增加大气中的CO2和碳在陆地生态系统中的运输时间
Estefanía Muñoz1, Ingrid Chanca1,2, Carlos A Sierra1
1Theoretical Ecosystem Ecology Group, Max Planck Institute for Biogeochemistry, Jena, Germany.
Global change biology
|October 5, 2023
概括
了解生态系统如何储存碳是关键. 这项研究建议使用碳过渡时间分布来跟踪新吸收的碳,揭示大多数是一年内呼吸,影响气候变化模型.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 气候科学 气候科学
背景情况:
- 陆地生态系统对大气中二氧化碳 (CO2) 升高的反应尚不清楚.
- 以前的森林实验显示了对二氧化碳影响的相互矛盾的结果.
- 由于二氧化碳增加,由于二氧化碳增加而同化碳的长期命运存在不确定性.
研究的目的:
- 为了解决生态系统在高二氧化碳水平下储存额外碳的数量和时间的不确定性.
- 介绍和证明碳转运时间分布 (TTD) 的实用性,以量化碳命运.
- 分析陆地生态系统中碳循环的时间尺度.
主要方法:
- 使用碳转运时间分布 (TTD) 的概念.
- 应用TTD来分析跨生态系统部分的碳运动.
- 作为一个案例研究,研究热带森林中的TTD.
主要成果:
- 该研究表明,TTD如何评估新吸收的碳的命运和时间表.
- 对热带森林TTD的分析表明,大多数固定碳 (60%) 在一年内被呼吸.
- 这表明,在高CO2下,新碳可能会遵循类似的快速呼吸途径.
结论:
- 碳过渡时间分布是量化生态系统对二氧化碳增加反应的关键概念.
- 在热带森林的例子中,大多数新吸收的碳都被快速循环.
- 进一步的研究应该更频繁地采用TTD,以解决在二氧化碳上升下碳捕获的不确定性.
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