NH3驱动的HONO生产作为在雪地覆盖和融化期间潜在的未知来源
Shengjin Xie1, Xuelei Zhang2, Aijun Xiu3
1State Key Laboratory of Black Soils Conservation and Utilization, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, 130102, China; State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Harbin, 150000, China; School of Environment, Harbin Institute of Technology, Harbin, 150000, China.
雪地覆盖显著增加酸 (HONO) 流量,特别是在融雪期间,作为中度的关键来源. 这项研究量化了冰层和大气之间的HONO交换.
科学领域:
- 大气化学 大气化学
- 环境科学 环境科学
- 地质物理学 地质物理学
背景情况:
- 雪地覆盖的高反射率和表面准液体层 (QLL) 促进酸 (HONO) 反应.
- 了解HONO来源和大气相互作用对于空气质量建模至关重要.
研究的目的:
- 更新CAMx模型以异质HONO反应,并模拟中国东北部的HONO流量.
- 调查季节性雪覆盖作为大气HONO的潜在来源的作用.
- 量化未知的HONO来源的贡献及其对OH,HO2和RO2基的影响.
主要方法:
- 将HONO的11种异质化学反应纳入CAMx模型.
- 在中国东北部进行了2024年3月的数值模拟.
- 建立了基于NH3,RH和未知的HONO来源的增强因子函数.
主要成果:
- 在雪融期,HONO流量达到峰值,超过积雪和无雪期.
- 中度的雪地表现出HONO流量,比极地地区高两倍.
- 在雪融期间,未知HONO来源的贡献很大 (高达19.78%),影响OH基度 (高达24.76%).
结论:
- 季节性雪地覆盖,特别是在中度地区,是大气HONO的重要潜在来源.
- 这项研究量化了HONO.HONO的冷层-大气流量交换.
- 揭示了季节性雪的HONO形成机制及其对大气氧化剂的影响.
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