A study of summer and winter highly time-resolved submicron aerosol composition measured at a suburban site in Prague
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10297087" target="_blank" >RIV/00216208:11310/15:10297087 - isvavai.cz</a>
Alternative codes found
RIV/67985858:_____/15:00446399
Result on the web
<a href="http://www.sciencedirect.com/science/article/pii/S1352231015302296" target="_blank" >http://www.sciencedirect.com/science/article/pii/S1352231015302296</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.atmosenv.2015.07.030" target="_blank" >10.1016/j.atmosenv.2015.07.030</a>
Alternative languages
Result language
angličtina
Original language name
A study of summer and winter highly time-resolved submicron aerosol composition measured at a suburban site in Prague
Original language description
The variability of aerosol chemical composition and the impact of the origin of respective air masses were studied in high time resolution for selected periods of high and low levels of aerosol burden at a suburban station in Prague-Suchdol, Czech Republic in summer and winter. Ambient aerosol measurements were performed using the compact-Time of Flight-Aerosol Mass Spectrometer (c-ToF-AMS) and variations in concentration of the main species are discussed. The average mass concentrations for the main species were (summer; winter): organic matter (4.2 mu g/m(3); 8.4 mu g/m(3)), SO42- (2.0 mu g/m(3); 4.4 mu g/m(3)), NH4+ (1.2 mu g/m(3); 2.8 mu g/m(3)), NO3- (0.8 mu g/m(3); 5.4 mu g/m(3)) and Cl- (0.1 mu g/m(3); 0.23 mu g/m(3)). We found an inverse relationship between non-refractory submicron particulate matter (NR-PM1) levels and the boundary layer height, mainly in winter. Furthermore, levels of pollution were influenced by the air mass origin, where cleaner maritime air masses resulted in lower aerosol levels compared to those of continental origin. Analysis of the diurnal variation of NR-PM1 showed minimum concentrations in the afternoon caused by dilution as a result of an increase in the boundary layer height. Most maximum concentrations of the main species occurred in the morning or night except sulphate which had a midday maximum, probably due to downdraft from upper boundary layer air and photochemical formation in the afternoon.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
CF - Physical chemistry and theoretical chemistry
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GAP209%2F11%2F1342" target="_blank" >GAP209/11/1342: Advanced study of physical and chemical properties of atmospheric aerosols in high time resolution</a><br>
Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Atmospheric Environment
ISSN
1352-2310
e-ISSN
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Volume of the periodical
2015
Issue of the periodical within the volume
118
Country of publishing house
GB - UNITED KINGDOM
Number of pages
13
Pages from-to
45-57
UT code for WoS article
000361409900005
EID of the result in the Scopus database
2-s2.0-84938774999