Number of the records: 1  

Source apportionment of fine aerosol at a rural background site in Central Europe based on seasonal distributions of dicarboxylic acids, sugars and related compounds

  1. 1.
    SYSNO ASEP0573525
    Document TypeA - Abstract
    R&D Document TypeThe record was not marked in the RIV
    R&D Document TypeNení vybrán druh dokumentu
    TitleSource apportionment of fine aerosol at a rural background site in Central Europe based on seasonal distributions of dicarboxylic acids, sugars and related compounds
    Author(s) Vodička, Petr (UCHP-M) RID, ORCID, SAI
    Kawamura, K. (JP)
    Deshmukh, D.K. (JP)
    Pokorná, Petra (UCHP-M) ORCID, RID, SAI
    Schwarz, Jaroslav (UCHP-M) RID, ORCID, SAI
    Ždímal, Vladimír (UCHP-M) RID, ORCID, SAI
    ActionEGU General Assembly 2023
    Event date23.04.2023 - 28.04.2023
    VEvent locationVienna
    CountryAT - Austria
    Event typeEUR
    Languageeng - English
    Keywordsfine aerosol ; rural background site ; seasonal distributions
    OECD categoryMeteorology and atmospheric sciences
    R&D ProjectsLM2018122 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    GC20-08304J GA ČR - Czech Science Foundation (CSF)
    Institutional supportUCHP-M - RVO:67985858
    AnnotationWater-soluble dicarboxylic acids (hereafter diacids) and sugars are an important part of the atmospheric water-soluble organic aerosol. Here, we studied diacids and other compounds in fine aerosol particles (PM1) collected at a rural background site National Atmospheric Observatory Košetice (NAOK), Czech Republic, Central Europe. Aerosol samples were collected every second day for 24 h from September 2013 to August 2014 (n=146). Based on receptor modeling (PMF), we identified PM1 organic compounds that are more typical to anthropogenic and to biogenic sources. We have apportioned two anthropogenic sources especially evident during the heating season from mid-October to mid-April: (i) biomass burning (BB) (main contribution of levoglucosan and methylsuccinic, maleic, methylmaleic and azelaic acids) and (ii) fossil fuel combustion (FF) (represented by phthalic, terephthalic and ketomalonic acids). Furthermore, we identified two sources of biogenic aerosols: (iii) summer factor was largely characterized by compounds with three and seven carbons (malonic, 4-ketopimelic, oxoheptanoic, methylmalonic acids) while (iv) spring biogenic factor was characterized mostly by primary sugars, normal chain diacids and their precursors (oxalic, malonic, succinic, glutaric, ketomalonic, 4-oxobutanoic and 5-oxopentanoic acids). Last but not least, we distinguished (v) background factor mainly represented by less oxidized diacids precursors such as glyoxal, methylglyoxal, glyoxylic and pyruvic acids, but also by aromatic diacids, which may originate from traffic emissions; a stable and year-round source.
    WorkplaceInstitute of Chemical Process Fundamentals
    ContactEva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227
    Year of Publishing2024
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.