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Author Edwards, P.J.; Williard, K.W.J.; Schoonover, J.E. url  openurl
  Title Fundamentals of watershed hydrology Type Journal Article
  Year 2015 Publication Journal of contemporary water research & education Abbreviated Journal  
  Volume (down) 154 Issue 1 Pages 3-20  
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  Publisher Wiley Online Library Place of Publication Editor  
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  Call Number THL @ luqianxue.zhang @ edwards2015fundamentals Serial 101  
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Author Elrashidi, M.A.; Adriano, D.C.; Workman, S.M.; Lindsay, W.L. openurl 
  Title Chemical equilibria of selenium in soils: a theoretical development1 Type Journal Article
  Year 1987 Publication Soil Science Abbreviated Journal  
  Volume (down) 144 Issue 2 Pages 141-152  
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  Publisher Lww Place of Publication Editor  
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  Call Number THL @ luqianxue.zhang @ elrashidi1987chemical Serial 103  
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Author Zhou, X.; Li, C. url  openurl
  Title Hydrogeochemistry of deep formation brines in the central Sichuan Basin, China Type Journal Article
  Year 1992 Publication Journal of Hydrology Abbreviated Journal  
  Volume (down) 138 Issue 1 Pages 1-15  
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  Abstract Subsurface brines are abundant in the Sichuan Basin, China. Five brine-bearing aquifers have been identified within rocks of Triassic age in the central part of the basin. These are of two types: brine-bearing clastic and brine-bearing carbonate aquifers. Brines in this region have high total dissolved solids and chemical species that are different from those of evaporatively concentrated seawater. Deep formation brines in clastic aquifers, in which evaporites do not exist, are characterized by high concentrations of Ca, Sr, Ba, Br and I, low concentrations of Mg and K, and lack of SO4, and are dominated by the NaCaCl type. Brines in carbonate aquifers, which have interbeds of evaporites, are characterized by high total dissolved solids, low concentrations of Ca, Mg and SO4, and lack of Ba, and are of the NaCl type. The brines in clastic aquifers originate from connate continental sedimentary waters mixed with marine waters; membrane filtration through shales has played an important part in modifying the chemical compositions and increasing the salinity of the brines. Those in carbonate aquifers are bittern marine sedimentary waters, with chemical compositions mainly controlled by precipitation of evaporites.  
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  ISSN 0022-1694 ISBN Medium  
  Area Asia Expedition Conference  
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  Call Number THL @ christoph.kuells @ Zhou19921 Serial 41  
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Author Löhnert, E.P.; Sonntag, C. openurl 
  Title Grundwasserversalzungen im Raum Hamburg im Licht neuer Isotopendaten Type Journal Article
  Year 1981 Publication Zeitschrift der Deutschen Geologischen Gesellschaft Abbreviated Journal  
  Volume (down) 132 Issue Pages 559-574  
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  Publisher Schweizerbart Science Publishers Place of Publication Stuttgart, Germany Editor  
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  Call Number THL @ christoph.kuells @ Loehhnert1981 Serial 185  
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Author Lucia, M.D.; Kempka, T.; Jatnieks, J.; Kuhn, M. doi  openurl
  Title Integrating surrogate models into subsurface simulation framework allows computation of complex reactive transport scenarios Type Journal Article
  Year 2017 Publication Energy Procedia Abbreviated Journal  
  Volume (down) 125 Issue Pages 580-587  
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  Call Number CUT @ phaedon.kyriakidis @ lucia2017 Serial 112  
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