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USDA-ARS, 119 Keim Hall, East Campus, Univ. of Nebraska, Lincoln, NE 68583-0915
Dep. of Agronomy, Plant Science Bldg., Univ. of Georgia, Athens, GA 30602
USDA-ARS, Durant, OK 74702
*Corresponding author.
ABSTRACT
Efficient use of fertilizer N requires an assessment of the N contribution from decomposing crop residues. The objectives of this study were to quantify and model the amount of mineralized N recovered by a growing crop from 15N-labeled sorghum (Sorghum bicolor [L.] Moench) residues of variable N concentration and composition. The residues were incorporated into the surface soil of field microplots. The microplots were double-cropped with sorghum and wheat (Triticum aestivum L.) for a 3-yr period. The 15N tag in the crop residue was used to distinguish between residue-derived N and that from soil organic matter. Between 4.5 and 25% of the residue N applied (36–83 kg N ha–1 was applied as crop residue N) was recovered by a sorghum crop 110 d after incorporation. This constituted 56 to 77% of the total N recovered during a 3-yr period. Accumulated N recovered over time was described by modified first-order models. Regression analysis indicated that 93% of the variability in N recovered by 110 d could be explained using the C/N ratio and acid-detergent fiber contents of the residues. Measurements of N mineralized, using the method described above, were compared with predicted N mineralized, using MINIMO (a subroutine of the CERES-Maize model). After adjusting MINIMO parameters using data collected 110 d after residue incorporation, the slope and intercept of a linear fit between measured and MINIMO-predicted N mineralized 1097 d after residue incorporation were not different from one and zero, respectively.
Research partially sponsored by Tennessee Valley Authority, Muscle Sholas, AL, and USDA-ARS in cooperation with the Dep. of Agronomy, Kansas State Univ., Manhattan. Contribution no. 90-385-J of the Kansas Agric. Exp. Stn.
Received for publication March 2, 1990.
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