从气相到谷物边界的过氧化吸收:雪和冰中的来源
Angela C Hong1, Thomas Ulrich2, Erik S Thomson3
1Department of Chemistry, University of Toronto, Toronto, Ontario M5S 3H6, Canada.
Environmental science & technology
|July 27, 2023
概括
这项研究表明,过氧化 (H2O2) 通过扩散从大气中轻易进入雪粒边界. 这种以前未知的途径显著增强了H2O2转移到极地雪,影响大气化学.
科学领域:
- 大气化学 大气化学
- 环境科学 环境科学
- 物理化学 物理化学
背景情况:
- 过氧化 (H2O2) 是一种关键的大气氧化剂,影响气相反应和硫酸盐形成.
- 之前的实验室研究表明,冰粒边界内有H2O2.2的加速氧化.
- 进入雪粒边界的H2O2的机制和程度仍然不清楚.
研究的目的:
- 提供第一个从气相向冰粒边界扩散吸收过氧化的实验证据.
- 测量H2O2在冰面上的吸附量.
- 为了确定谷物边界吸收与表面吸附对H2O2转移到雪的意义.
主要方法:
- 开发和利用一种新型流动反应堆系统,采用钻孔的冰流管.
- 在235258 K的温度范围内对H2O2吸附和扩散吸收的实验测量.
- 来自冰面吸附和粒度边界扩散的H2O2吸收贡献的分离.
主要成果:
- 实验证实了气态过氧化在冰粒边界的直接扩散吸收.
- 在冰面上吸附H2O2的量化.
- 证明谷物边界扩散吸收是H2O2转移到雪中的重要途径,特别是在极地相关温度下.
结论:
- 扩散吸收到谷物边界是大气过氧化转移到雪的新和重要的机制.
- 这一过程比以前认为的更为明显,特别是在极地环境中.
- 这种机制有助于在雪粒边界内的反应性杂质储以非酸性微量气体填充.
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