Impact of water uptake and mixing state on submicron particle deposition in the human respiratory tract (HRT) based on explicit hygroscopicity measurements at HRT-like conditions

dc.bibliographicCitation.firstPage12387
dc.bibliographicCitation.issue18
dc.bibliographicCitation.lastPage12399
dc.bibliographicCitation.volume22
dc.contributor.authorMan, Ruiqi
dc.contributor.authorWu, Zhijun
dc.contributor.authorZong, Taomou
dc.contributor.authorVoliotis, Aristeidis
dc.contributor.authorQiu, Yanting
dc.contributor.authorGröß, Johannes
dc.contributor.authorvan Pinxteren, Dominik
dc.contributor.authorZeng, Limin
dc.contributor.authorHerrmann, Hartmut
dc.contributor.authorWiedensohler, Alfred
dc.contributor.authorHu, Min
dc.date.accessioned2023-03-01T09:28:12Z
dc.date.available2023-03-01T09:28:12Z
dc.date.issued2022
dc.description.abstractParticle hygroscopicity plays a key role in determining the particle deposition in the human respiratory tract (HRT). In this study, the effects of hygroscopicity and mixing state on regional and total deposition doses on the basis of the particle number concentration for children, adults, and the elderly were quantified using the Multiple-Path Particle Dosimetry model, based on the size-resolved particle hygroscopicity measurements at HRT-like conditions (relative humidity = 98 %) performed in the North China Plain. The measured particle population with an external mixing state was dominated by hygroscopic particles (number fraction = (91.5 ± 5.7) %, mean ± standard deviation (SD); the same below). Particle hygroscopic growth in the HRT led to a reduction by around 24 % in the total doses of submicron particles for all age groups. Such a reduction was mainly caused by the growth of hygroscopic particles and was more pronounced in the pulmonary and tracheobronchial regions. Regardless of hygroscopicity, the elderly group of people had the highest total dose among three age groups, while children received the maximum total deposition rate. With 270 nm in diameter as the boundary, the total deposition doses of particles smaller than this diameter were overestimated, and those of larger particles were underestimated, assuming no particle hygroscopic growth in the HRT. From the perspective of the daily variation, the deposition rates of hygroscopic particles with an average of (2.88 ± 0.81) × 109 particles h-1 during the daytime were larger than those at night ((2.32 ± 0.24) × 109 particles h-1). On the contrary, hydrophobic particles interpreted as freshly emitted soot and primary organic aerosols exhibited higher deposition rates at nighttime ((3.39 ± 1.34) × 108 particles h-1) than those in the day ((2.58 ± 0.76) × 108 particles h-1). The traffic emissions during the rush hours enhanced the deposition rate of hydrophobic particles. This work provides a more explicit assessment of the impact of hygroscopicity and mixing state on the deposition pattern of submicron particles in the HRT. Copyright:eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11616
dc.language.isoeng
dc.publisherKatlenburg-Lindau : EGU
dc.relation.doihttps://doi.org/10.5194/acp-22-12387-2022
dc.relation.essn1680-7324
dc.relation.ispartofseriesAtmospheric chemistry and physics 22 (2022), Nr. 18eng
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectatmospheric chemistryeng
dc.subjectatmospheric depositioneng
dc.subjectconcentration (composition)eng
dc.subjecthygroscopicityeng
dc.subjectnumerical modeleng
dc.subjectparticle sizeeng
dc.subjectsize distributioneng
dc.subjectChinaeng
dc.subjectNorth China Plaineng
dc.subject.ddc550
dc.titleImpact of water uptake and mixing state on submicron particle deposition in the human respiratory tract (HRT) based on explicit hygroscopicity measurements at HRT-like conditionseng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleAtmospheric chemistry and physics
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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