Assessment of the spatial distribution of soil properties in a northern Everglades marsh.

J Environ Qual

GIS Research Laboratory, Soil and Water Science Department, University of Florida-Institute of Food and Agricultural Sciences, Gainesville 32611-0510, USA.

Published: October 2006

AI Article Synopsis

  • The Florida Everglades restoration plans focus on preserving the landscape's soil, vegetation, and water flow patterns.
  • A detailed study sampled three soil layers in Water Conservation Area 1, measuring various properties including bulk density and nutrient content.
  • The research identified significant spatial patterns in soil properties, such as a gradient from north to south, nutrient enrichment along the western canal, and iron enrichment along the eastern canal, while also highlighting uncertainty in predicting certain soil characteristics.

Article Abstract

Florida Everglades restoration plans are aimed at maintaining and restoring characteristic landscape features such as soil, vegetation, and hydrologic patterns. This study presents the results from an exhaustive spatial sampling of key soil properties in Water Conservation Area 1 (WCA 1), which is part of the northern Everglades. Three soil strata were sampled: floc, upper 0- to 10-cm soil layer, and 10- to 20-cm soil layer. A variety of properties were measured including bulk density (BD), loss on ignition (LOI), total phosphorus (TP), total inorganic phosphorus (TIP), total nitrogen (TN), total carbon (TC), total iron (TFe), total magnesium (TMg), total aluminum (TAl), and total calcium (TCa). Interpolated maps and model prediction uncertainties of properties were generated using geostatistical methods. We found that the uncertainty associated with spatial predictions of floc, particularly floc BD, was highest, whereas spatial predictions of soil chemical properties such as soil Ca were more accurate. The resultant spatial patterns for these soil properties identified three predominant features in WCA 1: (i) a north to south gradient in soil properties associated with the predominant hydrological gradient, (ii) areas of considerable soil nutrient enrichment along the western canal of WCA 1, and (iii) areas of considerable Fe enrichment along the eastern canal. By using geostatistical techniques we were able to describe the spatial dynamics of soil variables and express these predictions with an acceptable level of uncertainty.

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Source
http://dx.doi.org/10.2134/jeq2005.0255DOI Listing

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