Annual ecosystem respiration variability of alpine peatland on the eastern Qinghai–Tibet Plateau and its controlling factors

Peatlands are widely developed in the eastern Qinghai–Tibet Plateau, but little is known about carbon budgets for these alpine peatland ecosystems. In this study, we used an automatic chamber system to measure ecosystem respiration in the Hongyuan peatland, which is located in the eastern Qinghai–Tibet Plateau. Annual ecosystem respiration measurements showed a typical seasonal pattern, with the peak appearing in June. The highest respiration was 10.43 μmol CO 2 /m 2 /s, and the lowest was 0.20 μmol CO 2 /m 2 /s. The annual average ecosystem respiration was 2.06 μmol CO 2 /m 2 /s. The total annual respiration was 599.98 g C/m 2 , and respiration during the growing season (from May to September) accounted for 78 % of the annual sum. Nonlinear regression revealed that ecosystem respiration has a significant exponential correlation with soil temperature at 10-cm depth ( R 2 = 0.98). The Q 10 value was 3.90, which is far higher than the average Q 10 value of terrestrial ecosystems. Ecosystem respiration had an apparent diurnal variation pattern in growing season, with peaks and valleys appearing at approximately 14:00 and 10:00, respectively, which could be explained by soil temperature and soil water content variation at 10-cm depth.