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Cover crop effects on nitrogen mineralization and availability in conservation tillage cotton
Authors:Email author" target="_blank">Harry?H?SchombergEmail author  Dinku?M?Endale
Institution:(1) Agricultural Research Service, United States Department of Agriculture, J. Phil Campbell Sr. Natural Resource Conservation Center, 1420 Experiment Station Road, Watkinsville, Georgia, USA
Abstract:Understanding cover crop influences on N availability is important for developing N management strategies in conservation tillage systems. Two cover crops, cereal rye (Secale cereale L.) and crimson clover (Trifolium incarnatum L.), were evaluated for effects on N availability to cotton (Gossypium hirsutum L.) in a Typic Kanhapludult soil at Watkinsville, Ga. Seed cotton yields following clover and rye were 882 kg ha–1 and 1,205 kg ha–1, respectively, in 1997 and were 1,561 kg ha–1 and 2,352 kg ha–1, respectively, in 1998. In 1997, cotton biomass, leaf area index, and N were greater on some dates following crimson clover than following rye but not in 1998. During 1997, net soil N mineralized increased with time in both systems, but a similar response was not observed in 1998. Net soil N mineralization rates following crimson clover and rye averaged, respectively, 0.58 kg and 0.34 kg N ha–1 day–1 in 1997 and 0.58 kg and 0.23 kg N ha–1 day–1 in 1998. Total soil N mineralized during the cotton growing season ranged from 60 kg ha–1 to 80 kg ha–1 following crimson clover and from 30 kg ha–1 to 50 kg ha–1 following rye. Soil N mineralization correlated positively with heat units and cumulative heat units. Net soil N mineralization rates were 0.023 kg ha–1 heat unit–1 once net mineralization began. Soil heat units appeared to be a useful tool for evaluating N mineralization potential. Nearly 40% of the rye and 60% of the clover biomass decomposed during the 6 weeks prior to cotton planting, with nearly 35 kg N ha–1 mineralized from clover.
Keywords:Nitrogen mineralization  Heat units  Crop residue decomposition  Cotton growth
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