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Carbon gain in upper but loss in deeper cropland soils across China over the last four decades

文献类型： 外文期刊

作者： Zhou, Zhenghu 1 ; Wang, Chuankuan 1 ; Li, Yu'e 3 ; Wang, Xuhui 4 ; He, Xinhua 5 ; Xu, Minggang 8 ; Cai, Andong 3 ;

作者机构： 1.Northeast Forestry Univ, Sch Ecol, Harbin 150040, Peoples R China

2.Northeast Forestry Univ, Northeast Asia Biodivers Res Ctr, Harbin 150040, Peoples R China

3.Chinese Acad Agr Sci, Inst Environm & Sustainable Dev Agr, Beijing 100081, Peoples R China

4.Peking Univ, Inst Carbon Neutral, Sino French Inst Earth Syst Sci, Coll Urban & Environm Sci, Beijing 100871, Peoples R China

5.Shanxi Agr Univ, Inst Ecoenvironm & Ind Technol, Taiyuan 030031, Peoples R China

6.Univ Western Australia, Sch Biol Sci, Perth, WA 6009, Australia

7.Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA

8.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, State Key Lab Efficient Utilizat Arid & Semiarid A, Beijing 100081, Peoples R China

关键词： soil organic carbon; soil profile; carbon inputs; climate change; resampling

期刊名称：PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA （ 影响因子：9.1； 五年影响因子：10.6 ）

ISSN： 0027-8424

年卷期： 2025 年 122 卷 1 期

页码：

收录情况： SCI

摘要： Increasing soil organic carbon (SOC) in agricultural systems is a primary nature- based option for mitigating climate change, improving soil fertility, and ensuring food security. However, the consequences of global warming and increases in carbon inputs on cropland SOC stocks over the last few decades remain largely unknown, particularly in deeper soil layers. Here, by using repeated measurements, we reassess variations in SOC stocks across a 0 to 100 cm soil profile at the same locations in China's upland croplands in 1980 and 2023. We observe an overall net accumulation of 0.74 Pg SOC (7%) with a mean sequestration rate of 13.7 g SOC m-2 y-1. This accumulation results from 0.86 Pg SOC gains at upper soil depths (0 to 60 cm) induced by carbon inputs, alongside 0.12 Pg SOC losses at deeper soil layers (60 to 100 cm) prompted by warming- enhanced decomposition. While our findings indicate a successful, though lower than expected, increase in overall net SOC stocks, the loss of more recalcitrant deeper SOC warrants further consideration of its effects on enhancing cropland SOC accumulation to achieve carbon neutrality over the long term.

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