压缩碳
Terry Plank1, Craig E Manning2
1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA. tplank@ldeo.columbia.edu.
Nature
|October 18, 2019
概括
地球有一个隐藏的碳循环, 每年有数百万的碳进入沉降区. 这一过程影响了大气中的二氧化碳和氧气水平,
科学领域:
- 地质化学
- 地球科学
- 火山学
背景情况:
- 每年大量的碳进入地球的降温区.
- 这种压缩的碳影响大气组成和地球的长期碳平衡.
- 了解缩碳的命运对于理解全球生物地化学循环至关重要.
研究的目的:
- 阐明碳在潜伏区内的运动和转化过程.
- 研究弧形火山排放的二氧化碳的来源和循环机制.
- 分析碳输入和重新调动的全球变异性.
主要方法:
- 对碳输送到潜水区的地质过程进行审查.
- 沉积碳转化为流体,岩石,火山气体和钻石的分析.
- 检查火山气体的组成及其与沉积物质的关系.
主要成果:
- 碳通过微化石,有机物和碳酸盐沉物进入沉降区.
- 火山二氧化碳排放主要来自回收的沉降材料.
- 碳的转化和释放在全球不同的降温区之间有很大差异.
结论:
- 潜伏区作为地球内隐藏的碳循环的关键管道.
- 在地球历史上,沉降碳的回收对大气中的二氧化碳和氧气水平产生了重大影响.
- 收边缘作为自然实验室来研究复杂的降温碳循环.
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