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
Long-term thinning decreases the contribution of heterotrophic respiration to soil respiration in subalpine plantations
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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