Long-term thinning decreases the contribution of heterotrophic respiration to soil respiration in subalpine plantations
Longfei Chen , Zhibin He , Wenzhi Zhao , Xi Zhu , Qin Shen , Mingdan Song , Zhengpeng Li , Junqia Kong , Shuping Yang , Yuan Gao
Journal of Forestry Research ›› 2024, Vol. 35 ›› Issue (1) : 57
Interest in the dynamics of soil respiration (R s) in subalpine forest ecosystems is increasing due to their high soil carbon density and potential sensitivity to environmental changes. However, as a principal silvicultural practice, the long-term impacts of thinning on R s and its heterotrophic and autotrophic respiration components (R h and R a, respectively) in subalpine plantations are poorly understood, especially in winter. A 3-year field observation was carried out with consideration of winter CO2 efflux in middle-aged subalpine spruce plantations in northwestern China. A trenching method was used to explore the long-term impacts of thinning on R s, R h and R a. Seventeen years after thinning, mean annual R s, R h and R a increased, while the contribution of R h to R s decreased with thinning intensity. Thinning significantly decreased winter R s because of the reduction in R h but had no significant effect on R a. The temperature sensitivity (Q 10) of R h and R a also increased with thinning intensity, with lower Q 10 values for R h (2.1–2.6) than for R a (2.4–2.8). The results revealed the explanatory variables and pathways related to R h and R a dynamics. Thinning increased soil moisture and nitrate nitrogen (${\text{NO}}_{3}^{ - }$-N), and the enhanced nitrogen and water availability promoted R h and R a by improving fine root biomass and microbial activity. Our results highlight the positive roles of ${\text{NO}}_{3}^{ - }$-N in stimulating R s components following long-term thinning. Therefore, applications of nitrogen fertilizer are not recommended while thinning subalpine spruce plantations from the perspective of reducing soil CO2 emissions. The increased Q 10 values of R s components indicate that a large increase in soil CO2 emissions would be expected following thinning because of more pronounced climate warming in alpine regions.
Heterotrophic respiration / Autotrophic respiration / Long-term thinning impacts / Cold seasons / Subalpine plantations / Temperature sensitivity
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