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Chinese Journal of Applied Ecology ›› 2021, Vol. 32 ›› Issue (6): 1919-1927.doi: 10.13287/j.1001-9332.202106.028

• Special Features of Stable Isotope Ecology • Previous Articles     Next Articles

Vertical distribution of natural abundance of stable carbon and nitrogen isotopes along the soil profile and the underlying mechanisms

CHEN Miao1,2, LIU Shun1,2, XU Ge-xi1,2, SHI Zuo-min1,2,3*   

  1. 1Key Laboratory of Forest Ecology and Environment of National Forestry and Grassland Administration, Research Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China;
    2Miyaluo Research Station of Alpine Forest Ecosystem, Lixian 623100, Sichuan, China;
    3Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing 210037, China
  • Received:2020-12-30 Accepted:2021-04-09 Published:2021-12-15
  • Contact: * E-mail: shizm@caf.ac.cn
  • Supported by:
    Special Fund of Chinese Central Government for Basic Scientific Research Operations in Commonweal Research Institutes (CAFYBB2018ZA003) and the National Key R&D Program of China (2016YFC0502104-02).

Abstract: Understanding the changes of natural abundance of stable carbon and nitrogen isotopes (δ13C and δ15N) along soil profile is of great importance in revealing the mechanisms of soil carbon and nitrogen cycling in terrestrial ecosystems. Based on a comprehensive review on the distribution of δ13C and δ15N along soil profile, the mechanisms underlying their vertical distribution were mainly introduced here. There were three mechanisms driving the δ13C vertical distribution in soil profile: 1) historical changes of vegetation δ13C value, 2) changes of C3-C4 species dominance in plant communities, 3) accumulation of 13C-enriched microbial-derived carbon during decomposition. The effects of 13C Suess effect on the vertical distribution of δ13C in soil profile were also discussed. There were four mechanisms underlying the vertical distribution of δ15N in soil profile: 1) 15N-depletion gas loss during denitrification, 2) accumulation of 15N-enriched microbial-derived nitrogen during decomposition, 3) accumulation of 15N-encriched mycorrhizal fungi residues in deep soil as a result of transferring 15N-depleted nitrogen compounds to plants by mycorrhizae, 4) intera-ction between soil organic matter and mineral substance. We proposed important concerning points for the future study on vertical distribution of natural abundance of stable carbon and nitrogen isotopes in soil profile.

Key words: soil profile, carbon stable isotope, nitrogen stable isotope, isotopic fractionation, vertical distribution