Self-organized permeability in carbonate aquifers

Advances over the past 40 years have resulted in a clear understanding of how dissolution processes in carbonate rocks enhance aquifer permeability. Laboratory experiments on dissolution rates of calcite and dolomite have established that there is a precipitous drop in dissolution rates as chemical...

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Bibliographic Details
Published inGround water Vol. 47; no. 3; p. 326
Main Authors Worthington, S R H, Ford, D C
Format Journal Article
LanguageEnglish
Published United States Ground Water Publishing Company 01.05.2009
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