Temporal Variability in Soil Greenhouse Gas Fluxes and Influencing Factors of a Primary Forest on the Eastern Qinghai-Tibetan Plateau.

Soil greenhouse gas (GHG) fluxes relate to soil carbon and nitrogen budgets and have a significant impact on climate change. Nevertheless, the temporal variation and magnitude of the fluxes of all three major GHGs (CO₂, CH₄ and N₂O) and their influencing factors have not been elucidated clearly in primary forests on the eastern Qinghai-Tibetan Plateau. Herein, field chamber GHG fluxes from May to November, soil microbial community and enzyme activity were analyzed in a fir-dominated (Abies fargesii var. faxoniana) primary forest. The emission rates of CO₂ and N₂O ranged between 64.69–243.22 mg CO₂ m⁻² h⁻¹ and 1.69–5.46 ug N₂O m⁻² h⁻¹, exhibiting a temporally unimodal pattern with a peak in July. The soil acted as a CH₄ sink, and the uptake rate varied between 52.96 and 84.67 μg CH₄ m⁻² h⁻¹ with the higher uptake rates in June and November. The temporal variation in the CO₂ flux was significantly correlated with the geometric mean of enzyme activities, suggesting that the soil CO₂ flux was determined by microbial activity rather than soil microbial biomass. The soil N₂O flux was positively related to nitrate concentration with marginal significance, probably because N₂O was a byproduct of nitrification and denitrification processes. The soil CH₄ uptake was closely associated with methanotrophic biomass (18:1ω7c). The results highlight divergent temporal dynamics of GHG fluxes owing to different driving mechanisms and an important CH₄ sink in the primary forest soil, helping to evaluate the carbon and nitrogen budgets of primary forests on the eastern Qinghai-Tibetan Plateau. [ABSTRACT FROM AUTHOR]