Document Type

Thesis

Degree

Master of Science (MS)

Department

Geosciences

First Advisor's Name

Michael C. Sukop

First Advisor's Committee Title

Committee Chair

Second Advisor's Name

Grenville Draper

Third Advisor's Name

Florentin Maurrasse

Fourth Advisor's Name

Dean Whitman

Keywords

Geoscience, Karst, Lattice Boltzmann Modeling

Date of Defense

6-27-2013

Abstract

The Pleistocene carbonate rock Biscayne Aquifer of south Florida contains laterally-extensive bioturbated ooltic zones characterized by interconnected touching-vug megapores that channelize most flow and make the aquifer extremely permeable. Standard petrophysical laboratory techniques may not be capable of accurately measuring such high permeabilities. Instead, innovative procedures that can measure high permeabilities were applied. These fragile rocks cannot easily be cored or cut to shapes convenient for conducting permeability measurements. For the laboratory measurement, a 3D epoxy-resin printed rock core was produced from computed tomography data obtained from an outcrop sample. Permeability measurements were conducted using a viscous fluid to permit easily observable head gradients (~2 cm over 1 m) simultaneously with low Reynolds number flow. For a second permeability measurement, Lattice Boltzmann Method flow simulations were computed on the 3D core renderings. Agreement between the two estimates indicates an accurate permeability was obtained that can be applied to future studies.

Identifier

FI13080708

Included in

Hydrology Commons

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