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Abstract. Oxygen-18 content and hydrochemistry of the springs issuing from Semmering Massif was intensively monitored with the aim of characterizing the recharge areas and hydrochemical evolution. The 18O-altitude effect was determined using isotopic and hydrogeological data for small, mainly crystalline reference springs; it was approximated at 0.27 and 0.21/100m respectively for the northern and...
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