Modeling of crop residue decomposition for nutrient cycling and effect
iveness of residues to control soil erosion requires information on cr
op-specific decomposition coefficients (k). Respiration of decomposing
residues reflects the activity of the microbial community and should
give an indication of the residue decomposition rate. A method for est
imating k using substrate-induced respiration (SIR) of plant residues
was evaluated. Basal respiration, total SIR, fungal SIR and bacterial
SIR were measured for five crop residues monthly for 1 y. In general,
total SIR and basal respiration declined for the more decomposable res
idues, but were somewhat constant for the more resistant residues. Mas
s loss was used to determine k for a single exponential decay function
. Prediction of k from SIR using an equation proposed by Neely et al.
(1991) (Soil Biology & Biochemistry 23, 947-954) was unsatisfactory fo
r the five crops. A new equation (k = -6.07 x 10(-4) + 6.23 x 10(-6) x
SIR) was determined using the data of Neely et al. (1991) and data fr
om the current study. Prediction of k using the 60-day SIR measurement
was significantly improved with the new equation. Predicting k from S
IR could greatly reduce the labor and time involved in evaluating deco
mposition differences between residues and locations. Published by Els
evier Science Ltd.