FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2556281736> ?p ?o ?g. }

• W2556281736 endingPage "83" @default.
• W2556281736 startingPage "73" @default.
• W2556281736 abstract "To examine the relationship between the chemical composition of light-absorbing organic aerosols and the absorption properties of the aerosols, daily PM2.5 samples were collected during winter at an urban site of Gwangju, Korea, and analyzed for organic carbon and elemental carbon (OC and EC), water-soluble organic carbon (WSOC), humic-like substances (HULIS), and water-soluble inorganic substances. The real-time black carbon (BC) concentration in PM2.5 was also measured using a dual-spot aethalometer. During the study period, average WSOC/OC and HULIS-C/WSOC ratios were 0.53 and 0.52, respectively. K+/EC and K+/OC ratios indicate that biomass burning (BB) emissions are a possible source of the observed carbonaceous aerosols and K+. Moderate-to-strong correlations of HULIS with NO3−, oxalate, SO42 −, K+, CO, and ΔBC (= BC@370 nm − BC@880 nm) suggest that in addition to the primary BB emissions, secondary processing is another important contributor to the formation of HULIS in winter at the site. The average absorption Ångstrӧm exponent (α) of fine aerosols for the wavelengths of 370–950 nm and 590–950 nm was 1.29 and 1.18, respectively, but the aerosol α value was higher in the near UV wavelength range (370–520 nm), with an average of 1.51 (0.76–2.36), indicating that aerosol absorption characteristics during winter were influenced by BB aerosol sources, as well as by traffic emissions. Over the study period, the α370–520 nm value during the highest EC, highest OC, and Asian dust events was 1.42 ± 0.10 (1.26–1.59), 1.44 ± 0.15 (1.16–1.68), and 1.90 ± 0.28 (1.54–2.36), respectively. Higher α370–520 nm values during the Asian dust event were attributed to the influence of dust particles. In addition, the light absorption coefficients of aerosols at 370 nm were strongly correlated with OC (R2 = 0.76), water-insoluble OC (R2 = 0.70), and water-soluble HULIS (R2 = 0.64). These tight correlations suggest that water-insoluble fractions of OC, as well as the water-soluble brown carbon, could be important contributors to aerosol light absorption. This study demonstrates that a newly-developed dual-spot aethalometer could be utilized to characterize light absorption properties of organic aerosols and dust particles." @default.
• W2556281736 created "2016-11-30" @default.
• W2556281736 creator A5018886501 @default.
• W2556281736 creator A5052451680 @default.
• W2556281736 date "2017-03-01" @default.
• W2556281736 modified "2023-09-26" @default.
• W2556281736 title "Relationship between carbonaceous components and aerosol light absorption during winter at an urban site of Gwangju, Korea" @default.
• W2556281736 cites W1907369419 @default.
• W2556281736 cites W1963957504 @default.
• W2556281736 cites W1966123638 @default.
• W2556281736 cites W1971563001 @default.
• W2556281736 cites W1973465612 @default.
• W2556281736 cites W1977992740 @default.
• W2556281736 cites W1979648709 @default.
• W2556281736 cites W1980038151 @default.
• W2556281736 cites W1982624714 @default.
• W2556281736 cites W1983961531 @default.
• W2556281736 cites W1985293027 @default.
• W2556281736 cites W1992981622 @default.
• W2556281736 cites W2005114907 @default.
• W2556281736 cites W2017959016 @default.
• W2556281736 cites W2023595964 @default.
• W2556281736 cites W2026570524 @default.
• W2556281736 cites W2028830256 @default.
• W2556281736 cites W2028999185 @default.
• W2556281736 cites W2035555288 @default.
• W2556281736 cites W2037181694 @default.
• W2556281736 cites W2038230768 @default.
• W2556281736 cites W2039020884 @default.
• W2556281736 cites W2041028539 @default.
• W2556281736 cites W2044499383 @default.
• W2556281736 cites W2048553701 @default.
• W2556281736 cites W2054459239 @default.
• W2556281736 cites W2060117860 @default.
• W2556281736 cites W2061296883 @default.
• W2556281736 cites W2062684589 @default.
• W2556281736 cites W2066828854 @default.
• W2556281736 cites W2069925249 @default.
• W2556281736 cites W2077426193 @default.
• W2556281736 cites W2080320130 @default.
• W2556281736 cites W2080389570 @default.
• W2556281736 cites W2084107749 @default.
• W2556281736 cites W2084693817 @default.
• W2556281736 cites W2088710710 @default.
• W2556281736 cites W2099852381 @default.
• W2556281736 cites W2103689507 @default.
• W2556281736 cites W2104542221 @default.
• W2556281736 cites W2105668460 @default.
• W2556281736 cites W2106161186 @default.
• W2556281736 cites W2106163623 @default.
• W2556281736 cites W2107996035 @default.
• W2556281736 cites W2110596142 @default.
• W2556281736 cites W2113003851 @default.
• W2556281736 cites W2117827600 @default.
• W2556281736 cites W2118451559 @default.
• W2556281736 cites W2128144672 @default.
• W2556281736 cites W2130042267 @default.
• W2556281736 cites W2130969229 @default.
• W2556281736 cites W2131143916 @default.
• W2556281736 cites W2131562297 @default.
• W2556281736 cites W2131722586 @default.
• W2556281736 cites W2132436820 @default.
• W2556281736 cites W2133544629 @default.
• W2556281736 cites W2138673550 @default.
• W2556281736 cites W2145442232 @default.
• W2556281736 cites W2148674484 @default.
• W2556281736 cites W2153571463 @default.
• W2556281736 cites W2156913934 @default.
• W2556281736 cites W2157155949 @default.
• W2556281736 cites W2158718341 @default.
• W2556281736 cites W2162214076 @default.
• W2556281736 cites W2164304376 @default.
• W2556281736 cites W2166809452 @default.
• W2556281736 cites W2168354226 @default.
• W2556281736 cites W2176867834 @default.
• W2556281736 cites W2177030578 @default.
• W2556281736 cites W2198926240 @default.
• W2556281736 cites W2229026040 @default.
• W2556281736 cites W2297822143 @default.
• W2556281736 cites W2327098554 @default.
• W2556281736 cites W2329080388 @default.
• W2556281736 cites W2335248124 @default.
• W2556281736 cites W2338146787 @default.
• W2556281736 cites W2341505721 @default.
• W2556281736 cites W2404916334 @default.
• W2556281736 cites W783510035 @default.
• W2556281736 doi "https://doi.org/10.1016/j.atmosres.2016.11.005" @default.
• W2556281736 hasPublicationYear "2017" @default.
• W2556281736 type Work @default.
• W2556281736 sameAs 2556281736 @default.
• W2556281736 citedByCount "32" @default.
• W2556281736 countsByYear W25562817362017 @default.
• W2556281736 countsByYear W25562817362018 @default.
• W2556281736 countsByYear W25562817362019 @default.
• W2556281736 countsByYear W25562817362020 @default.
• W2556281736 countsByYear W25562817362021 @default.
• W2556281736 countsByYear W25562817362022 @default.
• W2556281736 countsByYear W25562817362023 @default.

• next