<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Rana MS</submitter><funding>Division of Chemistry</funding><pagination>2900-2909</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9762487</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>6(12)</volume><pubmed_abstract>Biomass burning emissions contain abundant phenolic aldehydes (e.g., syringaldehyde, vanillin, and 4-hydroxybenaldehyde) that are oxidized during atmospheric transport, altering the physicochemical properties of particulates. Herein, the oxidative processing of thin films made of syringaldehyde, vanillin, and 4-hydroxybenaldehyde is studied at the air-solid interface under a variable O&lt;sub>3&lt;/sub>(g) molar ratio (410 ppbv-800 ppmv) and relative humidity (0-90%). Experiments monitored the absorption changes of C=C, C=O, and -COOH vibration changes during the oxidation of thin films by transmission Fourier transform infrared spectroscopy (FTIR). Selected spectroscopic features of aromatic ring cleavage by O&lt;sub>3&lt;/sub>(g) revealed the production of carboxylic acids. Instead, monitoring O-H stretching provided a comparison of a hydroxylation channel from in situ produced hydroxyl radical. The overall oxidation reactivity trend syringaldehyde > vanillin > 4-hydroxybenzladehyde can be explained based on the additional electron density from methoxide substituents to the ring. The reactive uptake coefficient of O&lt;sub>3&lt;/sub>(g) increases for higher relative humidity, e.g., for syringaldehyde by 18 and 215 times at 74% and 90% relative humidity (RH), respectively, as compared to dry conditions. A Langmuir-Hinshelwood mechanism fits well the kinetics of oxidation under a variable O&lt;sub>3&lt;/sub>(g) molar ratio at 74% RH, providing useful information that should be included in atmospheric chemistry models.</pubmed_abstract><journal>ACS earth &amp; space chemistry</journal><pubmed_title>Oxidation of Phenolic Aldehydes by Ozone and Hydroxyl Radicals at the Air-Solid Interface.</pubmed_title><pmcid>PMC9762487</pmcid><funding_grant_id>1903744</funding_grant_id><pubmed_authors>Guzman MI</pubmed_authors><pubmed_authors>Rana MS</pubmed_authors></additional><is_claimable>false</is_claimable><name>Oxidation of Phenolic Aldehydes by Ozone and Hydroxyl Radicals at the Air-Solid Interface.</name><description>Biomass burning emissions contain abundant phenolic aldehydes (e.g., syringaldehyde, vanillin, and 4-hydroxybenaldehyde) that are oxidized during atmospheric transport, altering the physicochemical properties of particulates. Herein, the oxidative processing of thin films made of syringaldehyde, vanillin, and 4-hydroxybenaldehyde is studied at the air-solid interface under a variable O&lt;sub>3&lt;/sub>(g) molar ratio (410 ppbv-800 ppmv) and relative humidity (0-90%). Experiments monitored the absorption changes of C=C, C=O, and -COOH vibration changes during the oxidation of thin films by transmission Fourier transform infrared spectroscopy (FTIR). Selected spectroscopic features of aromatic ring cleavage by O&lt;sub>3&lt;/sub>(g) revealed the production of carboxylic acids. Instead, monitoring O-H stretching provided a comparison of a hydroxylation channel from in situ produced hydroxyl radical. The overall oxidation reactivity trend syringaldehyde > vanillin > 4-hydroxybenzladehyde can be explained based on the additional electron density from methoxide substituents to the ring. The reactive uptake coefficient of O&lt;sub>3&lt;/sub>(g) increases for higher relative humidity, e.g., for syringaldehyde by 18 and 215 times at 74% and 90% relative humidity (RH), respectively, as compared to dry conditions. A Langmuir-Hinshelwood mechanism fits well the kinetics of oxidation under a variable O&lt;sub>3&lt;/sub>(g) molar ratio at 74% RH, providing useful information that should be included in atmospheric chemistry models.</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 Dec</publication><modification>2026-06-03T12:29:44.933Z</modification><creation>2025-04-25T20:01:28.275Z</creation></dates><accession>S-EPMC9762487</accession><cross_references><pubmed>36561198</pubmed><doi>10.1021/acsearthspacechem.2c00206</doi></cross_references></HashMap>