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Geosciences 2018, 8(7), 268;

Diffuse Versus Conduit Flow in Coastal Karst Aquifers: The Consequences of Island Area and Perimeter Relationships

Department of Natural Sciences, Shawnee State University, 940 Second Street, Portsmouth, OH 45662, USA
Department of Geosciences, Mississippi State University, P.O. Box 5448, Mississippi State, MS 39762, USA
Author to whom correspondence should be addressed.
Received: 29 June 2018 / Revised: 15 July 2018 / Accepted: 17 July 2018 / Published: 20 July 2018
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The majority of limestone islands are made of eogenetic carbonate rock, with intrinsic high porosity and permeability. The freshwater lenses of small islands are dominated by diffuse flow regimes as the island perimeter is everywhere close to the meteoric catchment of the island interior. This flow regime produces flank margin caves at the lens margin, where dissolution is enhanced by mixing corrosion, superposition of organic decay horizons and higher flow velocities as the lens thins. The lens interior develops touching-vug flow systems that result in enhanced permeability and lens thinning over time. As islands become larger, the area (meteoric catchment) goes up by the square, but the island perimeter (discharge zone) goes up linearly; diffuse flow becomes inefficient; conduit flow develops to produce traditional epigenic cave systems that discharge the freshwater lens by specific turbulent flow routes, which in turn are fed by diffuse flow in the island interior. Locally, diffuse flow to the island perimeter continues in coastal proximal areas between major conduit flow routes to produce flank margin caves. The Bahamian Archipelago represents a case history in which tectonics is limited, the rocks are entirely eogenetic and the diffuse to conduit flow transition is demonstrated. View Full-Text
Keywords: carbonate island karst; flank margin caves; Bahamas; area/perimeter relationships carbonate island karst; flank margin caves; Bahamas; area/perimeter relationships

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Larson, E.B.; Mylroie, J.E. Diffuse Versus Conduit Flow in Coastal Karst Aquifers: The Consequences of Island Area and Perimeter Relationships. Geosciences 2018, 8, 268.

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