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The hydrogeochemistry and isotope geochemistry of groundwater from 85 wells in fractured dolomite aquifers of Central Slovenia were investigated. This groundwater represents waters strongly influenced by chemical weathering of dolomite with an average of δ13CCARB value of +2.2 ‰. The major groundwater geochemical composition is HCO3 ? > Ca2+ > Mg2+. Several differences in hydrogeochemical properties among the classes of dolomites were observed when they were divided based on their age and sedimentological properties, with a clear distinction of pure dolomites exhibiting high Mg2+/Ca2+ ratios and low Na+, K+ and Si values. Trace element and nutrient concentrations (SO4 2?, NO3 ?) were low, implying that karstic and fractured dolomite aquifers are of good quality to be used as tap water. Groundwater was generally slightly oversaturated with respect to calcite and dolomite, and dissolved CO2 was up to 46 times supersaturated relative to the atmosphere. The isotopic composition of oxygen (δ18OH2O), hydrogen (δDH2O) and tritium ranged from ?10.3 to ?8.4 ‰, from ?68.5 to ?52.7 ‰ and from 3.5 TU to 10.5 TU, respectively. δ18O and δD values fell between the GMWL (Global Meteoric Water Line) and the MMWL (Mediterranean Meteoric Water Line) and indicate recharge from precipitation with little evaporation. The tritium activity in groundwater suggests that groundwater is generally younger than 50 years. δ13CDIC values ranged from ?14.6 to ?9.3 ‰ and indicated groundwater with a contribution of degraded organic matter/dissolved inorganic carbon in the aquifer. The mass balances for groundwater interacting with carbonate rocks suggested that carbonate dissolution contributes from 43.7 to 65.4 % and degradation of organic matter from 34.6 to 56.3 %. 相似文献
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Many Mediterranean areas have recently witnessed a proliferation of new urban and tourist-related features following low-density residential patterns that contrast with the traditional high-density urban typologies of Mediterranean cities. The aim of this research is to investigate the links between residential tourism and water consumption through swimming pools, which constitute one key element of the new urban landscapes in the coast of Alicante (southeastern Spain). We have digitized pools in nine municipalities of coastal Alicante and calculated the average depth and estimated water losses due to evaporation. Results show that swimming pools are widely available in tourist residential enclaves but that they tend to display different characteristics according to factors such as the history of the urbanization process and relative wealth of the different areas. We have detected a clear contrast between the large individual pools of the richer northern municipalities and the smaller individual pools and community pools in the newly developed but less well-off urban enclaves of the southern coast. 相似文献
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A conventional value for the geoid reference potential W_{0} 总被引:1,自引:1,他引:0
L. Sánchez R. Čunderlík N. Dayoub K. Mikula Z. Minarechová Z. Šíma V. Vatrt M. Vojtíšková 《Journal of Geodesy》2016,90(9):815-835
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