1997
DOI: 10.2134/agronj1997.00021962008900050003x
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Nitrogen Release from Surface‐Applied Cover Crop Residues: Evaluating the CERES‐N Submodel

Abstract: Further improvement of residue decomposition models may help to optimize the use of N released from cover crop residues. CERES models are widely used to simulate crop‐soil systems and have a common subroutine that describes N dynamics (CERES‐N). In this work, we tested CERES‐N with results from a litterbag study over 120 d in which crimson clover (Trifolium incarnatum (L.), rye (Secale cereale( L.), wheat (Triticum aestivum( L.), and oat (Avena sativa L.) residues were allowed to decompose on the soil surface.… Show more

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Cited by 42 publications
(19 citation statements)
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“…Crop residues retain water and reduce soil temperature (Quemada and Cabrera, 2002). Decomposition rates of crop residues covering the soil are lower than incorporated residues, the risk of ammonia volatilization increases when stubble and fertilizers remain on the soil surface, and larger N immobilization is expected in conservation tillage (Quemada et al, 1997). Because of these factors, optimum fertilization is even more important with conservation than with conventional tillage (Wang et al, 2011).…”
Section: -Soil Mulchingmentioning
confidence: 99%
“…Crop residues retain water and reduce soil temperature (Quemada and Cabrera, 2002). Decomposition rates of crop residues covering the soil are lower than incorporated residues, the risk of ammonia volatilization increases when stubble and fertilizers remain on the soil surface, and larger N immobilization is expected in conservation tillage (Quemada et al, 1997). Because of these factors, optimum fertilization is even more important with conservation than with conventional tillage (Wang et al, 2011).…”
Section: -Soil Mulchingmentioning
confidence: 99%
“…A complete description of the methodology used for these simulations and preliminary results can be found in Guereña et al (2001), Mínguez et al (2004Mínguez et al ( , 2007 and Olesen et al (2007). Briefly, CERES wheat and maize models (Ritchie & Otter 1985, Jones & Kiniry 1986, within the DSSAT 3.5 frame, Tsuji et al 1994), previously calibrated for various Iberian locations (Mariscal 1993, Rebollo 1993, Iglesias & Mínguez 1995, Quemada et al 1997, López-Cedrón et al 2005, were used to perform simulations for the control period and the A2 scenario using daily outputs from RCMs. Maximum and minimum temperature, solar radiation, precipitation, wind speed and relative humidity at surface level were formatted according to weather files of the crop models, thus applying the 'direct use' method.…”
Section: Multi-model Ensemble Of Climate and Impact Projectionsmentioning
confidence: 99%
“…Thus allowing the distribution of carbon between the three FPOOLs to be a model input that characterizes the organic substrate will alter the rate of net N mineralization (as shown by Quemada and Cabrera, 1995;Quemada et al, 1997). However changing the pool sizes alone cannot alter whether a source exhibits initial net N mineralization or immobilization (since this is determined by the C:N ratio of the substrate).…”
Section: Modelling the Decomposition Of Organic Sourcesmentioning
confidence: 99%