To quantitatively investigate the influence of plant nitrogen and ligni n content on the residue carbon decomposition, CO 2_C was measured from an incu ba tion experiment with 19 plant residues plus soil under 25 ℃ and water conte nt of 400 g·kg -1 air dried soil over a 9_week period. The 19 residues were sam pled fro m different organs with 13 plants, including Glycine max, Vigna sesquipedalis, D ioscorea esculenta, Luffa cylindrical, Oryza sativa, Zea mays, Triticum aestivum , Saccharum officinarum, Festuca arundinacea, Acorus calamus, Trapa quadrispinos a, Pi ttosporum tobira and Firmiana simplex. Weight loss of these residues was a lso ob tained from a field burying experiment over a 23_week period by using litter bag method. Decomposition of plant residues during the early 3_week incubation period was fa st with a wide variation. Thereafter the decomposition decreased and the variati on among residues became gradually insignificant. Cumulative amount of CO 2_C r el eased over the 9_week incubation period was found to be different among the resi dues. Average of the cumulative CO 2_C emission for all 19 residues was 178.0 m g, ranging from 103.6 mg for Oryza sativa root to 256.2 mg for Pittosporum t obira leaf. Correlation analysis indicated that decomposition of the plant res idue was positively dependent on its initial nitrogen content and negatively dependent o n its initial lignin content as well as the ratio of lignin to nitrogen. A furth er investigation suggested that the decomposition can be quantitatively describe d by Y=B 0+B 1N+B 2L. Parameters B 0, B 1 and B 2 are regressi on coefficients. The N and L represent the initial contents of nitrogen and lignin for a given residue, respectively. The Y could be either the first_order decay rate (B 0=3.51 ×10 -2 , B 1=4.61×10 -4 , B 2=-1.53×10 -4 , R 2=0.812 ** , n=19), or the percentage of CO 2_C re leased over the 9_week period (B 0=100, B 1=0.974, B 2=-0.364, R 2= 0.828 ** , n=19), or the percentage of weight loss over the 23_week period in the field burying e xperiment (B 0=150, B 1=1.496, B 2=-0.572, R 2=0.799 ** , n=17) . In addition, a good agreement (R 2=0.863 ** ,n=17) existed between amounts of the CO 2_C released from the incubation and the weight loss from the field burying experiment. It is concluded that decomposition of the plant residue either expressed as CO 2_ C emission in the laboratory incubation or as weight loss in the field burying e xperiment was significantly dependent on its initial contents of nitrogen and li gnin. Residues with higher nitrogen decomposed fast, while those with higher lig nin content decomposed slowly. Difference in the decomposition for various plant residues can be well identified over a 9_week incubation under 25 ℃ and water content of 400 g·kg -1 air dried soil. A further conclusion is that approx imately 8 0% of the variability in the decomposition can be quantitatively expressed by a linear combination of the initial contents of nitrogen and lignin for a given re sidue. The result also suggests that fraction of the labile carbon for a given p lant reside could be estimated from weight loss in the field burying experiment over a 23_week period.
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