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Late Neogene to quaternary soil evolution across relict terraces in Northwest Florida
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Late Neogene to quaternary soil evolution across relict terraces in Northwest Florida

Chelsea Joel Randall
University of West Florida
Master of Science (MS), University of West Florida
2019

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Abstract

Delineation of relict terraces along the Northwest Florida coast can facilitate investigation of soil development within the Gulf of Mexico (GOM) coastal plain. Previous work to define terraces has primarily relied on topographic studies with little consensus on the number and extent of terraces. Research investigating soil development within the GOM coastal plain is also limited. The present study utilizes Geographic Information Systems (GIS) and a LiDAR derived Digital Elevation Model (DEM) to apply a Surface Classification Model (SCM) for selection of terrace surfaces based on slope and surface roughness. The SCM output was analyzed for peaks in pixel count by elevation. Five terraces were defined between the following elevation ranges: 0-3.6 m, 4-9 m, 16-27 m, 29.5-51 m, and 57-64 m. Soil properties known to exhibit time related trends were analyzed across the delineated terraces. At increasing elevations, and presumably ages, soils exhibited a thickening of both the solum and Bt horizon, an increase in clay content, and a decrease in organic matter content. Bt horizons were observed at increasingly greater depths, with the exception of terrace 5, which was at shallower depth. Likely due to erosion associated with the high elevation and greater exposure of the surface.
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