<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>8(12)</volume><submitter>De Haan DO</submitter><pubmed_abstract>Hydroxyacetone (HA) is an atmospheric oxidation product of isoprene and other organic precursors that can form brown carbon (BrC). Measured bulk aqueous-phase reaction rates of HA with ammonium sulfate, methylamine, and glycine suggest that these reactions cannot compete with aqueous-phase hydroxyl radical oxidation. In cloud chamber photooxidation experiments with either gaseous or particulate HA in the presence of the same N-containing species, BrC formation was minor, with similar mass absorption coefficients at 365 nm (&lt;0.05 m&lt;sup>2&lt;/sup> g&lt;sup>-1&lt;/sup>). However, rapid changes observed in aerosol volume and gas-phase species concentrations suggest that the lack of BrC was not due to slow reactivity. Filter-based UHPLC/(+)ESI-HR-QTOFMS analysis revealed that the SOA became heavily olig</pubmed_abstract><journal>ACS earth &amp; space chemistry</journal><pagination>2574-2586</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC11664653</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Kinetics and Oligomer Products of the Multiphase Reactions of Hydroxyacetone with Atmospheric Amines, Ammonium Sulfate, and Cloud Processing.</pubmed_title><pmcid>PMC11664653</pmcid><pubmed_authors>Rafla MA</pubmed_authors><pubmed_authors>Pennington EA</pubmed_authors><pubmed_authors>Welsh HG</pubmed_authors><pubmed_authors>De Haan AC</pubmed_authors><pubmed_authors>Cazaunau M</pubmed_authors><pubmed_authors>Hawkins LN</pubmed_authors><pubmed_authors>Cui T</pubmed_authors><pubmed_authors>De Haan DO</pubmed_authors><pubmed_authors>Pangui E</pubmed_authors><pubmed_authors>Andretta AD</pubmed_authors><pubmed_authors>Symons MA</pubmed_authors><pubmed_authors>Doussin JF</pubmed_authors><pubmed_authors>Le C</pubmed_authors><pubmed_authors>Rodriguez AA</pubmed_authors><pubmed_authors>Surratt JD</pubmed_authors></additional><is_claimable>false</is_claimable><name>Kinetics and Oligomer Products of the Multiphase Reactions of Hydroxyacetone with Atmospheric Amines, Ammonium Sulfate, and Cloud Processing.</name><description>Hydroxyacetone (HA) is an atmospheric oxidation product of isoprene and other organic precursors that can form brown carbon (BrC). Measured bulk aqueous-phase reaction rates of HA with ammonium sulfate, methylamine, and glycine suggest that these reactions cannot compete with aqueous-phase hydroxyl radical oxidation. In cloud chamber photooxidation experiments with either gaseous or particulate HA in the presence of the same N-containing species, BrC formation was minor, with similar mass absorption coefficients at 365 nm (&lt;0.05 m&lt;sup>2&lt;/sup> g&lt;sup>-1&lt;/sup>). However, rapid changes observed in aerosol volume and gas-phase species concentrations suggest that the lack of BrC was not due to slow reactivity. Filter-based UHPLC/(+)ESI-HR-QTOFMS analysis revealed that the SOA became heavily olig</description><dates><release>2024-01-01T00:00:00Z</release><publication>2024 Dec</publication><modification>2025-04-04T20:28:54.118Z</modification><creation>2025-04-04T20:28:54.118Z</creation></dates><accession>S-EPMC11664653</accession><cross_references><pubmed>39720219</pubmed><doi>10.1021/acsearthspacechem.4c00237</doi></cross_references></HashMap>