6533b828fe1ef96bd1288dfc

RESEARCH PRODUCT

Aerosol Chemistry Resolved by Mass Spectrometry: Linking Field Measurements of Cloud Condensation Nuclei Activity to Organic Aerosol Composition.

Thorsten HoffmannUlla MakkonenUlrich PöschlJohn CrowleyChristina Müller-tautgesHannele HakolaJohannes SchneiderAlexander L. VogelGavin PhillipsChristoph ZuthDiana RoseMeinrat O. AndreaeMira L. Pöhlker

subject

010504 meteorology & atmospheric sciencesAnalytical chemistryAtmospheric-pressure chemical ionizationGeneral Chemistry010501 environmental sciencesMass spectrometry01 natural sciencesAerosolchemistry.chemical_compoundchemistryEnvironmental ChemistryAerosol mass spectrometryCloud condensation nucleiSulfateChemical compositionMass fraction0105 earth and related environmental sciences

description

Aerosol hygroscopic properties were linked to its chemical composition by using complementary online mass spectrometric techniques in a comprehensive chemical characterization study at a rural mountaintop station in central Germany in August 2012. In particular, atmospheric pressure chemical ionization mass spectrometry ((-)APCI-MS) provided measurements of organic acids, organosulfates, and nitrooxy-organosulfates in the particle phase at 1 min time resolution. Offline analysis of filter samples enabled us to determine the molecular composition of signals appearing in the online (-)APCI-MS spectra. Aerosol mass spectrometry (AMS) provided quantitative measurements of total submicrometer organics, nitrate, sulfate, and ammonium. Inorganic sulfate measurements were achieved by semionline ion chromatography and were compared to the AMS total sulfate mass. We found that up to 40% of the total sulfate mass fraction can be covalently bonded to organic molecules. This finding is supported by both on- and offline soft ionization techniques, which confirmed the presence of several organosulfates and nitrooxy-organosulfates in the particle phase. The chemical composition analysis was compared to hygroscopicity measurements derived from a cloud condensation nuclei counter. We observed that the hygroscopicity parameter (κ) that is derived from organic mass fractions determined by AMS measurements may overestimate the observed κ up to 0.2 if a high fraction of sulfate is bonded to organic molecules and little photochemical aging is exhibited.

10.1021/acs.est.6b01675https://pubmed.ncbi.nlm.nih.gov/27709898