在过去30年中,中国内陆水域的溶解碳储存和流动动态
Shuoyue Wang1,2,3, Gaboury Benoit3, Peter A Raymond3
1Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
National science review
|July 11, 2025
概括
中国中国中国中国.
科学领域:
- 环境科学 环境科学
- 气候变化研究 气候变化研究
- 碳循环研究 碳循环研究
背景情况:
- 内陆水域是全球气候和碳循环的关键调节者.
- 中国的内陆水域对区域碳预算有很大的影响.
- 这些系统中溶解碳动态的长期数据有限.
研究的目的:
- 检查中国内陆水域三十年来溶解碳 (DC) 储存和流动的时空模式.
- 确定DC动态变化的关键驱动因素.
- 评估内陆水域在全球碳循环中的作用.
主要方法:
- 湖泊和水库溶解碳储存的分析.
- 在过去的30年里,河流溶解的碳流量量化.
- 统计分析以确定气候,人为因素和水化学的影响.
主要成果:
- 中国的内陆水溶解碳储量从96兆克 (上世纪90年代) 增加到142兆克 (2010年代).
- 河流溶解的碳流保持稳定,约为每年13.2 Tg C.
- 河流溶解碳主要是由气候和人类活动 (> 50%) 驱动的,而湖泊和水库则受到水化学的影响 (> 70%).
结论:
- 气候变化,人类活动和水化学共同影响内陆水的碳动态.
- 溶解无机碳度通过水化学 (EC,pH) 与气候有关.
- 溶解有机碳度受气候和营养状况的影响,突出了内陆水域在全球碳预算中的关键作用.
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