Department of Earth & Environmental Science, Xi'an Jiaotong University, Xi'an, Shaanxi Province 710049, China; Key Laboratory of Degraded and Unused Land Consolidation Engineering, The Ministry of Natural Resources of China, Xi'an, Shaanxi Province 710075, China.
Department of Earth & Environmental Science, Xi'an Jiaotong University, Xi'an, Shaanxi Province 710049, China; Technology Innovation Center for Land Engineering and Human Settlements, Shaanxi Land Engineering Construction Group Co. Ltd and Xi'an Jiaotong University, Xi'an, Shaanxi Province 710115, China.
Sci Total Environ. 2022 Sep 1;837:155469. doi: 10.1016/j.scitotenv.2022.155469. Epub 2022 May 4.
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 yr during the 70 years following afforestation, and that SOC could decline thereafter (-8.89 g C m yr), 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.
土壤有机碳(SOC)储量的动态变化是影响气候的一个重要因素,而生态恢复是通过增强植被和土壤碳储量来减缓气候变化的一种潜在有效措施,从而抵消温室气体排放。自 1999 年以来,中国黄土高原(LP)实施的退耕还林还草工程(GFGP)是世界上最大的生态恢复项目之一。然而,生态恢复和气候变化对生态系统土壤碳固存的贡献仍不清楚。在本研究中,我们通过优化基于 SOC 全空间模拟的初始 SOC 储量,改进了土壤碳分解框架,并纳入了激发效应,以调查 1982 年至 2017 年期间 LP GFGP 地区的 SOC 动态变化。结果表明,1982 年至 2017 年期间,GFGP 地区的 SOC 储量增加了 20.18 Tg C。大部分 SOC 增加(15.83 Tg C)发生在 GFGP 启动时,由于植被恢复形成了一个 SOC 汇,碳吸收量为 16.12 Tg C,而在此期间由于气候变暖导致碳损失 0.29 Tg C。SOC 与森林冠层高度之间的关系以及造林后 SOC 动态的研究表明,造林后 70 年内 SOC 的积累率可达 24.68 g C m yr,此后 SOC 可能会下降(-8.89 g C m yr),这主要是由于气候变暖所致。本研究提供了一种量化生态恢复对 SOC 变化贡献的新方法,并提醒人们注意未来气候变暖可能导致 LP 成熟森林土壤 SOC 损失的潜在风险。