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Author Kisi, O.; Azamathulla, H.M.; Cevat, F.; Kulls, C.; Kuhdaragh, M.; Fuladipanah, M. openurl 
  Title Enhancing river flow predictions: Comparative analysis of machine learning approaches in modeling stage-discharge relationship Type Journal Article
  Year 2024 Publication Results in Engineering Abbreviated Journal  
  Volume (down) 22 Issue Pages 102017  
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  Corporate Author Thesis  
  Publisher Elsevier Place of Publication Editor  
  Language Summary Language Original Title  
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  Notes Approved no  
  Call Number THL @ christoph.kuells @ kisi2024enhancing Serial 217  
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Author Pacheco, F.A.L.; Szocs, T. doi  openurl
  Title “Dedolomitization reactions” driven by anthropogenic activity on loessy sediments, SW Hungary Type Journal Article
  Year 2006 Publication Applied Geochemistry Abbreviated Journal  
  Volume (down) 21 Issue 4 Pages 614-631  
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  Abstract In the Szigetvár area, SW Hungary, shallow groundwaters draining upper Pleistocene loess and Holocene sediments are considerably contaminated by domestic effluents and leachates of farmland fertilizers. The loess contains calcite and dolomite, but gypsum was not recognized in these sediments. The anthropogenic inputs contain significant amounts of Ca and SO4. The Ca from these anthropogenic inputs is promoting calcite growth, with concomitant consumption of carbonate alkalinity, undersaturation of the system with respect to dolomite, and dolomite dissolution; in brief, is driving “dedolomitization reactions”. Geochemical arguments supporting the occurrence of “dedolomitization reactions” in the area are provided by the results of mass balance and thermodynamic analyses. The mass balances predicted the weather sequence dolomite\textgreatercalcite\textgreaterplagioclase\textgreaterK-feldspar, at odds with widely accepted sequences of weatherability where calcite is the first mineral in the weathering sequence. The exchange between calcite and dolomite can be a side effect of “dedolomitization reactions” because they cause precipitation of calcite. The thermodynamic prerequisites for “dedolomitization reactions” are satisfied by most local groundwaters (70%) since they are supersaturated (or in equilibrium) with respect to calcite, undersaturated (or in equilibrium) with respect to dolomite, and undersaturated with respect to gypsum. The Ca vs. SO4 and Mg vs. SO4 trends are also compatible with homologous trends resulting from “dedolomitization reactions”.  
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  ISSN 0883-2927 ISBN Medium  
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  Notes Approved no  
  Call Number THL @ christoph.kuells @ Pacheco2006 Serial 35  
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Author Egbi*, C.D.; Anornu, G.; Appiah‑Adjei, E.K.; Ganyaglo, S.Y.; Dampare, S.B. doi  openurl
  Title Evaluation of water quality using hydrochemistry, stable isotopes, and water quality indices in the Lower Volta River Basin of Ghana Type Journal Article
  Year 2019 Publication Environ. Dev. Sustain. Abbreviated Journal  
  Volume (down) 21 Issue Pages 3033-3063  
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  Notes Approved no  
  Call Number CUT @ phaedon.kyriakidis @ Egbi2018 Serial 124  
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Author Jesús Carrera, Juan J. Hidalgo, Luit J. Slooten, Enric Vázquez-Suñé url  doi
openurl 
  Title Computational and conceptual issues in the calibration of seawater intrusion models Type Journal Article
  Year 2010 Publication Hydrogeology Journal Abbreviated Journal  
  Volume (down) 18 Issue Pages 131-145  
  Keywords Coastal aquifers; Inverse modelling; Numerical modeling  
  Abstract The inverse problem of seawater intrusion(SWI) is reviewed. It represents a challenge because of both conceptual and computational difficulties and because coastal aquifer models display many singularities:(1) head measurements need to be complemented with density information; (2) salinity concentration data are

very sensitive to flow within the borehole. Data problems can be reduced by incorporating the measurement process within model calibration; (3) SWI models are extremely sensitive to aquifer bottom topography; (4) the initial conditions may be far from steady state and depend on the location and type of sea-aquifer connection. Problems with aquifer geometry and initial conditions can be addressed by parameterization, which allows for modification during inversion. The four sets of difficulties can be partly overcome by using tidal response and electrical conductivity data, which are highly informative and

provide extensive coverage. Still, SWI inversion is extremely demanding from a computation point of view. Computational improvements are discussed.
 
  Address J. Carrera : J. J. Hidalgo ()) : L. J. Slooten : E. Vázquez-Suñé, Spain e-mail: juan.hidalgo@upc.edu  
  Corporate Author Institute of Environmental Ass Institute of Environmental Assessment and Water Research (IDAEA), Spanish National Research Council (CSIC), Jordi Girona 18, 08034 Barcelona, e-mail: juan.hidalgo@upc.edu Thesis  
  Publisher IAH Place of Publication Editor Springer  
  Language English Summary Language Original Title  
  Series Editor Series Title Abbreviated Series Title  
  Series Volume Series Issue Edition  
  ISSN 1431- 2174 (online: 1435-0157) ISBN Medium  
  Area 'Hydrogeology'; 'groundwater modelling' Expedition Conference  
  Notes Approved yes  
  Call Number MGRE @ redha.menani @ Serial 51  
Permanent link to this record
 

 
Author Nas, B. openurl 
  Title Geostatistical approach to assessment of spatial distribution of groundwater quality Type Journal Article
  Year 2009 Publication Polish J. of Environ. Stud. Abbreviated Journal  
  Volume (down) 18 Issue 6 Pages 1073-1082  
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  Notes Approved no  
  Call Number CUT @ phaedon.kyriakidis @ nas2009 Serial 109  
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