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Hygroscopic behavior of inorganic–organic aerosol systems including ammonium sulfate, dicarboxylic acids, and oligome.r

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    SYSNO ASEP0523796
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleHygroscopic behavior of inorganic–organic aerosol systems including ammonium sulfate, dicarboxylic acids, and oligome.r
    Author(s) Bouzidi, Hichem (UCHP-M) ORCID, RID, SAI
    Zuend, A. (CA)
    Ondráček, Jakub (UCHP-M) RID, ORCID, SAI
    Schwarz, Jaroslav (UCHP-M) RID, ORCID, SAI
    Ždímal, Vladimír (UCHP-M) RID, ORCID, SAI
    Article number117481
    Source TitleAtmospheric Environment. - : Elsevier - ISSN 1352-2310
    Roč. 229, 15 May (2020)
    Number of pages17 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsaerosol particles ; aerosol hygroscopic growth ; water uptake
    Subject RIVDG - Athmosphere Sciences, Meteorology
    OECD categoryMeteorology and atmospheric sciences
    R&D ProjectsLM2015037 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    GA17-19798S GA ČR - Czech Science Foundation (CSF)
    EF16_013/0001315 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Method of publishingOpen access
    Institutional supportUCHP-M - RVO:67985858
    UT WOS000530031600020
    EID SCOPUS85083048409
    DOI10.1016/j.atmosenv.2020.117481
    AnnotationWe provide indirect evidence for the presence of an organic solid alongside solid AS. Hypothetically, the observed disagreement could also be due to a preferential interaction between –COOH and –CH2OCH2- groups, which may prevent a fraction of the organic acid amount to interact with water. For fully deliquesced particles, good agreement between model predictions and measurements are found for the mixed PEG–organic acids–AS systems. Upon dehydration, when the mass fraction of PEG <20%, the signature of effloresced AS in solid–liquid equilibrium with the remaining solution was observed. However, with higher organic volume fraction, the particles release water gradually without a noticeable efflorescence of AS down to 20% RH. For quinary PEG–organic acids–AS systems, the AIOMFAC-based equilibrium model predicts that liquid–liquid phase separation (LLPS) occurs with a clear distinction between a predominantly electrolyte-rich phase alfa (composed mainly of ammonium and sulfate ions, organic acids and water) and an organic-rich phase beta (composed mainly of PEG). The onset of LLPS is predicted at RH levels of 83–89% depending on the mixed particle’s composition. We also show that a residence time of ~10 s in the humidified section of the HTDMA instrument is sufficient for establishing gas–particle equilibrium of the 100 nm sized organic–inorganic particles studied in this work, this may differ in other cases when highly viscous particles are involved. The measurements offer valuable data for future work on the development and validation of organic solid–liquid equilibrium in thermodynamic models.
    WorkplaceInstitute of Chemical Process Fundamentals
    ContactEva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227
    Year of Publishing2021
    Electronic addresshttps://www.sciencedirect.com/journal/atmospheric-environment/vol/229/suppl/C
Number of the records: 1  

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