Formation of HONO from the NH<sub>3</sub>-promoted hydrolysis of NO<sub>2</sub> dimers in the atmosphere.
basic_science · Level V
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- Record sourced from PubMed, PMID 29941594.
- Also identified by DOI 10.1073/pnas.1807719115 and PMC identifier 6048549.
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Abstract
One challenging issue in atmospheric chemistry is identifying the source of nitrous acid (HONO), which is believed to be a primary source of atmospheric "detergent" OH radicals. Herein, we show a reaction route for the formation of HONO species from the NH<sub>3</sub>-promoted hydrolysis of a NO<sub>2</sub> dimer (ONONO<sub>2</sub>), which entails a low free-energy barrier of 0.5 kcal/mol at room temperature. Our systematic study of HONO formation based on NH<sub>3</sub> + ONONO<sub>2</sub> + <i>n</i>H<sub>2</sub>O and water droplet systems with the metadynamics simulation method and a reaction pathway searching method reveals two distinct mechanisms: (<i>i</i>) In monohydrates (<i>n</i> = 1), tetrahydrates (<i>n</i> = 4), and water droplets, only one water molecule is directly involved in the reaction (denoted the single-water mechanism); and (<i>ii</i>) the splitting of two neighboring water molecules is seen in the dihydrates (<i>n</i> = 2) and trihydrates (<i>n</i> = 3) (denoted the dual-water mechanism). A comparison of the computed free-energy surface for NH<sub>3</sub>-free and NH<sub>3</sub>-containing systems indicates that gaseous NH<sub>3</sub> can markedly lower the free-energy barrier to HONO formation while stabilizing the product state, producing a more exergonic reaction, in contrast to the endergonic reaction for the NH<sub>3</sub>-free system. More importantly, the water droplet reduces the free-energy barrier for HONO formation to 0.5 kcal/mol, which is negligible at room temperature. We show that the entropic contribution is important in the mechanism by which NH<sub>3</sub> promotes HONO formation. This study provides insight into the importance of fundamental HONO chemistry and its broader implication to aerosol and cloud processing chemistry at the air-water interface.