基可以在微滴的空气-水界面自发形成吗? 一个喷雾电离式质谱学研究
1Department of Chemistry, Graduate School of Science and Technology, University of Tsukuba, Tsukuba 305-8571, Japan.
The journal of physical chemistry letters
|October 30, 2025
概括
基基 (OH) 在微滴的空气-水界面上不会自发形成. 使用酸作为清除剂的实验只在外部供应时确认OH的存在,而不是自产.
科学领域:
- 环境化学环境化学
- 大气化学 大气化学
- 物理化学 物理化学
背景情况:
- 基基 (OH) 是大气化学中的关键氧化剂.
- 之前的研究表明,在空气-水接口 (AWI) 上可能会形成水性微滴.
- 研究界面反应对于理解大气过程至关重要.
研究的目的:
- 为了确定基 (OH) 是否在水性微滴的空气-水界面 (AWI) 自发形成.
- 在实验条件下量化自发形成的OH的潜在度.
主要方法:
- 使用喷雾电离质谱法 (SIMS) 来分析微滴.
- 使用酸 (BA-) 作为基根清除剂.
- 通过检测基酸 (基BA-) 形成,确认OH的存在.
- 使用DMSO作为替代OH清理剂.
主要成果:
- 在气态OH存在时检测到氧-BA-信号.
- 在没有外部OH的微滴中没有观察到氧-BA-信号.
- 使用FeCl2/H2O2的实验在已知的OH生成条件下证实了氧-BA-形成.
- 单独使用FeCl2的实验没有产生氧-BA-.
- 使用DMSO清除器,没有发现自发形成OH的证据.
- 自发OH度的上限被确定为大约0.2μM.
结论:
- 在研究条件下,基 (OH) 在水性微滴的空气-水界面 (AWI) 上不会自发形成.
- 在AWI的OH存在需要外部源.
- 确定了自发OH度的上限,为大气模型提供了有价值的数据.
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