Karst Hydrological Zones
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Underground cavities with karst-hydrological activity percade the karstified region in a three-dimensional network. The movements of the water, especially the slow ones, are hindered only slightly so that there is a division in space, the accumulations of water below, the water-impoverishes areas above. The very dense network of interstices and narrow open joints shows a behavior of its own and will only be included in this division to a limited degree.
KeywordsVadose Zone Open Joint Karst Water Karst Spring Karstified Region
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