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Author Narany, T.S.; Ramli, M.F.; Aris, A.Z.; Sulaiman, W.N.A.; Juahir, H.; Fakharian, K. doi  openurl
  Title Identification of the hydrogeochemical processes in groundwater using classic integrated geochemical methods and geostatistical techniques, in Amol-Babol plain, Iran Type Journal Article
  Year 2014 Publication Sci. World J. Abbreviated Journal  
  Volume (down) 419058, Issue Pages 15  
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  Call Number CUT @ phaedon.kyriakidis @ narany2014 Serial 117  
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Author Mahindawansha, A.; Külls, C.; Kraft, P.; Breuer, L. url  doi
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  Title Estimating water flux and evaporation losses using stable isotopes of soil water from irrigated agricultural crops in tropical humid regions Type Journal Article
  Year 2019 Publication Hydrology and Earth System Sciences Discussions Abbreviated Journal  
  Volume (down) 2019 Issue Pages 1-28  
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  Call Number THL @ christoph.kuells @ hess-2019-213 Serial 105  
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Author Hammami Abidi, J.; Farhat, B.; Ben Mammou, A.; Oueslati, N. url  doi
openurl 
  Title Characterization of Recharge Mechanisms and Sources of Groundwater Salinization in Ras Jbel Coastal Aquifer (Northeast Tunisia) Using Hydrogeochemical Tools, Environmental Isotopes, GIS, and Statistics Type Journal Article
  Year 2017 Publication Journal of Chemistry Abbreviated Journal  
  Volume (down) 2017 Issue Pages 8610894  
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  Abstract Groundwater is among the most available water resources in Tunisia; it is a vital natural resource in arid and semiarid regions. Located in north-eastern Tunisia, the Metline-Ras Jbel-Raf Raf aquifer is a mio-plio-quaternary shallow coastal aquifer, where groundwater is the most important source of water supply. The major ion hydrochemistry and environmental isotope composition δ18O, δ2H were investigated to identify the recharge sources and processes that affect the groundwater salinization. The combination of hydrogeochemical, isotopic, statistical, and GIS approaches demonstrates that the salinity and the groundwater composition are largely controlled by the water-rock interaction particularly the dissolution of evaporate minerals and the ion exchange process, the return flow of the irrigation water, agricultural fertilizers, and finally saltwater intrusion which started before 1980 and which is partially mitigated by the artificial recharge since 1993. As for the stable isotope signatures, results showed that groundwater samples lay on and around the local meteoric water line LMWL; hence, this arrangement signifies that the recharge of the Ras Jbel aquifer is ensured by recent recharge from Mediterranean air masses.  
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  Publisher Hindawi KW Place of Publication Editor  
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  ISSN 2090-9063 ISBN Medium  
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  Notes Approved no  
  Call Number THL @ christoph.kuells @ Serial 189  
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Author Qi, H.; Ma, C.; He, Z.; Hu, X.; Gao, L. url  doi
openurl 
  Title Lithium and its isotopes as tracers of groundwater salinization: A study in the southern coastal plain of Laizhou Bay, China Type Journal Article
  Year 2019 Publication The Science of the Total Environment Abbreviated Journal Sci Total Environ  
  Volume (down) 650 Issue Pt 1 Pages 878-890  
  Keywords Brine and seawater intrusion; Groundwater salinization; Hydrochemistry; Lithium isotope; Southern coastal plain of Laizhou Bay  
  Abstract In the southern coastal plain of Laizhou Bay, due to intensive exploitation of groundwater since the early 1970s, the shallow aquifer has been severely influenced by saltwater intrusion, which causes the extraction to shift from shallow to deeper aquifer changing the hydrogeological condition greatly. This study was conducted to investigate the groundwater salinization using hydrochemistry and H, O and Li isotope data. Dissolved Li shows a linear correlation with Cl and Br in seawater, brine and saline groundwater indicating the marine Li source, whereas the enrichment of Li in surface water, brackish and fresh groundwater is impacted by dissolution of silicate minerals. The analyses of hydrochemistry and isotopes (H, O and Li) indicate that brine originated from seawater evaporation, followed by mixing processes and some water-rock interactions; shallow saline groundwater originated from brine diluted with seawater and fresh groundwater; deep saline groundwater originated from seawater intrusion. The negative correlation of δ(7)Li and Li/Na in surface water, brackish and fresh groundwater is contrary to the general conclusion, indicating the slow weathering of silicate minerals and hydraulic interaction between surface water and shallow groundwater in this area. The analyses of hydrochemistry and isotopes (Li, H and O) can well identify the salinity sources and isotope fractionation in groundwater flow and mixing, especially groundwater with high TDS. As both mixing with saltwater and isotope fractionation can explain the combination of high δ(7)Li and low TDS in brackish groundwater, isotope fractionation may limit their use in recognizing salinity sources of groundwater with low TDS.  
  Address School of Environmental Studies, China University of Geosciences, Wuhan 430074, China  
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  ISSN 0048-9697 ISBN Medium  
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  Notes PMID:30308862 Approved no  
  Call Number THL @ christoph.kuells @ Serial 184  
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Author Kreynsa*, P.; Genga, X.; Michaela, H.A. doi  openurl
  Title The influence of connected heterogeneity on groundwater flow and salinity distributions in coastal volcanic aquifers Type Journal Article
  Year 2020 Publication J.Hydrol. Abbreviated Journal  
  Volume (down) 586 Issue Pages 124863  
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  Call Number CUT @ phaedon.kyriakidis @ Kreynsa2020 Serial 138  
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