了解C动力学:局部碳循环对同位素不平衡和储停留时间的影响
Sabyasachi Rout1, Sonali Yadav1, Vandana Pulhani1
1Bhabha Atomic Research Centre, Mumbai, India; Homi Bhabha National Institute, Mumbai, India.
The Science of the total environment
|November 9, 2025
概括
放射性碳 (C) 的动态因生态系统而异. 红树林释放现代碳,而内陆地区则出口老化碳,影响当地大气碳预算.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 通过放射性碳测年法进行测年.
背景情况:
- 了解各种碳储库中的放射性碳 (C) 动态对于准确的碳循环和来源归因至关重要.
- 受到水库年龄和碳循环影响的局部14C变化是不太了解的.
研究的目的:
- 在对比的生态系统中调查大气,陆地和水中水库的14C空间变化.
- 估计异流量并推导碳循环动态,以评估储库作为碳来源或沉积点.
主要方法:
- 加速器质谱 (AMS) 用于C分析.
- 与大气相对的异流估计.
- 碳循环动态的平稳状态建模.
主要成果:
- 红树林的叶子显示有丰富的14C和正异流,表明现代的碳固定和大气Δ14CO2.2的调制.
- 沿海沉积物和土壤呈现负Δ14C和高异流量,这表明老化/化石碳出口和陆地与海洋的合.
- 内陆水库的负同流量,循环速度较慢,碳排放时间较长,与红树林有很大不同.
结论:
- 14C动态是高度水库和特定位置的,影响当地的大气14C预算.
- 红树林充当现代碳的热点,而内陆生态系统则出口老化的碳.
- 碳循环的异质性挑战了稳定状态模型在过渡条件下的适用性.
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