Single-particle measurements of bouncing particles and in situ collection efficiency from an airborne aerosol mass spectrometer (AMS) with light-scattering detection

dc.bibliographicCitation.firstPage3801
dc.bibliographicCitation.issue10
dc.bibliographicCitation.journalTitleAtmospheric measurement techniques : AMTeng
dc.bibliographicCitation.lastPage3820
dc.bibliographicCitation.volume10
dc.contributor.authorLiao, Jin
dc.contributor.authorBrock, Charles A.
dc.contributor.authorMurphy, Daniel M.
dc.contributor.authorSueper, Donna T.
dc.contributor.authorWelti, André
dc.contributor.authorMiddlebrook, Ann M.
dc.date.accessioned2023-02-27T08:51:28Z
dc.date.available2023-02-27T08:51:28Z
dc.date.issued2017
dc.description.abstractA light-scattering module was coupled to an airborne, compact time-of-flight aerosol mass spectrometer (LS-AMS) to investigate collection efficiency (CE) while obtaining nonrefractory aerosol chemical composition measurements during the Southeast Nexus (SENEX) campaign. In this instrument, particles scatter light from an internal laser beam and trigger saving individual particle mass spectra. Nearly all of the single-particle data with mass spectra that were triggered by scattered light signals were from particles larger than ĝ1/4 280ĝ€nm in vacuum aerodynamic diameter. Over 33ĝ€000 particles are characterized as either prompt (27ĝ€%), delayed (15ĝ€%), or null (58ĝ€%), according to the time and intensity of their total mass spectral signals. The particle mass from single-particle spectra is proportional to that derived from the light-scattering diameter (<i>d</i>va-LS) but not to that from the particle time-of-flight (PToF) diameter (<i>d</i>va-MS) from the time of the maximum mass spectral signal. The total mass spectral signal from delayed particles was about 80ĝ€% of that from prompt ones for the same <i>d</i>va-LS. Both field and laboratory data indicate that the relative intensities of various ions in the prompt spectra show more fragmentation compared to the delayed spectra. The particles with a delayed mass spectral signal likely bounced off the vaporizer and vaporized later on another surface within the confines of the ionization source. Because delayed particles are detected by the mass spectrometer later than expected from their <i>d</i>va-LS size, they can affect the interpretation of particle size (PToF) mass distributions, especially at larger sizes. The CE, measured by the average number or mass fractions of particles optically detected that had measurable mass spectra, varied significantly (0.2-0.9) in different air masses. The measured CE agreed well with a previous parameterization when CE > 0.5 for acidic particles but was sometimes lower than the minimum parameterized CE of 0.5.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11527
dc.identifier.urihttp://dx.doi.org/10.34657/10561
dc.language.isoeng
dc.publisherKatlenburg-Lindau : Copernicus
dc.relation.doihttps://doi.org/10.5194/amt-10-3801-2017
dc.relation.essn1867-8548
dc.rights.licenseCC BY 3.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/3.0
dc.subject.ddc550
dc.subject.otheraerosoleng
dc.subject.otherair masseng
dc.subject.otherchemical compositioneng
dc.subject.otherefficiency measurementeng
dc.subject.otherionizationeng
dc.subject.otherparameterizationeng
dc.subject.otherparticle sizeeng
dc.subject.otherspectrometereng
dc.titleSingle-particle measurements of bouncing particles and in situ collection efficiency from an airborne aerosol mass spectrometer (AMS) with light-scattering detectioneng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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