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氨与甲胺对地球大气中核化的协同效应:一项理论研究

Synergistic Effect of Ammonia and Methylamine on Nucleation in the Earth's Atmosphere. A Theoretical Study.

作者信息

Wang Chun-Yu, Jiang Shuai, Liu Yi-Rong, Wen Hui, Wang Zhong-Quan, Han Ya-Juan, Huang Teng, Huang Wei

机构信息

Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics & Fine Mechanics , Chinese Academy of Sciences , Hefei , Anhui 230031 , China.

School of Information Science and Technology , University of Science and Technology of China , Hefei , Anhui 230026 , China.

出版信息

J Phys Chem A. 2018 Apr 5;122(13):3470-3479. doi: 10.1021/acs.jpca.8b00681. Epub 2018 Mar 23.

DOI:10.1021/acs.jpca.8b00681
PMID:29547296
Abstract

Ammonia and amines are important common trace atmospheric species that can enhance new particle formation (NPF) in the Earth's atmosphere. However, the synergistic effect of these two bases involving nucleation is still lacking. We studied the most stable geometric structures and thermodynamics of quaternary (NH)(CHNH)(HSO) (HO) ( m = 1-3, n = 0-4) clusters at the PW91PW91/6-311++G(3df,3pd) level of theory for the first time. We find that the proton transfer from HSO molecule to CHNH molecule is easier than to NH molecule in the free or hydrated HSO-base clusters, and thus leads to the stability. The energetically favorable formation of the (NH)(CHNH)(HSO) (HO) ( n = 0-4) clusters, by hydration or attachment of base or substitution of ammonia by methylamine at 298.15 K, indicate that ammonia and methylamine together could enhance the stabilization of small binary clusters. At low RH and an ambient temperature of 298.15 K, the concentration of total hydrated (NH)(CHNH)(HSO) clusters could reach that of total hydrated (NH)(HSO) clusters, which is the most stable ammonia-containing cluster. These results indicate that the synergistic effect of NH and CHNH might be important in forming the initial cluster with sulfuric acid and subsequently growth process. In addition, the evaporation rates of (NH)(CHNH)(HSO)(HO), (NH)(CHNH)(HSO) and (NH)(CHNH)(HSO) clusters, three relative abundant clusters in (NH)(CHNH)(HSO) (HO) system, were calculated. We find the stability increases with the increasing number of HSO molecules.

摘要

氨和胺是大气中重要的常见痕量物种,能够促进地球大气中的新粒子形成(NPF)。然而,这两种碱在成核过程中的协同效应仍不明确。我们首次在PW91PW91/6 - 311++G(3df,3pd)理论水平上研究了季铵盐(NH)(CHNH)(HSO)(HO) (m = 1 - 3,n = 0 - 4)团簇的最稳定几何结构和热力学性质。我们发现,在自由或水合的HSO - 碱团簇中,质子从HSO分子转移到CHNH分子比转移到NH分子更容易,从而导致了稳定性。在298.15 K时,通过水合、碱附着或用甲胺取代氨,(NH)(CHNH)(HSO)(HO) (n = 0 - 4)团簇在能量上有利于形成,这表明氨和甲胺共同作用可以增强小二元团簇的稳定性。在低相对湿度和298.15 K的环境温度下,总水合(NH)(CHNH)(HSO)团簇的浓度可以达到总水合(NH)(HSO)团簇的浓度,而(NH)(HSO)团簇是最稳定的含氨团簇。这些结果表明,NH和CHNH的协同效应在与硫酸形成初始团簇以及随后的生长过程中可能很重要。此外,还计算了(NH)(CHNH)(HSO)(HO)体系中相对丰富的三个团簇(NH)(CHNH)(HSO)(HO)、(NH)(CHNH)(HSO)和(NH)(CHNH)(HSO)的蒸发速率。我们发现稳定性随着HSO分子数量的增加而增加。

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