Issue 1, 2023

Photolysis of nitrophenols in gas phase and aqueous environment: a potential daytime source for atmospheric nitrous acid (HONO)

Abstract

The daytime atmospheric nitrous acid (HONO) source has attracted considerable attention due to its important role in determining the concentrations of hydroxyl radicals (OH˙), O3, and secondary organic aerosols (SOAs). The widespread nitrophenols (NPs) are potential HONO sources; however, the relevant reaction mechanism has not been explored yet. We employ quantum mechanical calculations combined with the statistical RRKM rate theory to explore the photochemical reaction paths of two common NPs (2-NP and 4-NP) to form HONO in the gas and aqueous phases. It is revealed that both NPs have strong sunlight absorption, and photolysis occurs on the excited T1 state. Both NPs can easily dissociate under light in both gas and aqueous phases, where OH˙ and NO are the major products rather than HONO. Due to the higher solubility, 4-NP is found to more easily generate HONO in aqueous solution, which experiences the intermolecular excited state hydrogen transfer with vicinal water molecules. Kinetics shows that the relative humidity (RH) hardly promotes the gas-phase photolysis, and the temperature slightly affects the reaction rates. However, as a minor product, HONO generations from gas-phase 2-NP and aqueous 4-NP have high photolysis frequencies of 5.73 × 10−5 and 5.25 × 10−6 s−1, respectively, indicating that the hydrolysis of NPs can be important sources for atmospheric HONO.

Graphical abstract: Photolysis of nitrophenols in gas phase and aqueous environment: a potential daytime source for atmospheric nitrous acid (HONO)

Supplementary files

Article information

Article type
Paper
Submitted
12 May 2022
Accepted
08 Nov 2022
First published
10 Nov 2022
This article is Open Access
Creative Commons BY license

Environ. Sci.: Atmos., 2023,3, 143-155

Photolysis of nitrophenols in gas phase and aqueous environment: a potential daytime source for atmospheric nitrous acid (HONO)

S. Guo and H. Li, Environ. Sci.: Atmos., 2023, 3, 143 DOI: 10.1039/D2EA00053A

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