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Hydrologic Gradients and Topsoil Additions Affect Soil Properties of Virginia Created Wetlands

G. L. Brulanda,* and C. J. Richardsonb

a Soil and Water Science Dep., Univ. of Florida, Institute of Food and Agricultural Sciences, 2169 McCarty Hall, P.O. Box 110290, Gainesville, FL 32611-0290
b Duke Univ. Wetland Center, Nicholas School of the Environment and Earth Sciences, Box 90333, Durham, NC 27708-0333



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Fig. 1. Map of study site locations across the Coastal Plain of Virginia.

 


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Fig. 2. Effect of position along the hydrologic gradient and topsoil status on (a) soil moisture, (b) bulk density, (c) soil organic matter, (d) clay, (e) silt, (f) sand, (h) water holding capacity, (h) the P sorption index, and (i) microbial biomass C. Data presented are means and error bars represent ±1 standard error. Data points with different letters are significantly different at the p < 0.10 level according to a least-squared differences test.

 





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