植物生态学报

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大气CO2浓度升高和增温对土壤有机碳库积累、分子组成和结构的稳定性影响

范亚冉1,夏少攀1,于冰冰1,朱紫琪1,李强2,杨威3,范豫川4,刘晓雨1,张旭辉1,郑聚锋1   

  1. 1. 南京农业大学
    2. 天津师范大学
    3. 内蒙古农业大学
    4. 佛罗里达大学
  • 收稿日期:2024-10-21 修回日期:2025-01-18 发布日期:2025-02-26

The effects of elevated atmospheric CO2 concentration and warming on stability of soil organic carbon pool accumulation, molecular composition and structure

亚冉 范1,Shao-pan Xia2,冰冰 于1,Ziqi Zhu1,Qiang Li3,Wei Yang4,Yuchuan Fan5,Xiaoyu Liu1,Xuhui Zhang1,Jufeng Zheng1   

  1. 1. Nanjing Agricultural University
    2.
    3. Tianjin Normal University
    4. Inner Mongolia Agricultural University
    5. University of Florida-IFAS, Gainesville
  • Received:2024-10-21 Revised:2025-01-18

摘要: 在固碳减排和“双碳”目标的背景下,以大气CO2浓度增加和温度升高协同作用为特征的气候变化对土壤有机碳(SOC)动态变化的影响成为当前的研究热点,气候变化与SOC库之间的相互作用及耦合机制一直是学术界研究的难点问题。以往大多数研究从植物生长、凋落物基质质量、土壤理化性质、有机碳物理/化学组分和微生物群落结构等层面考察气候变化对SOC库改变的驱动过程及作用机理,而且关于气候变化对陆地生态系统碳过程的研究仍然是基于CO2浓度增加或温度升高单一因素。结合国内外研究进展,本文在论述CO2浓度升高和增温对土壤有机碳库积累的影响及机制基础上,从土壤有机碳组分、分子组成、结构特征、表层与底层响应差异与有机碳稳定性的耦合效应方面,揭示CO2浓度升高和增温对SOC积累和转化的内在机制。在此基础上,未来研究中应着重关注(1)明晰SOC端元输入-分子组成-结构特征耦合关系,(2)揭示长期气候变化对多生态系统SOC稳定性和埋藏潜力的影响机制。理清土壤碳源/汇功能,必须全面深入了解气候变化下陆地生态系统土壤有机碳来源、转化、埋藏和分解的生物地球化学循环过程,旨在为将来土壤碳中和管理决策提供科学的理论依据。

关键词: 气候变化, 土壤有机碳, 分子组成与结构, 稳定性, 深层土壤, 热点关键词知识图谱

Abstract: In the context of carbon sequestration and emission reduction and the "Dual Carbon" goals, currently, the impact of climate change, characterized by the combined changes of elevated atmospheric carbon dioxide (CO2) concentration and warming, on the dynamic changes of soil organic carbon (SOC) has become a research hotspot. The interaction and coupling mechanism between climate change and SOC pools have always been a difficult issue in academic research. Most previous studies have examined the driving processes and mechanisms of climate change on SOC pool changes from the perspectives of plant growth, litter substrate quality, soil physicochemical properties, organic carbon physical/chemical components, and microbial community structure. Moreover, research on the impact of climate change on terrestrial ecosystem carbon processes is still based on a single factor of elevated CO2 concentration or warming. Based on the research progress at home and abroad, this review summarizes the effect and mechanism of elevated CO2 concentration and warming on soil organic carbon accumulation. We combine the coupling effects of soil organic carbon fractions, molecular composition, structural characteristic, differences in response between topsoil and subsoil, and organic carbon stability, so as to reveal the intrinsic mechanism of elevated CO2 concentration and warming on organic carbon accumulation and transformation. On this basis, future research should focus on (1) clarifying the coupling relationship between SOC end inputs, molecular composition, as well as structural characteristic, and (2) revealing the impact mechanism of long-term climate change on the stability and burial potential of SOC in multiple ecosystems. To clarify soil carbon source/sink functions, it is necessary to comprehensively and deeply understand the biogeochemical processes of SOC sources, transformation, burial, and decomposition in terrestrial ecosystems under climate change, aiming to provide scientific theoretical basis for soil carbon neutrality management decisions in the future.

Key words: climate change, soil organic carbon, molecular composition and structure, stability, subsoil, knowledge map of hot keywords