Abstract
It is generally considered that karst aquifers have distinctly different properties from other bedrock aquifers. A search of the literature found five definitions that have been proposed to differentiate karst aquifers from non-karstic aquifers. The five definitions are based upon the presence of solution channel networks, hydraulic conductivities >10−6 m/s, karst landscapes, channels with turbulent flow, and caves. The percentage of unconfined carbonate aquifers that would classify as ‘karst’ ranges from <1 to >50%.
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Worthington, S. R. H., Jeannin, P. Y., Alexander, E. C., Davies, G. J., & Schindel, G. M. (2017). Définitions contrastées pour le terme ‘aquifère karstique.’ Hydrogeology Journal, 25(5), 1237–1240. https://doi.org/10.1007/s10040-017-1628-7
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