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Organic Matter Oxidation Potential Determination in a Periodically Flooded Histosol under Sugarcane

D. R. Morris*,a, B. Glaza and S. H. Daroubb

a USDA–ARS, Sugarcane Field Station, 12990 U.S. Hwy. 441, Canal Point, FL 33438
b Everglades Research and Education Center, Univ. of Florida, 3200 E. Palm Beach Road, Belle Glade, FL 33430



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Fig. 1. Mean benzoate C oxidation (A), soil respiration (B), and microbial biomass (C) averaged across the drainage period as influenced by water table treatments. The least square difference of the mean (LSD) was calculated from the day x water table interaction.

 


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Fig. 2. Mean soluble organic C (A), soil moisture (B), and soil temperatures at the 7-cm depth (C) averaged across the drainage period as influenced by water table treatments. The least square difference of the mean (LSD) was calculated from the day x water table interaction.

 





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