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The Grain-for-Green project offsets warming-induced soil organic carbon loss and increases soil carbon stock in Chinese Loess Plateau

  • Huiwen Li
  • , Yiping Wu
  • , Shuguang Liu
  • , Wenzhi Zhao
  • , Jingfeng Xiao
  • , Leigh A. Winowiecki
  • , Tor Gunnar Vågen
  • , Jianchu Xu
  • , Xiaowei Yin
  • , Fan Wang
  • , Bellie Sivakumar
  • , Yue Cao
  • , Pengcheng Sun
  • , Guangchuang Zhang
  • Xi'an Jiaotong University
  • The Ministry of Natural Resources of China
  • Central South University of Forestry & Technology
  • CAS - Northwest Institute of Eco-Environment and Resources
  • University of New Hampshire
  • World Agroforestry Centre
  • CAS - Kunming Institute of Botany
  • Indian Institute of Technology Bombay
  • Xi'an Institute for Innovative Earth Environment Research
  • Ministry of Water Resources, P.R. China

科研成果: 期刊稿件文章同行评审

71 引用 (Scopus)

摘要

The dynamics of soil organic carbon (SOC) stock is a vital element affecting the climate, and ecological restoration is potentially an effective measure to mitigate climate change by enhancing vegetation and soil carbon stocks and thereby offsetting greenhouse gas emissions. The Grain-for-Green project (GFGP) implemented in Chinese Loess Plateau (LP) since 1999 is one of the largest ecological restoration projects in the world. However, the contributions of ecological restoration and climate change to ecosystem soil carbon sequestration are still unclear. In this study, we improved a soil carbon decomposition framework by optimizing the initial SOC stock based on full spatial simulation of SOC and incorporating the priming effect to investigate the SOC dynamics across the LP GFGP region from 1982 through 2017. Our results indicated that SOC stock in the GFGP region increased by 20.18 Tg C from 1982 through 2017. Most portion (15.83 Tg C) of the SOC increase was accumulated when the GFGP was initiated, with a SOC sink of 16.12 Tg C owing to revegetation restoration and a carbon loss of 0.29 Tg C due to warming during this period. The relationships between SOC and forest canopy height and investigations on the SOC dynamics after afforestation revealed that the accumulation rate of SOC could be as high as 24.68 g C m−2 yr−1 during the 70 years following afforestation, and that SOC could decline thereafter (−8.89 g C m−2 yr−1), which was mainly caused by warming. This study provides a new method for quantifying the contribution of ecological restoration to SOC changes, and also cautions the potential risk of LP SOC loss in the mature forest soil under future warming.

源语言英语
文章编号155469
期刊Science of the Total Environment
837
DOI
出版状态已出版 - 1 9月 2022

联合国可持续发展目标

此成果有助于实现下列可持续发展目标:

  1. 可持续发展目标 13 - 气候行动
    可持续发展目标 13 气候行动

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