现代类似的氨流从陆地热水特征到阿克海大气层的氨流
1Physical and Environmental Sciences Department, Center for Water Supply Studies, Texas A&M University - Corpus Christi, Corpus Christi, USA. joseph.felix@tamucc.edu.
Scientific reports
|January 17, 2024
概括
早期地球上的热水特征可能通过氨水空气流提供了大量的生物可利用. 这一过程为前坎布里亚时期的循环提供了新的视角,补充了其他固定途径.
科学领域:
- 地质化学 地质化学
- 早期地球的条件.
- 生物地质化学循环是什么
背景情况:
- 岩石中的同位素比率 (δ15N) 提供了早期地球反应性源的线索.
- 之前对高δ15N值的解释包括化和古古中的氨-氨平衡.
- 在现代水生系统中,水空气流受到温度的影响,而不仅仅是性pH值.
研究的目的:
- 为了研究水-空气氨 (NH) 流从热水特征作为固定的来源在早期地球上的作用.
- 评估这种流量对早期地球气预算的定量贡献.
主要方法:
- 从1022个现代热水特征中分析化学和物理成分.
- 基于热水特征数据的氨 (NH3) 流速的建模.
- 模拟流量与现代生物固速率的比较.
主要成果:
- 从热水特征的模拟平均NH3流量为2.1公斤N m-2年-1 (1.2公斤N m-2年-1年不包括异常值).
- 如果水热特征仅占古地球表面的0.0092%至0.017%,这种流动可能与现代生物固相匹配.
- 来自陆地热水系统的水空气NH流被确定为一个重要的源.
结论:
- 陆地热水特征可能在为早期生命提供可生物利用的方面发挥了关键作用.
- 通过水空气流的氨 (NH3) 挥发是早期地球循环的一个可行的机制.
- 这种机制有助于解决解释早期前剑桥时期同位素数据的模两可.
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