Abstract

To assess the effects of long-term intensive management on soil carbon cycle and microbial functional diversity, we sampled soil in Chinese hickory (Carya cathayensis Sarg.) stands managed intensively for 5, 10, 15, and 20 years, and in reference Chinese hickory–broad-leaved mixed forest (NMF) stands. We analyzed soil total organic carbon (TOC), microbial biomass carbon (MBC), and water-soluble organic carbon (WSOC) contents, applied 13C-nuclear magnetic resonance analysis for structural analysis, and determined microbial carbon source usage. TOC, MBC, and WSOC contents and the MBC to TOC ratios were lower in the intensively managed stands than in the NMF stands. The organic carbon pool in the stands managed intensively for twenty years was more stable, indicating that the easily degraded compounds had been decomposed. Diversity and evenness in carbon source usage by the microbial communities were lower in the stands managed intensively for 15 and 20 years. Based on carbon source usage, the longer the management time, the less similar the samples from the monospecific Chinese hickory stands were with the NMF samples, indicating that the microbial community compositions became more different with increased management time. The results call for changes in the management of the hickory stands to increase the soil carbon content and restore microbial diversity.

Highlights

  • Soil organic carbon is one of the main factors affecting the storage and supply of nutrients in soil, soil structure stability, soil water-holding capacity, and soil biological activity [1,2]

  • Labile organic carbon plays an important role in maintaining fertility and reflecting changes in soil carbon storage, and it is more sensitive to changes in the microenvironment than other forms of organic carbon [6,7,8]

  • The results suggest that the total organic carbon (TOC) contents in the managed stands could not be expected to increase under intensive management

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Summary

Introduction

Soil organic carbon is one of the main factors affecting the storage and supply of nutrients in soil, soil structure stability, soil water-holding capacity, and soil biological activity [1,2]. It is one of the main indicators for evaluating soil fertility and sustainable land use, as it is associated with different soil physico-chemical and biological processes [3]. The quality, quantity, and distribution of soil organic carbon reflects the spatial distribution of surface plant communities [4,5]. Soil labile organic carbon is mineralized by microorganisms. As the main players and regulators of soil nutrient cycles and biochemical processes, soil microbes are one of the most active

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