离子诱导气溶胶成核过程的研究

大气与环境光学学报 ›› 2016, Vol. 11 ›› Issue (2): 81-90.

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离子诱导气溶胶成核过程的研究

温作赢1,2,3，顾学军1,3，荣华1,3,4，朱宇鹏1,3，唐小锋1,3，盖艳波1,3，胡长进1,3，赵卫雄1,3，张为俊1,3,4

(1 中国科学院安徽光学精密机械研究所中国科学院大气成分与光学重点实验室，安徽合肥 230031;
2 中国科学技术大学研究生院，安徽合肥 230026;
3 中国科学院安徽光学精密机械研究所大气物理化学研究室，安徽合肥 230031;
4 中国科学技术大学环境科学与光电技术学院，安徽合肥 230026 )

收稿日期:2015-12-21 修回日期:2015-12-31 出版日期:2016-03-28 发布日期:2016-03-18
作者简介:温作赢（1991-），男，浙江温州人，研究生，主要从事气溶胶成核研究。
基金资助:
国家自然科学基金资助项目(41175121,41375147)、大科学装置联合基金（U1232209)资助

Study of the Process of Aerosol Particle Formation by Ion-Induced Nucleation

WEN Zuoying1,2,3, GU Xuejun1,3, RONG Hua1,3,4, ZHU Yupeng1,3, TANG Xiaofeng1,3, GAI Yanbo1,3, HU Changjin1,3, ZHAO Weixiong1,3, ZHANG Weijun1,3,4

(1 Key Laboratory of Atmospheric Composition and Optical Radiation, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, Anhui, China;
2 Graduate School, University of Science and Technology of China, Hefei, 230026, Anhui, China;
3 Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, Anhui, China;
4 School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei, 230026, Anhui, China )

Received:2015-12-21 Revised:2015-12-31 Published:2016-03-28 Online:2016-03-18
Contact: 温作赢（1991-），男，浙江温州人，研究生，主要从事气溶胶成核研究。 E-mail:zywen@mail.ustc.edu.cn

摘要/Abstract

摘要：

离子诱导成核是大气气溶胶形成的重要路径之一。大气中团簇离子的形成，主要由宇宙射线电离空气产生的初级离子与H2O、H2SO4、HNO3、NH3、有机物等物质发生的离子-分子反应而产生。成核是团簇离子生长和蒸发相互竞争的一个过程，团簇离子生长到临界核尺寸时，便可自发生长。研究表明临界核大小约1.6 nm，对应的粒子的质量数在5000 amu以上。离子诱导生成的气溶胶粒子对气候的影响以及离子诱导成核在大气成核事件中是否占主要作用还存在很大争议，这需要进行进一步的外场观察、理论模拟、实验室研究来充分弄清离子诱导成核机理。

关键词: 离子诱导成核, 气溶胶, 团簇离子, 临界核, 宇宙射线, 气候

Abstract:

Ion-induced nucleation is one of the most significant pathway of aerosol particle formation in the atmosphere. Air molecules are radiated by the cosmic ray to generate a mass of initial primary ions which will quickly react with common trace air constituents such as H2O, H2SO4, HNO3, NH3 and organic species to form more stable ions, called as cluster ions. Processes for aerosol formation are the competition between growth and evaporation. When the critical nucleus forms, the formed small aerosol particle growth become spontaneous. This critical diameter can be calculated and predicted to be about 1.6 nm with mass number more than 5000 amu at standard atmospheric condition. However, there exist many controversies on ion-induced nucleation to what extent of influencing global climate and new particle nucleation. More observations, molding and laboratory studies should be carried out to explore the mechanism of ion-induced nucleation clearly.

Key words: ion-induced nucleation, aerosol, cluster ions, critical nucleus, cosmic ray, climate

中图分类号:

X513

温作赢顾学军荣华朱宇鹏唐小锋盖艳波胡长进赵卫雄张为俊. 离子诱导气溶胶成核过程的研究[J]. 大气与环境光学学报, 2016, 11(2): 81-90.

WEN Zuo-Ying, GU Xue-Jun, RONG Hua, ZHU Yu-Feng, TANG Xiao-Feng, GAI Yan-Bo, HU Chang-Jin, ZHAO Wei-Xiong, ZHANG Wei-Jun. Study of the Process of Aerosol Particle Formation by Ion-Induced Nucleation[J]. Journal of Atmospheric and Environmental Optics, 2016, 11(2): 81-90.

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离子诱导气溶胶成核过程的研究

Study of the Process of Aerosol Particle Formation by Ion-Induced Nucleation

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