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Author Hooshmand, A.; Delghandi, M.; Izadi, A.; Aali, K.A. doi  openurl
  Title Application of kriging and cokriging in spatial estimation of groundwater quality parameters Type Journal Article
  Year 2011 Publication Afr. J. Agric. Res. Abbreviated Journal  
  Volume (up) 6 (14) Issue Pages 3402-3408  
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  ISSN 1991-637x ISBN Medium  
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  Call Number CUT @ phaedon.kyriakidis @ Hooshmand2011 Serial 133  
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Author Oehler, T.; Tamborski, J.; Rahman, S.; Moosdorf, N.; Ahrens, J.; Mori, C.; Neuholz, R.Ã.©; Schnetger, B.; Beck, M. url  doi
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  Title DSi as a Tracer for Submarine Groundwater Discharge Type Journal Article
  Year 2019 Publication Frontiers in Marine Science Abbreviated Journal  
  Volume (up) 6 Issue Pages 563  
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  Abstract Submarine groundwater discharge (SGD) is an important source of nutrients and metals to the coastal ocean, affects coastal ecosystems, and is gaining recognition as a relevant water resource. SGD is usually quantified using geochemical tracers such as radon or radium. However, a few studies have also used dissolved silicon (DSi) as a tracer for SGD, as DSi is usually enriched in groundwater when compared to surface waters. In this study, we discuss the potential of DSi as a tracer in SGD studies based on a literature review and two case studies from contrasting environments. In the first case study, DSi is used to calculate SGD fluxes in a tropical volcanic-carbonate karstic region (southern Java, Indonesia), where SGD is dominated by terrestrial groundwater discharge. The second case study discusses DSi as a tracer for marine SGD (i.e., recirculated seawater) in the tidal flat area of Spiekeroog (southern North Sea), where SGD is dominantly driven by tidal pumping through beach sands. Our results indicate that DSi is a useful tracer for SGD in various lithologies (e.g., karstic, volcanic, complex) to quantify terrestrial and marine SGD fluxes. DSi can also be used to trace groundwater transport processes in the sediment and the coastal aquifer. Care has to be taken that all sources and sinks of DSi are known and can be quantified or neglected. One major limitation is that DSi is used by siliceous phytoplankton and therefore limits its applicability to times of the year when primary production of siliceous phytoplankton is low. In general, DSi is a powerful tracer for SGD in many environments. We recommend that DSi should be used to complement other conventionally used tracers, such as radon or radium, to help account for their own shortcomings.  
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  Call Number THL @ christoph.kuells @ Oehler2019 Serial 192  
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Author Al-Omran, A.M.; Aly, A.A.; Al-Wabel, M.I.; Al-Shayaa, M.S.; Sallam, A.S.; Nadeem, M.E. doi  openurl
  Title Geostatistical methods in evaluating spatial variability of groundwater quality in Al-Kharj Region, Saudi Arabia Type Journal Article
  Year 2017 Publication Appl. Water Sci. Abbreviated Journal  
  Volume (up) 7 Issue Pages 4013-4023  
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  Call Number CUT @ phaedon.kyriakidis @ Al-Omran2017 Serial 118  
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Author Esfahani, H.K.; Datta, B. doi  openurl
  Title Simulation of reactive geochemical transportprocesses in contaminated aquifers using surrogate models Type Journal Article
  Year 2015 Publication Int. J. of GEOMATE Abbreviated Journal  
  Volume (up) 8 Issue 1 Pages 1190-1196  
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  Call Number CUT @ phaedon.kyriakidis @ esfahani2015 Serial 113  
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Author Ajmera, T.K.; Rastogi, A.K. openurl 
  Title Artificial Neural Network Application on Estimation of Aquifer Transmissivity Type Journal Article
  Year 2008 Publication Journal of Spatial Hydrology Abbreviated Journal  
  Volume (up) 8 Issue 2 Pages 15-31  
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  Call Number CUT @ phaedon.kyriakidis @ ajmera2008 Serial 115  
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