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  • . In the water of soils in the region composed of Magura strata less amounts of carbonates, sulphates and calcium were observed while there was more potassium than in the water of soils of the Inoceramus region. In the waters of bedrock of Magura strata
  • the principal components are sulphates and then carbonates. In the both areas average salts concentration in soil waters is lower than in bedrock waters. The quantity of material removed in solution is closely dependant on high water stages. The highest bulk