湖泊温室气体产排特征及通量监测方法综述
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中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室

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国家自然科学基金 (42107340和42225103)


Greenhouse gas production and emission characteristics and flux monitoring methods of different lake ecosystems
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Key Laboratory of Ecosytem Network Observation and Modeling,Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences

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    摘要:

    湖泊温室气体(CO2和CH4)排放研究对了解全球变化和碳循环具有重要意义。湖泊的空间分布广泛,性质复杂,温室气体排放具有明显的时空异质性。本文总结了全球不同地区277个湖泊温室气体的排放特征,对比分析了湖泊温室气体的排放途径、产生和消耗机制、监测方法及主要影响因子。结果表明,湖泊CO2排放通量范围为-15.92 mmol·m-2·d-1到245.30 mmol·m-2·d-1,CH4排放通量范围为4.38×10-4 mmol·m-2·d-1到11.00 mmol·m-2·d-1。海拔、湖泊盐度、面积、深度和营养水平均对湖泊温室气体的排放有显著影响,其产生过程主要是由微生物驱动的碳转化过程,并通过扩散、冒泡和植物传输三种主要途径排放至大气。环境因子通过影响微生物碳转化过程的底物、反应温度和反应活性,温室气体排放途径,观测过程等影响湖泊温室气体排放通量。当前研究的监测体系和方法不同导致排放通量结果的可比性相对较差;温室气体产生、排放和转化的微观机制也还不够深入。因此,未来应完善温室气体通量观测方法学体系,加强宏观通量与微生物驱动的微观转化机制探索,结合人工智能模型,开展系统的湖泊温室气体产排研究。

    Abstract:

    As the vital component of inland water bodies, lakes are hotspots for greenhouse gas (GHG), specifically carbon dioxide and methane (CO2 and CH4) emissions, and the carbon cycles, contributing significantly to global carbon budget. However, lakes are widespread and exhibit complex ecological characteristics. The complex carbon cycling process within lake systems, coupled with numerous influencing factors under the global changes, demonstrating pronounced spatial and temporal heterogeneity in CO2 and CH4 emission fluxes, leading to large uncertainties in estimation of lake CO2 and CH4 emission fluxes. The study of lake CO2 and CH4 emission patterns and the driving mechanisms is crucial for advancing our understanding of global carbon budget estimation and the role of lake in global carbon cycle. This work synthesized the emission characteristics of CO2 and CH4 from 277 lakes across various global regions and provided a comparative analysis of emission pathways, production and consumption mechanisms, monitoring methods, and the key influencing factors. The results indicated that CO2 emission fluxes ranged from -15.92 mmol·m-2·d-1 to 245.30 mmol·m-2·d-1, while CH4 fluxes ranged from 4.38×10-4 mmol·m-2·d-1 to 11.00 mmol·m-2·d-1. The CO2 and CH4 fluxes exhibited distinct characteristics according to their geographical location and physicochemical properties. Thus, we categorized the lakes included in this study based on elevation, salinity, surface area, water depth, and the trophic statues. The results suggested these lake characteristics significantly influenced CO2 and CH4 emissions, which primarily produced by microbial-driven carbon transformation processes. Furthermore, these lake factors are closely coupled with other hydrological factors, resulting in complex synergistic effects. They influenced the processes of gas production, consumption, and emission within lakes, thereby affecting the CO2 and CH4 emission fluxes from lakes. The primary pathways of CO2 and CH4 emission from lakes include: diffusion, bubbling, and transport by plants. Environmental factors modulated CO2 and CH4 emission fluxes by affecting substrate availability, reaction temperature, and the activity of microbial carbon transformation processes, as well as the chosen monitoring methods. The heterogeneity in monitoring systems and methodologies used in current research led to challenges in the comparability of emission flux data. Additionally, the complex mechanisms underlying CO2 and CH4 production, emission, and transformation in lakes remained inadequately explored. Therefore, future studies should focus on enhancing methodological frameworks for CO2 and CH4 flux observation, investigating the mechanisms of microbially driven transformations, and exploring deeper relationships between GHG fluxes and these carbon transformation processes in lakes. The results will contributing foundational data for artificial intelligence modeling and providing scientific supports for accurate estimation of the global carbon budgets.

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吴 凡,黎佳佳,哈咸瑞,高 扬.湖泊温室气体产排特征及通量监测方法综述.生态学报,,(). http://dx. doi. org/[doi]

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