4.7 Article

Impacts of fire on soil respiration and its components A global meta-analysis

期刊

AGRICULTURAL AND FOREST METEOROLOGY
卷 336, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.agrformet.2023.109496

关键词

Atmospheric CO 2 flux; Autotrophic respiration; Heterotrophic respiration; Terrestrial ecosystem; Wildfire

向作者/读者索取更多资源

The effects of fire on soil respiration (SR) and heterotrophic respiration (HR) depend on fire severity and type. High and low severity fires reduce SR and HR, while moderate severity fires have negligible effects. Wildfires significantly decrease SR and HR, while prescribed fire decreases SR but does not affect HR. The responses also vary with ecosystem types. Additionally, the changes in soil organic C, dissolved C, microbial biomass C, and belowground biomass are the main drivers of the effects of fire on SR and HR.
As a general disturbance in terrestrial ecosystems, fire can have far-reaching consequences on the carbon (C) cycle. Although soil respiration (SR) is important in regulating atmospheric CO2 concentrations, a general pattern of the response of SR to fire in terrestrial ecosystems remains unclear. In this study, a meta-analysis of 91 studies on fires across 116 global sites was conducted to investigate the effects of fire on SR and its components. The results revealed that the responses of SR and heterotrophic respiration (HR) to fire were dependent on fire severity (low-, moderate-, and high-severity) and types (wildfire and prescribed fire). Specifically, the high- and low-severity fires reduced SR and HR, whereas moderate-severity fires had negligible effects on these parameters. On average, wildfires significantly decreased SR and HR by 13.9% and 18.6%, respectively, across all ecosystems, while prescribed fire reduced SR by 8.4% but did not change HR. In addition, the responses of SR and HR varied with the ecosystem types. Fire decreased SR in all three types of forests (boreal forests: -14.8%, temperate forests: -13.8%, and tropical forests: -28.9%), whereas decreased HR only in boreal and temperate forests (-23.8% and 20.7%, respectively) but not in tropical forests. Moreover, SR decreased directly followed by an increase, whereas HR declined with time after low- and high-severity fires. At a global scale, the responses of SR and HR to fire largely resulted from the changes in soil organic C, dissolved C, microbial biomass C, and belowground biomass, as indicated by the correlation analysis. In addition, the response of SR to fire was negatively affected by the mean annual precipitation in the forests. Overall, our study revealed the mechanisms driving the effects of fire and provided a framework for understanding soil C emissions under intensified fire regimes.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据