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a Dep. of Land, Air, and Water Resources, Univ. of California, Davis, CA, 95616
b Dep. of Agron. and Range Sci., Univ. of California, Davis, CA 95616
* Corresponding author (jabird{at}socrates.berkeley.edu)
The transition from open-field burning of straw residues to alternative residue management practices may affect soil C sequestration potential and the supply of nutrients to crops. A field study of dual-labeled (13C and 15N) rice (Oryza sativa L.) residues examined the effects of winter-fallow flooding (vs. nonflooded) and straw residue incorporation (vs. untilled, open-field burned residue) on straw C and N dynamics in soil organic matter (SOM) fractions. We examined the fate of C and N in the straw, crown, and root system in the incorporated treatments and the uncombusted stubble, crown, and roots in burned treatments during 1 yr. During the winter fallow, straw residue incorporation reduced residue 15N loss but increased residue 13C loss compared with burning. Straw 13C loss after 1 yr was unaffected by either winter flooding or straw management (77.1% of applied). Slightly more straw 15N was lost of that applied in burned (65.5 ± 3.5%) compared with incorporated (52.0 ± 3.8%) during 1 yr. A greater proportion of soil-recovered 13C remained as nonalkali extractable humics (humin) in burned (62.0%) compared with incorporated (40.8%). In contrast, incorporated treatments had a larger proportion of 15N remaining as mobile humic acid (MHA) than burned (42.4 vs. 37.7%). Straw incorporation increased the relative retention of straw 15N to 13C compared with burning, indicating that straw 15N additions with incorporation may increase soil organic N reserves at an even greater rate than the larger straw additions might predict. These results show that straw incorporation results in markedly different straw C and N sequestration pathways compared with untilled, open-field burned residues.
Abbreviations: GLM, general linear model IRGA, infrared gas analyzer IRMS, isotope ratio mass spectrometer LF, light fraction MFA, mobile fulvic acids MHA, mobile humic acids NF, nonwinter flooded PVC, polyvinyl chloride SMB, soil microbial biomass SOM, soil organic matter WF, winter flooded WHC, water-holding capacity
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