陆地溶解有机物输入影响FT-ICR MS揭示的氧化排放
Zezheng Wang1, Lu Li1, Chengchao Liao1
1State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China; University of Chinese Academy of Sciences, Beijing 100049, China.
The Science of the total environment
|November 29, 2024
概括
陆地溶解有机物 (DOM) 侵入显著影响湖泊氧化 (N2O) 排放,主要是通过脱. 可生物降解的DOM成分,特别是来自人为来源的DOM,加速N2O生产,影响温室气体监管.
科学领域:
- 环境科学 环境科学
- 生物地质化学生物地质化学
- 微生物生态学 微生物生态学
背景情况:
- 湖泊中氧化 (N2O) 的排放受到陆地有机物输入的影响.
- 溶解有机物 (DOM) 影响N2O排放的具体机制尚不清楚.
研究的目的:
- 调查不同陆地DOM来源 (人为,自然,表面下水) 如何影响N2O排放.
- 阐明推动这些变化的生物地质化学和微生物机制.
- 评估DOM生物利用性在N2O生产中的作用.
主要方法:
- 使用吸收光谱学,激发发射矩阵光学和里埃转换离子循环子共振质谱法对DOM进行表征.
- 微生物分析以确定关键的微生物通路.
- 模拟不同的陆地DOM输入,以评估N2O的排放变化.
主要成果:
- 陆地DOM主要通过脱化影响N2O排放,影响narG和nirK+S基因丰度.
- 沉积物中的可生物降解DOM成分直接增加N2O排放.
- 水生系统中的不稳定DOM成分会被代谢成不太反应的形式,而类似人为蛋白质的DOM会迅速增加N2O的产生.
- 沉积物中的微生物调节的碳和代谢会对N2O流量产生负面影响.
结论:
- DOM生物可用性是控制湖泊N2O排放的一个关键因素.
- 人类DOM来源可以显著加快N2O生产.
- 了解这些过程对于管理水生生态系统的温室气体排放至关重要.
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