Atmospheric chemistry of CH3CHO: the hydrolysis of CH3CHO catalyzed by H2SO4. Issue 11 (2nd March 2018)

• Record Type: Journal Article
• Authors: Tan, Xing-Feng; Long, Bo; Ren, Da-Sen; Zhang, Wei-Jun; Long, Zheng-Wen; Mitchell, Ellen
• Is Part Of: Physical chemistry chemical physics. Volume 20:Issue 11(2018)
• Page Start: 7701
• Page End: 7709
• Publication Date: 2018-03-02
• Subjects: Chemistry, Physical and theoretical -- Periodicals; 541.3
• DOI: 10.1039/c7cp07312g
• Languages: English
• ISSNs: 1463-9076

Abstract

Abstract : We found the catalytic effect of H2 SO4 on the hydrolysis of CH3 CHO in the atmosphere. Abstract : Elucidating atmospheric oxidation mechanisms and the reaction kinetics of atmospheric compounds is of great importance and necessary for atmospheric modeling and the understanding of the formation of atmospheric organic aerosols. While the hydrolysis of aldehydes has been detected in the presence of sulfuric acid, the reaction mechanism and kinetics remain unclear. Herein, we use electronic structure methods with CCSD(T)/CBS accuracy and canonical variational transition state theory combined with small-curvature tunneling to study the reaction mechanism and kinetics of the hydrolysis of CH3 CHO. The calculated results show that the hydrolysis of CH3 CHO needs to overcome an energy barrier of 37.21 kcal mol −1, while the energy barrier is decreased to −9.79 kcal mol −1 with a sulfuric acid catalyst. In addition, the calculated kinetic results show that the H2 SO4 ⋯H2 O + CH3 CHO reaction is faster than H2 SO4 + CH3 CHO⋯H2 O. Additionally, the H2 SO4 ⋯H2 O + CH3 CHO reaction can play an important role in the sink of CH3 CHO below 260 K occurring during the night period when OH, H2 SO4, and H2 O concentrations are 10 4, 10 8, and 10 17 molecules cm −3, respectively, because it can compete well with the CH3 CHO + OH reaction. There are wide implications in atmospheric chemistry from these findings because of the potential importance of the catalytic effect of H2 SO4 on the hydrolysis of CH3 CHO in the atmosphere and in the formation of secondary organic aerosols.