在北大西洋和北太平洋的寡合性海洋中溶解和合性铁
1Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. jingfeng@mit.edu
概括
超过显示海洋中的可溶性铁和配体比以前认为的要低. 这种铁的大部分是合体,影响了植物浮游生物的生物可用性和海洋铁循环模型.
科学领域:
- 海洋化学 海洋化学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 之前对之前估计的估计.
研究的目的:
- 研究铁在寡质海洋中的真正度和物种化.
- 澄清铁对植物浮游生物的生物利用性.
- 改进海洋铁循环模型.
主要方法:
- 超过技术用于分离可溶和合物分离物.
- 分析铁和结合铁的有机连接物度.
- 铁的尺寸分数分布与营养成分的比较.
主要成果:
- 溶性铁和带的含量明显低于之前定义的含量.
结论:
- 大量的海洋铁存在于体尺寸范围内.
- 体铁的动态,包括聚合和沉积,对于海洋铁循环至关重要.
- 根据新的尺寸分离数据,对植物浮游生物的铁生物可用性进行重新评估是必要的.
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