Climate-management interactions drive soil organic carbon sequestration potential in China's croplands during 2020–2060

Wenfang Jiang , Ziqi Lin , Zhangcai Qin , Xinqing Lu , Wen Zhang , Qing Zhang , Sijing Ye , Huirong Li , Huilin Ge , Guocheng Wang
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Abstract

Soil organic carbon (SOC) sequestration in croplands plays a vital role in mitigating climate change and enhancing soil fertility. As one of the world's leading agricultural nations, China's croplands exhibit highly representative climate types, soil conditions, crop varieties, and farming systems on a global scale. Despite extensive studies on SOC dynamics, the spatial variability of SOC sequestration potential remains insufficiently quantified across China's diverse agricultural regions, which adopt varying straw management practices. This study employs a process-based modeling approach to systematically assess the dynamics and sequestration potential of SOC in China's croplands (122 ​Mha) from 2020 to 2060. We found that by sustaining a moderate historical management during 2015–2020 (i.e., an average of ∼37% residue retention rate in addition to traditional root residue retention and farmyard manure application), China's croplands SOC stock is projected to increase by more than 25% by 2060, corresponding to total SOC sequestration of ∼ 1650 ​Tg ​C at the national scale. Regional variability exists, with southern China (e.g., east and central, south and central, and southwest regions) contributing to ∼84% of total SOC sequestration, while northeast region has minimal sequestration potential. Carbon inputs, temperature, and precipitation are positively correlated with SOC dynamics, while initial SOC density shows a negative partial correlation with changes in SOC. This study not only characterizes the dynamics of SOC in China's croplands over the next 40 years under different carbon management practices and climate change scenarios, but also presents the pathways for achieving sustainable carbon sequestration in future croplands. Our findings highlight the importance of sustaining and optimizing straw return practices, alongside region-specific strategies, to maximize SOC sequestration and support global climate mitigation goals.
气候管理相互作用对2020-2060年中国农田土壤有机碳固存潜力的影响
农田土壤有机碳的固存对减缓气候变化和提高土壤肥力具有重要作用。作为世界领先的农业国家之一,中国的农田在全球范围内表现出极具代表性的气候类型、土壤条件、作物品种和耕作制度。尽管对土壤有机碳动态进行了广泛的研究,但中国不同农区土壤有机碳固存潜力的空间变异性仍未得到充分量化。本研究采用基于过程的建模方法,系统评估了2020 - 2060年中国耕地(122mha)有机碳的动态和固碳潜力。我们发现,通过在2015-2020年期间保持适度的历史管理(即,除了传统的根渣保留和农家肥施用之外,平均残渣保留率为~ 37%),到2060年,中国的农田有机碳储量预计将增加25%以上,相当于在全国范围内总有机碳封存量为~ 1650 Tg C。存在区域差异,华南地区(如东部和中部、南部和中部以及西南地区)贡献了总有机碳固存的~ 84%,而东北地区的固存潜力最小。碳输入、温度和降水与有机碳动态呈正相关,而初始有机碳密度与有机碳变化呈负偏相关。本研究不仅分析了未来40年不同碳管理模式和气候变化情景下中国农田有机碳的动态特征,还提出了未来农田实现可持续碳固存的途径。我们的研究结果强调了维持和优化秸秆还田实践以及区域特定战略的重要性,以最大限度地提高有机碳封存和支持全球气候减缓目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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