Matches in SemOpenAlex for { <https://semopenalex.org/work/W2281120520> ?p ?o ?g. }
- W2281120520 endingPage "120" @default.
- W2281120520 startingPage "108" @default.
- W2281120520 abstract "Abstract PM2.5 mass concentrations and chemical compositions sampled over a 13-month period at a Central European rural background site (Kosetice) are presented in this work. A comprehensive chemical analysis of PM2.5 was performed, which provided elemental composition (Al, Si, S, Cl, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, As, Se, Br, Rb, Sr, Y, Zr, and Pb) and the concentration of water-soluble inorganic anions (SO42 −, NO3−. Cl−, NO2−, Br−, and H2PO4−) and cations (Na+, NH4+, K+, Ca2 +, and Mg2 +), elemental and organic carbon (EC and OC), and levoglucosan. Spearman correlation coefficients between individual chemical species and particle number concentrations were calculated for the following six size ranges: 10–25 nm (N10–25), 25–50 nm (N25–50), 50–80 nm (N50–80), 80–150 nm (N80–150), 150–300 nm (N150–300), and 300–800 nm (N300–800). Average concentrations of individual species were comparable with concentrations reported from similar sites across Central Europe. Organic matter (OM) accounted for 45% of the PM2.5 mass (calculated from OC by a factor of 1.6), while the second most common component were secondary aerosols (SO42 −: 19%, NO3−: 14%, NH4+: 10%), which accounted for 43% of the mass. Based on levoglucosan analysis, 31% of OM was attributed to emissions associated with biomass burning (OMBB). EC concentrations, determined using the EUSAAR_2 thermal optical protocol, contributed 4% to PM2.5 mass. A total of 1% of the mass was attributed to a mineral matter source, while the remaining 6% was from an undetermined mass. Seasonal variations showed highest concentrations of NO3− and OMBB in winter, nitrate share in spring, and an increase in percentage of SO42 − and mineral matter in summer. The largest seasonal variation was found for species associated with wood and coal combustion (levoglucosan, K+, Zn, Pb, As), which had clear maxima during winter. Correlation analysis of different size fraction particle number concentrations was used to distinguish the influence of fresh, local aerosol and aged, long-range transport aerosol. The influences of different air masses were also investigated. The lowest concentrations of PM2.5 were recorded under the influence of marine air masses from the NW, which were also marked by increased concentrations of marine aerosol. In contrast, the highest concentrations of PM2.5 and most major chemical components were measured during periods when continental easterly air masses were dominant." @default.
- W2281120520 created "2016-06-24" @default.
- W2281120520 creator A5001981953 @default.
- W2281120520 creator A5028309809 @default.
- W2281120520 creator A5048343615 @default.
- W2281120520 creator A5063930330 @default.
- W2281120520 creator A5067229374 @default.
- W2281120520 creator A5067467572 @default.
- W2281120520 creator A5069181410 @default.
- W2281120520 date "2016-07-01" @default.
- W2281120520 modified "2023-10-18" @default.
- W2281120520 title "PM2.5 chemical composition at a rural background site in Central Europe, including correlation and air mass back trajectory analysis" @default.
- W2281120520 cites W1965032887 @default.
- W2281120520 cites W1968048476 @default.
- W2281120520 cites W1968176949 @default.
- W2281120520 cites W1968814537 @default.
- W2281120520 cites W1971171963 @default.
- W2281120520 cites W1971290825 @default.
- W2281120520 cites W1973975204 @default.
- W2281120520 cites W1974890203 @default.
- W2281120520 cites W1975417144 @default.
- W2281120520 cites W1977438468 @default.
- W2281120520 cites W1979301559 @default.
- W2281120520 cites W1980127448 @default.
- W2281120520 cites W1981854537 @default.
- W2281120520 cites W1986887669 @default.
- W2281120520 cites W1989730047 @default.
- W2281120520 cites W1992127154 @default.
- W2281120520 cites W1997573841 @default.
- W2281120520 cites W2003403568 @default.
- W2281120520 cites W2004336358 @default.
- W2281120520 cites W2013168736 @default.
- W2281120520 cites W2015879402 @default.
- W2281120520 cites W2018055841 @default.
- W2281120520 cites W2024817158 @default.
- W2281120520 cites W2024817702 @default.
- W2281120520 cites W2025194650 @default.
- W2281120520 cites W2031691972 @default.
- W2281120520 cites W2032624599 @default.
- W2281120520 cites W2034826973 @default.
- W2281120520 cites W2036289626 @default.
- W2281120520 cites W2040239281 @default.
- W2281120520 cites W2040636734 @default.
- W2281120520 cites W2042865522 @default.
- W2281120520 cites W2044276853 @default.
- W2281120520 cites W2046070545 @default.
- W2281120520 cites W2053143391 @default.
- W2281120520 cites W2054887924 @default.
- W2281120520 cites W2064520087 @default.
- W2281120520 cites W2065829262 @default.
- W2281120520 cites W2072435951 @default.
- W2281120520 cites W2074912117 @default.
- W2281120520 cites W2077024417 @default.
- W2281120520 cites W2077419524 @default.
- W2281120520 cites W2077623996 @default.
- W2281120520 cites W2081973984 @default.
- W2281120520 cites W2088149573 @default.
- W2281120520 cites W2093091434 @default.
- W2281120520 cites W2093352306 @default.
- W2281120520 cites W2093914941 @default.
- W2281120520 cites W2094984703 @default.
- W2281120520 cites W2095351791 @default.
- W2281120520 cites W2095931348 @default.
- W2281120520 cites W2106528128 @default.
- W2281120520 cites W2107464250 @default.
- W2281120520 cites W2111570465 @default.
- W2281120520 cites W2114826007 @default.
- W2281120520 cites W2116218281 @default.
- W2281120520 cites W2116634041 @default.
- W2281120520 cites W2116817581 @default.
- W2281120520 cites W2116937628 @default.
- W2281120520 cites W2119770425 @default.
- W2281120520 cites W2121749506 @default.
- W2281120520 cites W2130598929 @default.
- W2281120520 cites W2132413744 @default.
- W2281120520 cites W2143965493 @default.
- W2281120520 cites W2147086057 @default.
- W2281120520 cites W2167183446 @default.
- W2281120520 cites W2329711844 @default.
- W2281120520 cites W2333565916 @default.
- W2281120520 cites W2952410089 @default.
- W2281120520 cites W4246953547 @default.
- W2281120520 cites W2110171985 @default.
- W2281120520 doi "https://doi.org/10.1016/j.atmosres.2016.02.017" @default.
- W2281120520 hasPublicationYear "2016" @default.
- W2281120520 type Work @default.
- W2281120520 sameAs 2281120520 @default.
- W2281120520 citedByCount "67" @default.
- W2281120520 countsByYear W22811205202016 @default.
- W2281120520 countsByYear W22811205202017 @default.
- W2281120520 countsByYear W22811205202018 @default.
- W2281120520 countsByYear W22811205202019 @default.
- W2281120520 countsByYear W22811205202020 @default.
- W2281120520 countsByYear W22811205202021 @default.
- W2281120520 countsByYear W22811205202022 @default.
- W2281120520 countsByYear W22811205202023 @default.
- W2281120520 crossrefType "journal-article" @default.
- W2281120520 hasAuthorship W2281120520A5001981953 @default.