Abstract

BackgroundThe carbon pools of forest soils play a vital role in global carbon sequestration and emissions. Forest management can regulate the sequestration and output of forest soil carbon pools to a certain extent; however, the kinetics of the effects of forest density on soil carbon pools require further investigation.MethodsWe established sample plots with stand density gradients in three different aged Larix principis-rupprechtii plantations and quantified the soil respiration, soil organic carbon (SOC), soil dissolved organic carbon (DOC), microbial biomass carbon (MBC), light fraction organic carbon (LFOC), and readily oxidized carbon (ROC).Results and conclusionsDuring the growth and development of plantations, stand density is an essential factor that impacts soil respiration and its associated elements. Moderate density was observed to promote both the soil and heterotrophic respiration rates and the sequestration of MBC and LFOC, whereas it inhibited the sequestration of ROC. The soil, heterotrophic, and autotrophic respiration rates of older forest stands were relatively rapid, whereas the contents of SOC, MBC, LFOC, DOC, and ROC were higher and more sensitive to changes in stand density. The MBC, LFOC, and ROC in soil labile organic carbon were closely related to both the soil and heterotrophic respiration, but not the SOC. Among them, the LFOC and MBC played the roles of “warehouse” and “tool” and were significantly correlated with soil and heterotrophic respiration. The ROC, as a “raw material”, exhibited a significantly negative correlation with the soil and heterotrophic respiration. When the soil and heterotrophic respiration rates were rapid, the ROC content in the soil maintained the low level of a “dynamically stabilized” state. The stand density regulated heterotrophic respiration by affecting the soil labile organic carbon, which provided an essential path for the stand density to regulate soil respiration.

Highlights

  • Forests comprise the world’s largest ecosystems, which contain tremendous quantities of carbon that are sequestered by plants (Poorter et al 2016; Khan et al 2018; Franklin et al 2009)

  • Except for the dissolved organic carbon (DOC) and light fraction organic carbon (LFOC), other organic carbon measures were not very sensitive to the interactive effects of stand density and age, which meant that the regulating effects of stand density on soil respiration were significant

  • Effects of stand density on soil respiration We analyzed the differences between the Rs, Heterotrophic respiration (Rh), and Ra at different density levels and employed the advantages of density sequence diagrams to discover the trends of these indicators with stand density

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Summary

Introduction

Forests comprise the world’s largest ecosystems, which contain tremendous quantities of carbon that are sequestered by plants (Poorter et al 2016; Khan et al 2018; Franklin et al 2009). It was considered that soil respiration (Rs) involves autotrophic respiration (Ra) and heterotrophic respiration (Rh), whereby the decomposition of microorganisms and turnover of roots in the soil are the main forms of heterotrophic and autotrophic respiration, respectively (Baggs 2006; Xu and Shang 2016; Hopkins et al 2013). This process provides a better understanding of the soil respiration mechanism and the various factors that influence it. Forest management can regulate the sequestration and output of forest soil carbon pools to a certain extent; the kinetics of the effects of forest density on soil carbon pools require further investigation

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