基和二氧化的气相结合率
Andrew K Mollner1, Sivakumaran Valluvadasan, Lin Feng
1Arthur Amos Noyes Laboratory of Chemical Physics, Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA.
形成酸 (HONO(2) 的反应对大气化学至关重要. 新的测量提供了更精确的速率常数,影响了洛杉矶等受污染地区的臭氧预测.
科学领域:
- 大气化学 大气化学
- 环境科学 环境科学
背景情况:
- 基基 (OH) 和二氧化 (NO2) 的反应形成气态酸 (HONO2) 是大气化学中的一个关键过程.
- 之前对HONO2形成速率系数的测量存在不确定性,特别是在热层条件下 (760 torr) 和由于产生过氧酸 (HOONO) 的二次通道.
研究的目的:
- 在相关大气条件下准确确定HONO2形成的速率系数.
- 要量化HONO2形成通道和HOONO形成通道之间的分区.
主要方法:
- 利用两种灵敏的激光谱技术,同时测量整体反应速率和分支比率.
- 在25°C和760 torr的气温下进行实验,以模拟热层条件.
主要成果:
- 获得了HONO2形成的显著更精确的速率常数:9.2 (±0.4) × 10^-12 cm^3分子^-1 s^-1 在760 torr.
- 新的速率常数低于之前报告的值,这表明该道的贡献比一些估计要少.
- 该研究量化了两个反应通道之间的分区.
结论:
- 对HONO2形成的修订速度常数为大气模型提供了更准确的参数.
- 这些发现表明了这种改进的动力数据对光化学模型预测的影响,特别是对洛杉矶等城市空气流域的臭氧度的影响.
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