HeterogeneousUptake onto Deliquesced Particles asan Atmospheric Fate of Isoprene-Derived Hydroxy-RO<sub>2</sub>

We integrated a chemical conversion technique to transform RO<sub>2</sub> into OH radicals with a method combining laser photolysis radical generation and time-resolved OH radical detection by laser-induced fluorescence (LP-LIF). This approach allowed us to investigate the uptake coefficient of an isoprene-derived hydroxy–RO<sub>2</sub>, ISOPOO (HOC<sub>5</sub>H<sub>8</sub>OO·), onto deliquesced NaCl particles and the effect of transition metal ions (Fe<sup>2+</sup> and Cu<sup>2+</sup>) on this uptake. We measured the uptake coefficients, <i>γ,</i> of ISOPOO on deliquesced NaCl particles doped with FeCl<sub>2</sub> and CuCl<sub>2</sub>, each added at 5 wt % of NaCl, at 301 K and 84% relative humidity (RH). The results were 0.45 ± 0.01 for FeCl<sub>2</sub> and 0.19 ± 0.01 for CuCl<sub>2</sub>. These values were 5 and 2 times greater than the uptake coefficient for deliquesced undoped NaCl particles, which was 0.09 ± 0.01. Preliminary simulation results for the western Japan domain, using a value of γ = 0.09 from a three-dimensional chemical transport model, indicate that the heterogeneous uptake of ISOPOO onto deliquesced particles contributed, on average, less than 3% of the ISOPOO loss process. This contribution increased to as much as 5% in remote forest and mountain areas during high PM<sub>2.5</sub> events.

Publication Details

Journal
Figshare
Published
2025-03-15
DOI
https://doi.org/10.1021/acsestair.4c00165.s001
Primary Topic
Atmospheric chemistry and aerosols
Type
article
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article

HeterogeneousUptake onto Deliquesced Particles asan Atmospheric Fate of Isoprene-Derived Hydroxy-RO2

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Atmospheric chemistry and aerosols
article

HeterogeneousUptake onto Deliquesced Particles asan Atmospheric Fate of Isoprene-Derived Hydroxy-RO2

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Abstract

We integrated a chemical conversion technique to transform RO<sub>2</sub> into OH radicals with a method combining laser photolysis radical generation and time-resolved OH radical detection by laser-induced fluorescence (LP-LIF). This approach allowed us to investigate the uptake coefficient of an isoprene-derived hydroxy–RO<sub>2</sub>, ISOPOO (HOC<sub>5</sub>H<sub>8</sub>OO·), onto deliquesced NaCl particles and the effect of transition metal ions (Fe<sup>2+</sup> and Cu<sup>2+</sup>) on this uptake. We measured the uptake coefficients, <i>γ,</i> of ISOPOO on deliquesced NaCl particles doped with FeCl<sub>2</sub> and CuCl<sub>2</sub>, each added at 5 wt % of NaCl, at 301 K and 84% relative humidity (RH). The results were 0.45 ± 0.01 for FeCl<sub>2</sub> and 0.19 ± 0.01 for CuCl<sub>2</sub>. These values were 5 and 2 times greater than the uptake coefficient for deliquesced undoped NaCl particles, which was 0.09 ± 0.01. Preliminary simulation results for the western Japan domain, using a value of γ = 0.09 from a three-dimensional chemical transport model, indicate that the heterogeneous uptake of ISOPOO onto deliquesced particles contributed, on average, less than 3% of the ISOPOO loss process. This contribution increased to as much as 5% in remote forest and mountain areas during high PM<sub>2.5</sub> events.

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