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Nitrogen Dynamics in Humic Fractions under Alternative Straw Management in Temperate Rice

Jeffrey A. Birda, Chris van Kesselb and William R. Horwath*,a

a Dep. of Land, Air and Water Resources, One Shields Avenue, University of California, Davis, CA 95616
b Dep. of Agronomy and Range Science, University of California, Davis, CA 95616



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Fig. 1. Nitrogen-15 atom excess values (%) of Soil organic matter fractions, 1997 through 1999 (0–15 cm depth). Least-squares means, standard errors (N = 16, average of all treatments). All treatments were flooded during the cropping season while only the winter flooded treatments were flooded during the winter fallow period.

 


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Fig. 2. Nitrogen-15 fertilizer in SOM fractions as a percentage of total 15N recovery as soil N over a 2-yr period (1997–1999) in the 0- to 15-cm soil depth. Least-squares means, standard errors (N = 16, averaged across treatments).

 


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Fig. 3. Percentage of recovery of applied 15N fertilizer in LF over a 2-yr period (1997–1999) in the 0- to 15-cm soil depth when straw was incorporated or burned and the fields were winter-flooded (WF) or nonwinter flooded (NF). Least-squares means, standard errors (N = 4).

 


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Fig. 4. Percentage of recovery of applied 15N fertilizer in MHA, MFA, MAHA, and HUM fractions over a 2-yr period (1997–1999) in the 0- to 15-cm soil depth when straw was incorporated or burned and the fields were winter-flooded (WF) or nonwinter flooded (NF). Least-squares means, standard errors (N = 4).

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
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Vadose Zone Journal
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Environmental Quality
The Plant Genome
Copyright © 2002 by the Soil Science Society of America.