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Publication Date
2007
Publication Title
Time in Karst
Abstract
Paper presents a simple mathematical model, which enables study of denudation rates in karst. A vertical flow of water which is uniformly infiltrated at the surface is assumed. Denudation rate is calculated from the time needed to remove certain thickness of rock. This is done concretely on a limestone block dissected by a vertical array of fractures. It is shown that denudation rate increases with the thickness of removed layer and approaches an upper limit which is defined by the maximum denudation equations, which are based on assumption that all dissolution potential is projected into a surface lowering.
Keywords
Karst, Denudation rate, Limestone dissolution, Mathematical model
Document Type
Article
Language
English and Slovenian
Identifier
K26-00156
Recommended Citation
Gabrovšek, Franci, "On Denudation Rates in Karst" (2007). KIP Articles. 46.
https://digitalcommons.usf.edu/kip_articles/46