在北极大气中追踪NOx的起源和命运,使用酸盐中的稳定同位素
Samuel Morin1, Joël Savarino, Markus M Frey
1CNRS, Institut National des Sciences de l'Univers, France. samuel.morin@ujf-grenoble.fr
概括
北极大气中的酸盐源于春季的雪地排放. 氧化物局部氧化氧化物 (NOx),显著影响酸盐预算和大气化学.
科学领域:
- 大气中的化学成分
- 同位素地质化学 同位素地质化学
- 北极环境科学 北极环境科学
背景情况:
- 氧化 (NOx) 对反应性循环和大气氧化能力至关重要.
- 酸盐沉积是活性循环的关键组成部分.
- 了解氧化和酸盐的来源和转化对于大气研究至关重要.
研究的目的:
- 研究大气氧化 (NOx) 和北极酸盐的季节性起源和命运.
- 为了利用酸盐中和氧的稳定同位素比,用于来源归因.
- 为了限制大气氧化剂在酸盐形成中的作用.
主要方法:
- 从北极大气层收集和分析酸盐样本.
- 在酸盐中测量和氧稳定同位素比率 (15N/14N和18O/16O).
- 应用同位素分析来推断NOx和酸盐的来源和转化途径.
主要成果:
- 在春季,来自雪盖的光化学驱动的反应性排放大大增加了大气中的NOx.
- 氧化物对NOx的局部氧化成为北极春季酸盐形成的主要途径.
- 酸盐的同位素成分为大气氧化剂的相对重要性提供了强大的约束.
结论:
- 该研究阐明了北极大气中酸盐形成的主要途径,特别是在春季.
- 以氧化物为媒介的NOx氧化被确定为影响北极酸盐预算的关键过程.
- 亚酸盐的同位素分析为重建过去的大气条件和氧化剂状态提供了强大的工具.
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