Objective To study the effects of temperature and elemental content on annual seasonal dynamic of coarse woody debris (CWD) respiration rate (RCWD) and provide reference for calculating the carbon flux of CWD respiration and the establishment of carbon pool model.
Method The RCWD of Pinus massoniana and Lithocarpus glaber were measured using an infrared gas exchange analyzer (Li-Cor8100) and the CWD initial element content. The effect of temperature and element content on RCWD were discussed.
Result The dynamics of RCWD were in accordance with the trend of seasonal temperature, which showed a distinct single peak curve pattern. Within the temperature range of 14.5-28.5℃ measured, the RCWD was significant positively correlated with temperature (p < 0.01). The temperature can predict 64.0%-75.6% of P. massoniana RCWD, and 69.3%-86.2% of L. glaber RCWD. The Q10 of P. massoniana (3.05) was significantly lower than that of L. glaber (5.05). The RCWD of P. massoniana was less than that of L. glaber, meanwhile the initial C content of P. massoniana was significantly higher than that of the L. glaber, and the initial N and P content was significantly lower than that of the L. glaber. RCWD was negatively correlated with initial C content, C/N and C/P, and the correlation coefficients R2 were 0.383, 0.590 and 0.546 respectively. RCWD was positively correlated with the initial N content, the correlation coefficient R2 was 0.416. But there was no significant correlation among RCWD, P content and N/P. These indicated that initial element content can explain the 38.3%-59.0% of the RCWD changes.
Conclusion The study showes that temperature and initial C/N can explain more than half RCWD changes in what place. Temperature and initial element content significantly affect the whole process of CWD respiration or decomposition.