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Titlebook: Karst Hydrology; With Special Referen Ognjen Bonacci Book 1987 Springer-Verlag Berlin Heidelberg 1987 Drainage.geomorphology.groundwater.hy

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Water Temperature in Karst,rground, etc. In order to determine thermal changes such measurements should be carried out with sensitive equipment, since these variations have very small amplitudes, i.e. very often, a few tenths of 1 °C. According to Komatina (1984), favourable conditions exist in karst for the application of ge
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,Man’s Influence on the Water Regime in the Karst Terrains,e built with the same objective, i.e. to improve the water regime, and hence, the living conditions in the region. Today, intensive works are being carried out related to the regulation of the water regime in karst. Past experience has shown that many of these works have been suboptimal. The benefit
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Book 1987llaborate towards a better understanding of karst areas. Evidently, karst phenomena have not been sufficiently and carefully studied worldwide. It is equally true that the first theories on water circulation in karst were developed according to ex­ periences in the Dinaric karst. This can easily be
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