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Author Carrera*, J.; Hidalgo, J.J.; Slooten, L.J.; Vázquez-Suñé, E. doi  openurl
  Title (up) Computational and conceptual issues in the calibration of seawater intrusion models Type Journal Article
  Year 2010 Publication Hydrogeol. J. Abbreviated Journal  
  Volume 18 Issue Pages 131-145  
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  Call Number CUT @ phaedon.kyriakidis @ Carrera2010 Serial 147  
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Author Mihajlidi-Zelić, A.; Deršek-Timotić, I.; Relić, D.; Popović, A.; Đorđević, D. url  openurl
  Title (up) Contribution of marine and continental aerosols to the content of major ions in the precipitation of the central Mediterranean Type Journal Article
  Year 2006 Publication Science of the total environment Abbreviated Journal  
  Volume 370 Issue 2-3 Pages 441-451  
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  Publisher Elsevier Place of Publication Editor  
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  Series Volume Series Issue Edition  
  ISSN 0048-9697 ISBN Medium  
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  Notes Approved no  
  Call Number THL @ luqianxue.zhang @ Mihajlidi-Zelić2006 Serial 60  
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Author Liu, F.; Wang, S.; Wang, L.; Shi, L.; Song, X.; Yeh, T.-C.J.; Zhen, P. doi  openurl
  Title (up) Coupling hydrochemistry and stable isotopes to identify the major factors affecting groundwater geochemical evolution in the Heilongdong Spring Basin, North China Type Journal Article
  Year 2019 Publication Journal of Geochemical Exploration Abbreviated Journal  
  Volume 205 Issue Pages  
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  Abstract Understanding the interference of natural processes and anthropogenic activities in geochemical evolution of groundwater is vital for groundwater sustainable management in water-stressed regions. This study is devoted to the identification of the main factors controlling the evolution of groundwater chemistry by the combined use of hydrogeochemical indicators along with isotope tracers in the Heilongdong Spring Basin, North China. Thirty-nine groundwater samples and twelve surface water samples were collected, and major ions and stable isotopes were measured during the two campaigns (December 2017 and August 2018). The isotope approach indicates that the groundwater is recharged by precipitation infiltration after evaporation, and interacts with surface water along preferential flow paths in fault zones and karst conduits. Currently, the main chemical facies of groundwater evolve from Ca-HCO3 and Ca-Mg-HCO3 types with low TDS, through Ca-Mg-HCO3-SO4 and Ca-HCO3-SO4 types with moderate TDS, to Ca-SO4, Ca-SO4-Cl and CaCl types with high TDS. Apart from natural processes (involving dissolution/precipitation of minerals, cation exchange, and evaporation) regulating the groundwater quality, the stagnant zones also play a crucial role in the formation of severe localized nitrate contamination. The deterioration in groundwater quality can be attributed to anthropogenic factors (including the change in groundwater exploitation, the leaching of solid waste, and the overuse of agricultural fertilizers). The high loads of agricultural fertilizers in irrigation return flows are likely to be the main contributor of the dissolved nitrate in groundwater. The findings of this work not only have important implications for groundwater sustainable utilization, but also could serve as a template for other rapidly industrialized and water-stressed regions.  
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  ISSN 0375-6742 ISBN Medium  
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  Call Number THL @ christoph.kuells @ Liu2019 Serial 29  
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Author Hanshaw, B.B.; Back, W. url  doi
openurl 
  Title (up) Deciphering hydrological systems by means of geochemical processes Type Journal Article
  Year 1985 Publication Hydrological Sciences Journal Abbreviated Journal  
  Volume 30 Issue 2 Pages 257-271  
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  Abstract The distribution of permeability and chemical character of groundwater in carbonate aquifers is significantly influenced by the many diagenetic processes

and reactions that occur in the early development of these rocks. Many of these diagenetic processes occur in the transition zone formed as the carbonate sediments emerge from the marine environment and become fresh-water aquifers. Analyses of trace elements and isotopes

indicate that calcite cements and dolomites are formed in this groundwater mixing zone. Reverse reactions such as mineral dissolution and dedolomitization occur in carbonate aquifer systems. The geochemical reactivity of the fresh-water/salt-water mixing zone results from the nonlinearity of geochemical parameters as a function of ionic strength and causes extensive dissolution in coastal carbonate rocks. Interpretation of geochemical reactions and isotopic composition of groundwater provides a method to determine hydrological parameters

such as porosity, hydraulic conductivity, and groundwater flow rates. This geochemical method is largely independent of the more conventional approach of determining these parameters by an evaluation of physical properties of aquifer systems.
 
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  ISSN 0262-6667 ISBN Medium  
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  Call Number THL @ christoph.kuells @ Hanshaw1985 Serial 25  
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Author Varouchakis, E.A.; Theodoridou, P.G.; Karatzas, G.P. doi  openurl
  Title (up) Decision-making tool for groundwater level spatial distribution and risk assessment using geostatistics in R Type Journal Article
  Year 2020 Publication J. Hazard. Toxic Radioact. Waste Abbreviated Journal  
  Volume 24 (1) Issue Pages 04019031  
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  Call Number CUT @ phaedon.kyriakidis @ varouchakis2020 Serial 106  
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