Molecular mechanisms and atmospheric implications of the simplest criegee intermediate and hydrochloric acid chemistry in the gas phase and at the aqueous interfaces

• Published in: Atmospheric environment (1994) 2024-08, Vol.330, p.120558, Article 120558
• Main Authors: Ding, Chao, Wen, Mingjie, Zhang, Tianlei, Li, Zeyao, Li, Rongrong, Wang, Rui, Ou, Ting, Song, Fengmin, Zhang, Qiang
• Format: Article
• Language: English
• ISSN: 1352-2310; 1873-2844
• DOI: 10.1016/j.atmosenv.2024.120558

The atmospheric chemistry of Criegee Intermediates has become a frontier research point in environmental pollution in recent years. In this work, quantum chemical calculations and Born-Oppenheimer Molecular Dynamics (BOMD) simulations were employed to explore the gas phase and aqueous interface behavior of the simplest Criegee Intermediate (sCI, CH2OO) and hydrochloric acid (HCl) reaction. Quantum chemical calculations have revealed that the product of ClCH2OOH (CMHP) formation from the CH2OO + HCl reaction without and with water molecule undergoes a barrierless or near barrierless process in the gas phase. The results of the rate coefficients calculated by the master equation indicate that the gas-phase CMHP formation from the reaction of CH2OO + HCl could compete with the hydrolysis of CH2OO with (H2O)2 at the altitude of 15 km. BOMD simulations at the aqueous interfaces show that the CH2OO + HCl reaction occurs through stepwise mechanisms that are distinct from those in the gas phase. Three different interfacial reaction channels were identified: i) CMHP direct formation, ii) water-mediated CMHP formation, and iii) HCl-mediated hydroxymethyl hydroperoxide (HMHP) formation, and completed in picosecond time scales. Considering the harsh reaction conditions between CH2OO and HCl at the interface (i.e., the two molecules must be sufficiently close to form the CH2OO-HCl complex), the route of HMHP formation via the hydrolysis of CH2OO remains the main atmospheric loss pathway of CH2OO at the aqueous interfaces. Interestingly, molecular dynamic simulations in nanosecond time scales reveal that the formed CMHP in the gas phase has a tendency to aggregate with sulfuric acids, ammonia, and water molecules to form stable clusters within 213–278 K. The present results for the CMHP and HMHP formations from the sCI-HCl chemistry in the atmosphere will enhance our comprehension of the atmospheric behavior of Criegee intermediates in urban and marine pollution areas. [Display omitted] •Clarification of gas phase and aqueous interface reaction mechanisms for CH2OO + HCl.•HCl could be a significant atmospheric scavenger of CH2OO at 15 km altitude.•The aqueous interface CMHP formation mechanism from CH2OO + HCl was confirmed.•Aqueous interface reactions occur in picoseconds and follow a stepwise mechanism.