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Soil Aggregation and Carbon and Nitrogen Pools under Rhizoma Peanut and Perennial Weeds

U. M. Sainju*, T. H. Terrill, S. Gelaye and B. P. Singh

Agricultural Res. Stn., Fort Valley State Univ., 1005 State University Drive, Fort Valley, GA 31030



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Fig. 1. Concentrations of (A) NH4–N, (B) potential C mineralization, and (C) microbial biomass C in whole-soil from the 0- to 90-cm depth under rhizoma peanut and weeds. Bars followed by different letters are significantly different between peanut and weeds and between soil depths at P <= 0.05 by the least square means test.

 


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Fig. 2. (A) Amount of particles as fragments retained in a 0.05-mm sieve used for determining particulate organic C and N after wet sieving of whole-soil extracted with sodium hexametaphosphate (particles > 0.05 mm), and (B) concentration of particulate organic N in whole-soil from the 0- to 90-cm depth under rhizoma peanut and weeds. Bars followed by different letters are significantly different between peanut and weeds and between soil depths at P <= 0.05 by the least square means test.

 





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