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Soot microstructure significantly influences the photochemical conversion of NO₂ to HONO, and potential regulatory pathways remain insufficiently understood. Here, we systematically investigated the photochemical pathways of NO₂ with soot and identified key structural factors governing the soot photoreactivity. Soot samples exhibited obviously distinct photoreactivity, as evidenced by varying NO₂ uptake coefficients and HONO yields. NO₂ uptake and HONO formation were positively correlated with photogenerated electrons (e⁻), suggesting that NO₂ was reduced to HONO by accepting free e⁻ on soot. Edge and surface defects in soot acted as the critical reactive sites for e⁻ generation, where oxygen-containing functional groups can facilitate the e⁻ transfer. Directed migration of photogenerated e⁻ from organic carbon (OC) to elemental carbon (EC) improved e⁻ utilization, enabling synergistic effects of EC and OC on HONO formation. The importance of the soot microstructure in modulating e⁻ generation and transport was well explored for driving NO₂ photoreduction to HONO.
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Lai et al. (2026) studied this question.
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