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Seasonal Nutrient Dynamics of Forested Floodplain Soil Influenced by Microtopography and Depth

Donald M. Stoeckel and Mary S. Miller-Goodman

Dep. Agronomy and Soils, Auburn Univ., Auburn, AL 36849



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Fig. 1. Seasonal nutrient dynamics in surface organic material at plots from two microtopographic classes (swales and slopes) on the Coosawhatchie River floodplain. Bars within a cluster with the same letter are not significantly different (P < 0.10). Letters in parentheses indicate values greater than the corresponding value of the other microtopographic class (P < 0.10)

 


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Fig. 2. Seasonal nutrient ratios in mineral soil from two microtopographic classes (swale and slope) at two depths (root zone and sub-root) on the Coosawhatchie River floodplain. Bars within a cluster with the same letter represent ratios that did not differ with season (P < 0.10). Letters in parentheses indicate values greater than the corresponding value from the other microtopographic class (P < 0.10). Missing bars in the SR layer during winter represent data not collected due to flooding

 





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