The chapter describes the correlations between the hydrogeological, structural and geochemical parameters in Slovenian dolomites. 15 different dolomite types were analyzed, which are visually not distinguishable. However, differences appear when analyzing the hydrogeological parameters (hydraulic conductivity, specific capacity etc.), where more "clean" dolomites have higher transmissivities than the others. This is confirmed by geochemical analysis of ground waters. As a new result, correlations were found between the mentioned parameters and the fractal flow dimension.
COBISS.SI-ID: 880734