微尺度的动力学促进了藻聚合物的分离脱,这些聚合物在大量含氧海水中慢慢沉没
Davide Ciccarese1, Omar Tantawi2, Irene H Zhang1,3
1Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA USA.
概括
海洋颗粒脱,对于碳捕获至关重要,发生在含氧水中. 缓慢沉没的藻聚合物产生无氧微站点,使这种无氧过程即使在粒子表面附近也可行.
科学领域:
- 海洋微生物生态学
- 生物地质化学循环是什么
- 海洋的碳捕获 海洋的碳捕获
背景情况:
- 沉没的海洋颗粒是生物的关键,封存大气中的碳.
- 颗粒上的细菌群体表现出高代谢活性,但脱的开始仍不清楚.
研究的目的:
- 研究海洋聚合物的脱机制.
- 确定与颗粒相关的氧化水中是否可以发生脱.
主要方法:
- 海洋藻聚合物的实验化.
- 微氧分析和基于光的细菌活动测定.
- 分析完整的与破碎的藻作为有机物质来源.
主要成果:
- 在缓慢沉没的藻聚合物中,在无氧微站内观察到活性脱.
- 脱发生在粒子边界附近,甚至在大量含氧水中.
- 缓慢泄漏的藻细胞促进了细菌的生长,减少了粒子氧,并增强了脱.
结论:
- 海洋聚合物可以在周围有氧化的条件下保持活跃的脱.
- 聚合物的物理结构和有机物质可变性会影响脱率.
- 了解这些过程对于准确建模海洋生物碳至关重要.
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