科研之友
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摘要
Soil CO2 efflux varies significantly in time and space in terrestrial ecosystems, obtaining a detailed understanding of what controls the dynamics of soil respiration (SR) can improve the estimation accuracy of forest carbon budgets. We examined the effects of forest conversion (from primary forest to both secondary forest and coniferous plantations) on the temporal dynamics of SR and its components (heterotrophic = R-H, and autotrophic = R-A), at both seasonal and inter-annual time scales within four adjacent forest stands in northeastern China. Trenching method was used to partition R-H and R-A. The results showed that RH was the primary contributor to the overall magnitude and variability of SR, which showed similar seasonal and inter-annual variation, while R-A displayed higher temporal variation compared to SR and R-H. Generally, the between-year seasonal variation of SR and R-H varied significantly in both secondary forest and plantations. The secondary forest exhibited a relatively higher seasonal change in R-A compared to that in primary forest and coniferous plantations, while there was no significant disparity in the seasonal and inter-annual variation of SR and R-H among forest stands. Soil temperature was the primary factor driving the temporal dynamics of R-H and accounted for 63-91% and 22-64% of seasonal and inter-annual variations, respectively. However, R-A was less controlled by soil temperature. This study implies that forest conversion magnifies the responses of R-H to the minor variations in the between-year seasonal patterns of soil temperature and increases the seasonal variability of R-A.
