FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2066373886> ?p ?o ?g. }

• W2066373886 endingPage "5858" @default.
• W2066373886 startingPage "5839" @default.
• W2066373886 abstract "Abstract. To better understand the size-segregated chemical composition of aged organic aerosols in the western North Pacific rim, day- and night-time aerosol samples were collected in Sapporo, Japan during summer 2005 using an Andersen impactor sampler with 5 size bins: Dp<1.1, 1.1–2.0, 2.0–3.3, 3.3–7.0, >7.0 μm. Samples were analyzed for the molecular composition of dicarboxylic acids, ketoacids, α-dicarbonyls, and sugars, together with water-soluble organic carbon (WSOC), organic carbon (OC), elemental carbon (EC) and inorganic ions. Based on the analyses of backward trajectories and chemical tracers, we found that during the campaign, air masses arrived from Siberia (a biomass burning source region) on 8–9 August, from China (an anthropogenic source region) on 9–10 August, and from the East China Sea/Sea of Japan (a mixed source receptor region) on 10–11 August. Most of the diacids, ketoacids, dicarbonyls, levoglucosan, WSOC, and inorganic ions (i.e., SO42−, NH4+ and K+) were enriched in fine particles (PM1.1) whereas Ca2+, Mg2+ and Cl− peaked in coarse sizes (>1.1 μm). Interestingly, OC, most sugar compounds and NO3− showed bimodal distributions in fine and coarse modes. In PM1.1, diacids in biomass burning-influenced aerosols transported from Siberia (mean: 252 ng m−3) were more abundant than those in the aerosols originating from China (209 ng m−3) and ocean (142 ng m−3), whereas SO42− concentrations were highest in the aerosols from China (mean: 3970 ng m−3) followed by marine- (2950 ng m−3) and biomass burning-influenced (1980 ng m−3) aerosols. Higher loadings of WSOC (2430 ng m−3) and OC (4360 ng m−3) were found in the fine mode, where biomass-burning products such as levoglucosan are abundant. This paper presents a case study of long-range transported aerosols illustrating that biomass burning episodes in the Siberian region have a significant influence on the chemical composition of carbonaceous aerosols in the western North Pacific rim." @default.
• W2066373886 created "2016-06-24" @default.
• W2066373886 creator A5002875581 @default.
• W2066373886 creator A5014283455 @default.
• W2066373886 creator A5021555258 @default.
• W2066373886 creator A5056801943 @default.
• W2066373886 date "2010-07-02" @default.
• W2066373886 modified "2023-10-14" @default.
• W2066373886 title "Size distributions of dicarboxylic acids, ketoacids, α-dicarbonyls, sugars, WSOC, OC, EC and inorganic ions in atmospheric particles over Northern Japan: implication for long-range transport of Siberian biomass burning and East Asian polluted aerosols" @default.
• W2066373886 cites W1932712003 @default.
• W2066373886 cites W1952525616 @default.
• W2066373886 cites W1964773166 @default.
• W2066373886 cites W1965775902 @default.
• W2066373886 cites W1966931810 @default.
• W2066373886 cites W1974430896 @default.
• W2066373886 cites W1974703729 @default.
• W2066373886 cites W1975262842 @default.
• W2066373886 cites W1976333366 @default.
• W2066373886 cites W1983570730 @default.
• W2066373886 cites W1989559574 @default.
• W2066373886 cites W1993069045 @default.
• W2066373886 cites W1994164018 @default.
• W2066373886 cites W1996265957 @default.
• W2066373886 cites W1998026389 @default.
• W2066373886 cites W1998980845 @default.
• W2066373886 cites W1999064974 @default.
• W2066373886 cites W2008981922 @default.
• W2066373886 cites W2011483523 @default.
• W2066373886 cites W2011522558 @default.
• W2066373886 cites W2012921378 @default.
• W2066373886 cites W2013306321 @default.
• W2066373886 cites W2015737182 @default.
• W2066373886 cites W2019458363 @default.
• W2066373886 cites W2023355455 @default.
• W2066373886 cites W2025194650 @default.
• W2066373886 cites W2027852854 @default.
• W2066373886 cites W2028581362 @default.
• W2066373886 cites W2032415871 @default.
• W2066373886 cites W2034636109 @default.
• W2066373886 cites W2034697559 @default.
• W2066373886 cites W2036289626 @default.
• W2066373886 cites W2039059078 @default.
• W2066373886 cites W2042117130 @default.
• W2066373886 cites W2042331645 @default.
• W2066373886 cites W2048943000 @default.
• W2066373886 cites W2049405423 @default.
• W2066373886 cites W2049802929 @default.
• W2066373886 cites W2052161718 @default.
• W2066373886 cites W2052457809 @default.
• W2066373886 cites W2053856375 @default.
• W2066373886 cites W2064496531 @default.
• W2066373886 cites W2065011172 @default.
• W2066373886 cites W2071077593 @default.
• W2066373886 cites W2073871217 @default.
• W2066373886 cites W2075568186 @default.
• W2066373886 cites W2075668796 @default.
• W2066373886 cites W2082899895 @default.
• W2066373886 cites W2084024865 @default.
• W2066373886 cites W2089565537 @default.
• W2066373886 cites W2089999855 @default.
• W2066373886 cites W2090210927 @default.
• W2066373886 cites W2092677013 @default.
• W2066373886 cites W2096049379 @default.
• W2066373886 cites W2099607486 @default.
• W2066373886 cites W2108642660 @default.
• W2066373886 cites W2116635723 @default.
• W2066373886 cites W2120033713 @default.
• W2066373886 cites W2122574093 @default.
• W2066373886 cites W2127510753 @default.
• W2066373886 cites W2128136443 @default.
• W2066373886 cites W2128874126 @default.
• W2066373886 cites W2128943120 @default.
• W2066373886 cites W2140888622 @default.
• W2066373886 cites W2141924834 @default.
• W2066373886 cites W2146249882 @default.
• W2066373886 cites W2155153115 @default.
• W2066373886 cites W2155516010 @default.
• W2066373886 cites W2160670359 @default.
• W2066373886 cites W2161651958 @default.
• W2066373886 cites W2163854746 @default.
• W2066373886 cites W2164346229 @default.
• W2066373886 cites W2165780998 @default.
• W2066373886 cites W4211082193 @default.
• W2066373886 doi "https://doi.org/10.5194/acp-10-5839-2010" @default.
• W2066373886 hasPublicationYear "2010" @default.
• W2066373886 type Work @default.
• W2066373886 sameAs 2066373886 @default.
• W2066373886 citedByCount "147" @default.
• W2066373886 countsByYear W20663738862012 @default.
• W2066373886 countsByYear W20663738862013 @default.
• W2066373886 countsByYear W20663738862014 @default.
• W2066373886 countsByYear W20663738862015 @default.
• W2066373886 countsByYear W20663738862016 @default.
• W2066373886 countsByYear W20663738862017 @default.
• W2066373886 countsByYear W20663738862018 @default.
• W2066373886 countsByYear W20663738862019 @default.
• W2066373886 countsByYear W20663738862020 @default.
• W2066373886 countsByYear W20663738862021 @default.

• next