人为来源和液态水驱动在喜马拉雅东部的二次有机气溶形成
Dhananjay Kumar1, Prashant Hegde1, B S Arun2
1Space Physics Laboratory, Vikram Sarabhai Space Centre, Thiruvananthapuram 695022, India.
The Science of the total environment
|July 31, 2024
概括
喜马拉雅山脉的有机气溶主要是加工的,是人为的,氧酸占主导地位. 气溶液体水通过水相过程驱动二次有机气溶的形成.
科学领域:
- 大气化学和气候科学.
- 气溶科学与空气污染.
背景情况:
- 大气中的气溶显著影响喜马拉雅辐射平衡.
- 在喜马拉雅山脉的有机气溶 (OA) 了解甚少,阻碍了气候影响评估.
研究的目的:
- 研究在喜马拉雅山东部水溶性OA的起源和形成.
- 阐明气溶液体水 (ALW) 在二次有机气溶 (SOA) 形成中的作用.
主要方法:
- 来自喜马拉雅山东拉的PM10样本的分析 (2019年3月至5月).
- 利用逆向空气质量轨迹和有机痕迹分析.
- 使用了气溶液体水 (ALW) 的热力学预测.
主要成果:
- 酸 (C2) 主导水溶性OA,表明大气处理.
- 证据表明OA的人类起源与远程运输.
- ALW与硫酸盐和水溶性有机物正相关.
- 氧化酸和预测的ALW之间的强烈正相关性通过水性光化学证实了SOA的形成.
结论:
- 在喜马拉雅山东部,水溶性OA来源于人为来源,并经历了重要的大气处理.
- 气溶液体水在该地区通过水相光化学过程在二次有机气溶形成中发挥着至关重要的作用.
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