铁化肥对南大洋碳封存的影响
Ken O Buesseler1, John E Andrews, Steven M Pike
1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. kbuesseler@whoi.edu
概括
将铁添加到南大洋增加了碳出口,但与自然开花相比,这种效果很小,对于全球碳预算或地球工程努力来说并不重要.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 铁化肥对海洋碳捕获的影响仍然是气候科学中的一个关键问题.
- 了解南大洋在全球碳循环中的作用至关重要.
研究的目的:
- 调查表面海洋铁输入的变化是否会影响到深海的碳流.
- 量化铁化肥对南大洋颗粒碳出口的影响.
主要方法:
- 进行了南洋铁实验 (SOFeX).
- 从表面混合层测量颗粒碳流量.
- 在实验补丁下面分析了粒子循环.
主要成果:
- 在铁肥后观察到颗粒碳流量的增加.
- 在受精区域下方检测到粒子循环的变化.
- 碳流量大小与南大洋自然开花相比较.
结论:
- 铁化肥可以提高碳出口,但其影响是温和的.
- 观察到的碳流是不足以显著的全球碳封存或大规模地质工程.
- 需要进一步的研究才能充分理解铁在海洋碳循环中的作用.
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