The carbonate aggressiveness of water in the karst areas of the basin of the Chocholowski and Koscieliski streams (Western Tatra Mts.)

Grzegorz Barczyk

Abstract


Changes of the carbonate aggressiveness of water in the karst areas of the basin of the Chochołowski and Kościeliski streams (Western Tatra Mts.) are presented. The saturation index SI[c] is lowest for rainwater, higher for groundwater and highest for surface water. Most of the surface water flowing out of the West Tatra Mountains has the ability to dissolve carbonate rocks.

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