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Na podstawie wyników badań hydrogeologicznych przeprowadzonych w rejonie Hornsundu (SW Spitsbergen) określono średnią wielkość odpływu całkowitego Q = 3,346 m3/s. Pomiary prowadzono w strefie wybrzeża Morza Grenlandzkiego o powierzchni 49,95 km2, ograniczonego lodowcami Werenskiolda i Hansa w sezonach letnich 2005–2007. Na odpływ całkowity składają się odpływy: rzeczny (3,008 m3/s) i podpowierzchniowy...
The hydrogeochemical background of electrolytical conductivity (36–188 µS/cm) and pH (from 6.23 to 7.35) of groundwater occurred in active layer of permafrost in the Hornsund region (SW Spitsbergen) was determined based on data collected in summer season of 2005. The shallow zone of water circulation (supramermafrost zone) in Arctic regions results during intensive melting of snow, glaciers and top...
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