Abstract
The carbonate radical anion CO3•− is a key intermediate in tropospheric anion chemistry. Despite its radical character, only a small number of reactions have been reported in the literature. Here we investigate the gas-phase reactions of CO3•− and CO3•−(H2O) with HCl under ultrahigh vacuum conditions. Bare CO3•− forms OHCl•− with a rate constant of 4.2 x 10-12 cm3 s-1, which corresponds to an efficiency of only 0.4%. Hydration accelerates the reaction, and ligand exchange of H2O against HCl proceeds with a rate of 2.7 X 10-10 cm3 s-1. Quantum chemical calculations reveal that OHCl•− is best described as an OH• hydrogen bonded to Cl-, while the ligand exchange product is Cl-(HCO3•). Under tropospheric conditions, where CO3•−(H2O) is the dominant species, Cl-(HCO3•) is efficiently formed. These reactions must be included in models of tropospheric anion chemistry.
Original language | English |
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Pages (from-to) | 192-197 |
Journal | The Journal of Physical Chemistry A |
Volume | 121 |
Issue number | 1 |
Online published | 13 Dec 2016 |
DOIs | |
Publication status | Published - 12 Jan 2017 |
Funding
M.K.B. acknowledges startup funds from the University of Innsbruck. C.K.S. thanks City University of Hong Kong (CityU) for financial support (Project No. 7004401). W.K.T. acknowledges Chow Yei Ching School of Graduate Studies, CityU, for his postgraduate studentship and scholarship.
Research Keywords
- MOLECULAR NEGATIVE-IONS
- PHOTODISSOCIATION SPECTROSCOPY
- CLUSTER IONS
- NITRIC-ACID
- DYNAMICS
- MODEL
- CO3
- THERMOCHEMISTRY
- PHOTODETACHMENT
- CHEMISTRY