; Braibant, G.; Pierre, D. url  doi
openurl 
  Title (up) Origins and processes of groundwater salinization in the urban coastal aquifers of Recife (Pernambuco, Brazil): a multi-isotope approach Type Journal Article
  Year 2015 Publication Science of the Total Environment Abbreviated Journal  
  Volume 530-531 Issue Pages 411-429  
  Keywords Salinization origins; Salinization processes; Groundwater; Coastal aquifer; Strontium isotopes; Boron isotopes; Recife; Brazil  
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  Publisher Elsevier Place of Publication Editor  
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  Call Number THL @ christoph.kuells @ cary:hal-01161949 Serial 85  
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Author Gopinath, S.; Srinivasamoorthy, K.; Saravanan, K.; Prakash, R. url  openurl
  Title (up) Tracing groundwater salinization using geochemical and isotopic signature in Southeastern coastal Tamilnadu, India Type Journal Article
  Year 2019 Publication Chemosphere Abbreviated Journal  
  Volume 236 Issue Pages 124305  
  Keywords Coastal groundwater, Hydrochemistry, Isotopes, Thermodynamics, Statistical analysis  
  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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  Series Volume Series Issue Edition  
  ISSN 0045-6535 ISBN Medium  
  Area Expedition Conference  
  Notes Approved no  
  Call Number THL @ christoph.kuells @ Gopinath2019124305 Serial 176  
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