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Author Faye, S.; Maloszewski, P.; Stichler, W.; Trimborn, P.; Faye, S. C.; Gaye, C. url  openurl
  Title Groundwater salinization in the Saloum (Senegal) delta aquifer: minor elements and isotopic indicators Type Journal Article
  Year (up) 2005 Publication Science of The Total Environment Abbreviated Journal  
  Volume 343 Issue 1 Pages 243-259  
  Keywords Minor elements, Hydrochemistry, Sorption/desorption, Mixing model, Salinization  
  Abstract The hydrochemistry of minor elements bromide (Br), boron (B), strontium (Sr), environmental stable isotopes (18O and 2H) together with major-ion chemistry (chloride, sodium, calcium) has been used to constrain the source(s), relative age, and processes of salinization in the Continental Terminal (CT) aquifer in the Saloum (mid-west Senegal) region. Seventy-one groundwater wells which include 24 wells contaminated by saltwater and three sites along the hypersaline Saloum River were sampled to obtain additional information on the hydrochemical characteristics of the groundwater defined in previous studies. Use of Br against Cl confirms the Saloum River saline water intrusion up to a contribution of 7% into the aquifer. In addition to this recent intrusion, a relatively ancient intrusion of the Saloum River water which had reached at least as far as 20 km south from the source was evidenced. The high molar ratio values of Sr/Cl and Sr/Ca indicate an additional input of strontium presumably derived from carbonate precipitation/dissolution reactions and also via adsorption reactions. The variable B concentrations (7–650 μg/L) found in the groundwater samples were tested against the binary mixing model to evaluate the processes of salinization which are responsible for the investigated system. Sorption of B and depletion of Na occur as the Saloum river water intrudes the aquifer (salinization) in the northern part of the region, whereas B desorption and Na enrichment occur as the fresh groundwater flushing displaces the saline waters in the coastal strip (refreshening). In the central zone where ancient intrusion prevailed, the process of freshening of the saline groundwater is indicated by the changes in major-ion chemistry as well as B desorption and Na enrichment. In addition to these processes, stable isotopes reveal that mixing with recently infiltrating waters and evaporation contribute to the changes in isotopic signature.  
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  Series Volume Series Issue Edition  
  ISSN 0048-9697 ISBN Medium  
  Area Expedition Conference  
  Notes Approved no  
  Call Number THL @ christoph.kuells @ Faye2005243 Serial 173  
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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 (up) 2006 Publication Applied Geochemistry Abbreviated Journal  
  Volume 21 Issue 4 Pages 614-631  
  Keywords  
  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  
  Area Expedition Conference  
  Notes Approved no  
  Call Number THL @ christoph.kuells @ Pacheco2006 Serial 35  
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Author de Paz, J.-M.; Sánchez, J.; Visconti, F. url  openurl
  Title Combined use of GIS and environmental indicators for assessment of chemical, physical and biological soil degradation in a Spanish Mediterranean region Type Journal Article
  Year (up) 2006 Publication Journal of environmental management Abbreviated Journal  
  Volume 79 Issue 2 Pages 150-162  
  Keywords  
  Abstract Soil is one of the main non-renewable natural resources in the world. In the Valencian Community (Mediterranean coast of Spain), it is especially important because agriculture and forest biomass exploitation are two of the main economic activities in the region. More than 44% of the total area is under agriculture and 52% is forested.

The frequently arid or semi-arid climate with rainfall concentrated in few events, usually in the autumn and spring, scarcity of vegetation cover, and eroded and shallow soils in several areas lead to soil degradation processes. These processes, mainly water erosion and

salinization, can be intense in many locations within the Valencian Community.

Evaluation of soil degradation on a regional scale is important because degradation is incompatible with sustainable development. Policy makers involved in land use planning require tools to evaluate soil degradation so they can go on to develop measures aimed at protecting and

conserving soils.

In this study, a methodology to evaluate physical, chemical and biological soil degradation in a GIS-based approach was developed for the Valencian Community on a 1/200,000 scale.

The information used in this study was obtained from two different sources: (i) a soil survey with more than 850 soil profiles sampled within the Valencian Community, and (ii) the environmental information implemented in the Geo-scientific map of the Valencian Community digitised on an Arc/Info GIS. Maps of physical, chemical and biological soil degradation in the Valencian Community on a 1/200,000 scale were obtained using the methodology devised. These maps can be used to make a cost-effective evaluation of soil degradation on a regional scale.

Around 29% of the area corresponding to the Valencian Community is affected by high to very high physical soil degradation, 36% by high to very high biological degradation, and 6% by high to very high chemical degradation. It is, therefore, necessary to draw up legislation and to establish the policy framework for actions focused on preventing soil degradation and conserving its productive potential.
 
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  Publisher Elsevier Place of Publication Editor  
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  ISSN 0301-4797 ISBN Medium  
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  Notes Approved no  
  Call Number THL @ luqianxue.zhang @ dePaz2006 Serial 47  
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Author Demirak, A.; Balci, A.; Karaoğlu, H.; Tosmur, B. url  openurl
  Title Chemical characteristics of rain water at an urban site of south western Turkey Type Journal Article
  Year (up) 2006 Publication Environmental monitoring and assessment Abbreviated Journal  
  Volume 123 Issue 1-3 Pages 271-283  
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  Corporate Author Thesis  
  Publisher Springer Place of Publication Editor  
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  ISSN 0167-6369 ISBN Medium  
  Area Expedition Conference  
  Notes Approved no  
  Call Number THL @ luqianxue.zhang @ Demirak2006 Serial 56  
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Author Mihajlidi-Zelić, A.; Deršek-Timotić, I.; Relić, D.; Popović, A.; Đorđević, D. url  openurl
  Title Contribution of marine and continental aerosols to the content of major ions in the precipitation of the central Mediterranean Type Journal Article
  Year (up) 2006 Publication Science of the total environment Abbreviated Journal  
  Volume 370 Issue 2-3 Pages 441-451  
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  Address  
  Corporate Author Thesis  
  Publisher Elsevier Place of Publication Editor  
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  Series Editor Series Title Abbreviated Series Title  
  Series Volume Series Issue Edition  
  ISSN 0048-9697 ISBN Medium  
  Area Expedition Conference  
  Notes Approved no  
  Call Number THL @ luqianxue.zhang @ Mihajlidi-Zelić2006 Serial 60  
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