Abstract
Karst evolution in its dimensions of space and time depends on the dissolution kinetics of limestone. The time needed to excavate conduits by solutional removal of limestone depends on the rates of dissolution. The length of these flow conduits is determined by the distance calcite-aggressive water can travel until it becomes saturated. This penetration distance is related to the velocity of flow and also to the kinetics of dissolution.
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.
