解读溶解有机物特性及其在冰川养的沙漠河 - - 中国塔林河 - - 的命运
Yufu Han1, Yulin Qi2, Jun Zhong1
1Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin, China.
Environmental research
|May 30, 2024
概括
塔林河中的冰川融水溶解有机物 (DOM) 呈现出明显的下游分子变化,陆地输入增加了类似的化合物. 这突显了冰川来源的DOM在干旱的阿尔卑斯山地区的命运.
科学领域:
- 环境化学环境化学
- 地质化学 地质化学
- 水文学的水文学
背景情况:
- 从冰川融水中溶解的有机物 (DOM) 对山区的碳循环至关重要.
- 在冰川养的沙漠河流中,了解河流DOM的分子特征和命运是有限的.
研究的目的:
- 为了研究DOM在塔林河流域的光学和分子特性.
- 确定DOM从支流到下游的变化和来源,在一个高山干旱地区.
主要方法:
- 使用光谱技术 (EEM-PARAFAC) 来分析DOM组件.
- 高分辨率质谱学揭示了DOM的分子组成.
- 支流和下游样本之间的DOM特征的比较.
主要成果:
- 下游溶解有机碳 (DOC) 度高于支流,但在全球范围内相当.
- 附属样本主要由类似蛋白质的DOM占据主导地位,而下游样本显示出更多类似的成分.
- 下游运输增加了更高的分子量,芳香化合物,包括多环芳香化合物和多化合物,表明陆地输入.
结论:
- 来自冰川的DOM在阿尔卑斯山干旱河流系统的过境过程中经历了重大变化.
- 陆地输入在下游塑造DOM签名方面发挥着重要作用,稀释了冰川信号.
- 这个地区的冰川来源的DOM经历了有限的光降解和人类影响,陆地输入是主要的修饰因素.
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