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USGS · 70241576

Sediment and sediment-associated contaminant transport through karst

Barbara Mahler·J.-C. Personne·F. Leo Lynch·Peter C. Van Metre
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Abstract

The unusual characteristics of subterranean flow in karst aquifers allow for the transport of sediment. Kartst ground-water system are created by dissolution of the bedrock matrix coupled with structural and stratigraphic controls. As a result, high flow velocities, large-diameter openings, and turbulent flow, all necessary for the entrainment and transport of particles, are present—at least episodically—in most karst systems.

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Barbara Mahler, J.-C. Personne, F. Leo Lynch, Peter C. Van Metre. 2007. Sediment and sediment-associated contaminant transport through karst. https://doi.org/10.1007/978-1-4020-5766-3_2

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