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- W2018689912 abstract "Soil water content, θ, is a major factor affecting residue decomposition, but simple formulation of this factor is often lacking. We observed that θ significantly (P < 0.001) affected the residue decomposition constant, k d. When θ varied from 0.09 g g−1 to 0.23 g g−1, k d ranged from 0.009 to 0.013 d−1 and from 0.009 to 0.022 d−1 for residues with carbon to nitrogen ratio (C/N) > 30 and C/N < 25, respectively. A θ factor was formulated in terms of the field capacity θ FC and the air‐dry θ d in the form f w = (θ − θ d) / (θ FC − θ d), and this was used to modify the potential k d as θ varied. Coupling f w with a first‐order residue decomposition equation resulted in the prediction of the decomposition of four residue types in the greenhouse (R2 = 0.94; relative root mean square error, RRMSE, = 0.06) and in the field (R2 = 0.93; RRMSE = 0.11)." @default.
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- W2018689912 date "2010-02-01" @default.
- W2018689912 modified "2023-09-27" @default.
- W2018689912 title "Simple Formulation of the Soil Water Effect on Residue Decomposition" @default.
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- W2018689912 doi "https://doi.org/10.1080/00103620903460781" @default.
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