Document Type
Thesis
Degree
Master of Science (MS)
Major/Program
Geosciences
First Advisor's Name
Rene Price
First Advisor's Committee Title
Committee chair
Second Advisor's Name
Leonard Scinto
Second Advisor's Committee Title
Committee member
Third Advisor's Name
William Anderson
Third Advisor's Committee Title
Committee member
Keywords
peat, everglades, hydrologic, hydrogeology, saltwater intrusion, peat properties, peat sediments, shark river slough, srs
Date of Defense
5-17-2022
Abstract
Peat sediments are the foundation of most wetlands, acting as a medium for water to flow through, governed by hydraulic conductivity, and as a potential source of nutrients. Shark River Slough is a known, main fresh waterway for Everglades National Park, distributing essential nutrients and freshwater into the wetland. Hydraulic conductivity was calculated through experimental (both in situ water and higher salinity water) falling head tests performed on mangrove and sawgrass peat cores. Nutrient concentrations were analyzed for the pore water released during hydrologic testing. Hydraulic conductivity values were higher in the sawgrass peat than the mangrove peat. No significant difference was found in hydraulic conductivity between in situ and higher salinity water. Total dissolved phosphorous concentrations were higher in mangrove peat porewater than in sawgrass peat porewater. Higher hydraulic conductivity in sawgrass peat allows water and nutrients to be transported more easily between surface water and groundwater.
Identifier
FIDC010810
Recommended Citation
Cordoba, Nicole, "Hydrologic Properties of Mangrove and Sawgrass Peat in Shark River Slough, Everglades, Florida" (2022). FIU Electronic Theses and Dissertations. 5129.
https://digitalcommons.fiu.edu/etd/5129
Included in
Biogeochemistry Commons, Geochemistry Commons, Geology Commons, Hydrology Commons, Soil Science Commons
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