Abstract
Karst is regarded as a geological and physicochemical process of interaction between the natural water and soluble rock. Its development is possible only under non-equilibrium conditions in the “groundwater–congruently soluble rock” system. It is shown that intense karst development, leading to the formation of underground cavities and passages, is possible in the presence of advective transport of dissolved substance, which can redistribute its considerable amounts in a relatively short time. The specific features of karst development are considered in the case of its manifestation in carbonate, sulfate, and chloride rocks.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
