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Author (down) Zhou*, H.; Gómez-Hernández, J.J.; Li, L. doi  openurl
  Title Inverse methods in hydrogeology: Evolution and recent trends Type Journal Article
  Year 2014 Publication Adv. Water Resour. Abbreviated Journal  
  Volume 63 Issue Pages 22-37  
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  Publisher Elsevier BV Place of Publication Editor  
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  Call Number CUT @ phaedon.kyriakidis @ Zhou2014 Serial 170  
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Author (down) Zhaoyong*, Z.; Abuduwaili, J.; Yimit, H. doi  openurl
  Title The occurrence, sources and spatial characteristics of soil salt and assessment of soil salinization risk in Yanqi Basin, Northwest China Type Journal Article
  Year 2014 Publication PLoS ONE Abbreviated Journal  
  Volume 9(9) Issue Pages 106079  
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  Notes Approved no  
  Call Number CUT @ phaedon.kyriakidis @ Zhaoyong2014 Serial 121  
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Author (down) Zhao, Q.; Su, X.; Kang, B.; Zhang, Y.; Wu, X.; Liu, M. url  doi
openurl 
  Title A hydrogeochemistry and multi-isotope (Sr, O, H, and C) study of groundwater salinity origin and hydrogeochemcial processes in the shallow confined aquifer of northern Yangtze River downstream coastal plain, China Type Journal Article
  Year 2017 Publication Applied Geochemistry Abbreviated Journal  
  Volume 86 Issue Pages 49-58  
  Keywords Coastal confined groundwater, Salinity, Hydrogeochemcial processes, Multiple environmental tracers  
  Abstract Economically developed coastal areas have a high water demand, and their groundwater resources can be threatened by salinization. Many methods and tracers have been used to discriminate the source of salinization because a single method does not yield reliable results. In this paper, the shallow confined coastal plain aquifer, north of the downstream Yangtze River in China, is used as a case study to investigate the origin of the salinity and the relevant geochemical processes for this aquifer. Multiple environmental tracers of major ions, minor ions (Br−, I−), and isotopes (18O, 2H, 13C, 87Sr, 3H, 14C) were used so as to provide reliable conclusions. The TDS distribution of the aquifer has an increasing trend, from below 500 mg/L in the inland areas to more than 20,000 mg/L around the southeast coastline. The water chemical type evolves from HCO3-Ca to Cl-Na as the TDS increases. The results suggest that the groundwater salinity is influenced by seawater intrusion. The seawater proportions in the groundwater samples range from 0.07% to 94.41% and show the same spatial distribution pattern as TDS. The 3H and 14C values show that the highest salinity was mainly caused by a seawater transgression around 6000a B.P. The aquifer is also affected by other hydrogeochemical processes: base exchange has enriched Ca2+ and depleted K+ and Na+, sulfate reduction has reduced the concentration of SO42− and enriched HCO3−, and iodine-rich organic matter decomposition has enriched the concentration of I−. The iodine enrichment also suggests paleo-seawater intrusion. In addition, the precipitation of carbonate minerals has decreased the concentration of Ca2+, Mg2+, and HCO3−, albeit to a limited extent.  
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  ISSN 0883-2927 ISBN Medium  
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  Call Number THL @ christoph.kuells @ Zhao201749 Serial 182  
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Author (down) Zhao, Q.; Su, X.; Gan, Y. url  doi
openurl 
  Title Hydrogeochemical and isotopic study of the origins of groundwater salinization in the deep confined aquifer of northern Yangtze River Type Journal Article
  Year 2019 Publication E3S Web Conf. Abbreviated Journal  
  Volume 98 Issue Pages 07034  
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  Call Number THL @ christoph.kuells @ Zhao2019 Serial 180  
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Author (down) Zghibi, A.; Zouhri, L.; Tarhouni, J.; Kouzana, L. url  openurl
  Title Groundwater mineralisation processes in Mediterranean semi-arid systems (Cap-Bon, North east of Tunisia): hydrogeological and geochemical approaches Type Journal Article
  Year 2013 Publication Hydrological Processes Abbreviated Journal  
  Volume 27 Issue 22 Pages 3227-3239  
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  Publisher Wiley Online Library Place of Publication Editor  
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  Call Number THL @ luqianxue.zhang @ zghibi2013groundwater Serial 73  
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