<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Zheng G</submitter><funding>National Natural Science Foundation of China</funding><funding>Max-Planck-Gesellschaft</funding><pagination>12571-12582</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC10469486</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>57(34)</volume><pubmed_abstract>Acidity is one central parameter in atmospheric multiphase reactions, influencing aerosol formation and its effects on climate, health, and ecosystems. Weak acids and bases, mainly CO&lt;sub>2&lt;/sub>, NH&lt;sub>3&lt;/sub>, and organic acids, are long considered to play a role in regulating atmospheric acidity. However, unlike strong acids and bases, their importance and influencing mechanisms in a given aerosol or cloud droplet system remain to be clarified. Here, we investigate this issue with new insights provided by recent advances in the field, in particular, the multiphase buffer theory. We show that, in general, aerosol acidity is primarily buffered by NH&lt;sub>3&lt;/sub>, with a negligible contribution from CO&lt;sub>2&lt;/sub> and a potential contribution from organic acids under certain conditions. Fo</pubmed_abstract><journal>Environmental science &amp; technology</journal><pubmed_title>Role of Carbon Dioxide, Ammonia, and Organic Acids in Buffering Atmospheric Acidity: The Distinct Contribution in Clouds and Aerosols.</pubmed_title><pmcid>PMC10469486</pmcid><funding_grant_id>22188102</funding_grant_id><pubmed_authors>Zheng G</pubmed_authors><pubmed_authors>Su H</pubmed_authors><pubmed_authors>Cheng Y</pubmed_authors></additional><is_claimable>false</is_claimable><name>Role of Carbon Dioxide, Ammonia, and Organic Acids in Buffering Atmospheric Acidity: The Distinct Contribution in Clouds and Aerosols.</name><description>Acidity is one central parameter in atmospheric multiphase reactions, influencing aerosol formation and its effects on climate, health, and ecosystems. Weak acids and bases, mainly CO&lt;sub>2&lt;/sub>, NH&lt;sub>3&lt;/sub>, and organic acids, are long considered to play a role in regulating atmospheric acidity. However, unlike strong acids and bases, their importance and influencing mechanisms in a given aerosol or cloud droplet system remain to be clarified. Here, we investigate this issue with new insights provided by recent advances in the field, in particular, the multiphase buffer theory. We show that, in general, aerosol acidity is primarily buffered by NH&lt;sub>3&lt;/sub>, with a negligible contribution from CO&lt;sub>2&lt;/sub> and a potential contribution from organic acids under certain conditions. Fo</description><dates><release>2023-01-01T00:00:00Z</release><publication>2023 Aug</publication><modification>2025-04-19T20:07:02.296Z</modification><creation>2025-04-19T20:07:02.296Z</creation></dates><accession>S-EPMC10469486</accession><cross_references><pubmed>37599651</pubmed><doi>10.1021/acs.est.2c09851</doi></cross_references></HashMap>