Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897277687> ?p ?o ?g. }
- W2897277687 endingPage "1240" @default.
- W2897277687 startingPage "1221" @default.
- W2897277687 abstract "Abstract. In this study, aerosol samples collected at a remote site in the Amazonian rainforest and an urban site in Manaus, Brazil, were investigated on a single-particle basis using a quantitative energy-dispersive electron probe X-ray microanalysis (ED-EPMA). A total of 23 aerosol samples were collected in four size ranges (0.25–0.5, 0.5–1.0, 1.0–2.0, and 2.0–4.0 µm) during the wet season in 2012 at two Amazon basin sites: 10 samples in Manaus, an urban area; and 13 samples at an 80 m high tower, located at the Amazon Tall Tower Observatory (ATTO) site in the middle of the rainforest, 150 km northeast of Manaus. The aerosol particles were classified into nine particle types based on the morphology on the secondary electron images (SEIs) together with the elemental concentrations of 3162 individual particles: (i) secondary organic aerosols (SOA); (ii) ammonium sulfate (AS); (iii) SOA and AS mixtures; (iv) aged mineral dust; (v) reacted sea salts; (vi) primary biological aerosol (PBA); (vii) carbon-rich or elemental carbon (EC) particles, such as soot, tarball, and char; (viii) fly ash; and (ix) heavy metal (HM, such as Fe, Zn, Ni, and Ti)-containing particles. In submicron aerosols collected at the ATTO site, SOA and AS mixture particles were predominant (50 %–94 % in relative abundance) with SOA and ammonium sulfate comprising 73 %–100 %. In supermicron aerosols at the ATTO site, aged mineral dust and sea salts (37 %–70 %) as well as SOA and ammonium sulfate (28 %–58 %) were abundant. PBAs were observed abundantly in the PM2−4 fraction (46 %), and EC and fly ash particles were absent in all size fractions. The analysis of a bulk PM0.25−0.5 aerosol sample from the ATTO site using Raman microspectrometry and attenuated total reflection Fourier-transform infrared spectroscopy (ATR-FTIR) showed that ammonium sulfate, organics, and minerals are the major chemical species, which is consistent with the ED-EPMA results. In the submicron aerosols collected in Manaus, either SOA and ammonium sulfate (17 %–80 %) or EC particles (6 %–78 %) were dominant depending on the samples. In contrast, aged mineral dust, reacted sea salt, PBA, SOA, ammonium sulfate, and EC particles comprised most of the supermicron aerosols collected in Manaus. The SOA, ammonium sulfate, and PBAs were mostly of a biogenic origin from the rainforest, whereas the EC and HM-containing particles were of an anthropogenic origin. Based on the different contents of SOA, ammonium sulfate, and EC particles among the samples collected in Manaus, a considerable influence of the rainforest over the city was observed. Aged mineral dust and reacted sea-salt particles, including mineral dust mixed with sea salts probably during long-range transatlantic transport, were abundant in the supermicron fractions at both sites. Among the aged mineral dust and reacted sea-salt particles, sulfate-containing ones outnumbered those containing nitrates and sulfate + nitrate in the ATTO samples. In contrast, particles containing sulfate + nitrate were comparable in number to particles containing sulfate only in the Manaus samples, indicating the different sources and formation mechanisms of secondary aerosols, i.e., the predominant presence of sulfate at the ATTO site from mostly biogenic emissions and the elevated influences of nitrates from anthropogenic activities at the Manaus site." @default.
- W2897277687 created "2018-10-26" @default.
- W2897277687 creator A5002397251 @default.
- W2897277687 creator A5004314326 @default.
- W2897277687 creator A5014338518 @default.
- W2897277687 creator A5023742352 @default.
- W2897277687 creator A5031583397 @default.
- W2897277687 creator A5033684035 @default.
- W2897277687 creator A5049613671 @default.
- W2897277687 creator A5058815626 @default.
- W2897277687 creator A5070465686 @default.
- W2897277687 creator A5082416286 @default.
- W2897277687 creator A5088279612 @default.
- W2897277687 creator A5090899168 @default.
- W2897277687 date "2019-01-31" @default.
- W2897277687 modified "2023-10-16" @default.
- W2897277687 title "Single-particle characterization of aerosols collected at a remote site in the Amazonian rainforest and an urban site in Manaus, Brazil" @default.
- W2897277687 cites W1482944906 @default.
- W2897277687 cites W1533925427 @default.
- W2897277687 cites W1551950854 @default.
- W2897277687 cites W1665716048 @default.
- W2897277687 cites W1741463987 @default.
- W2897277687 cites W1932223131 @default.
- W2897277687 cites W1966617311 @default.
- W2897277687 cites W1972384340 @default.
- W2897277687 cites W1973733962 @default.
- W2897277687 cites W1976333725 @default.
- W2897277687 cites W1985036498 @default.
- W2897277687 cites W1999531617 @default.
- W2897277687 cites W2001897543 @default.
- W2897277687 cites W2002564429 @default.
- W2897277687 cites W2002577066 @default.
- W2897277687 cites W2008946624 @default.
- W2897277687 cites W2009209364 @default.
- W2897277687 cites W2017566509 @default.
- W2897277687 cites W2023380448 @default.
- W2897277687 cites W2029157867 @default.
- W2897277687 cites W2031040246 @default.
- W2897277687 cites W2032587168 @default.
- W2897277687 cites W2036017094 @default.
- W2897277687 cites W2036489038 @default.
- W2897277687 cites W2037761347 @default.
- W2897277687 cites W2043339911 @default.
- W2897277687 cites W2047942032 @default.
- W2897277687 cites W2050818795 @default.
- W2897277687 cites W2055337218 @default.
- W2897277687 cites W2062171611 @default.
- W2897277687 cites W2062684589 @default.
- W2897277687 cites W2062762388 @default.
- W2897277687 cites W2063987765 @default.
- W2897277687 cites W2065449930 @default.
- W2897277687 cites W2065623307 @default.
- W2897277687 cites W2067944069 @default.
- W2897277687 cites W2069254477 @default.
- W2897277687 cites W2069893215 @default.
- W2897277687 cites W2074296323 @default.
- W2897277687 cites W2075507236 @default.
- W2897277687 cites W2084780196 @default.
- W2897277687 cites W2093850590 @default.
- W2897277687 cites W2096190218 @default.
- W2897277687 cites W2104231037 @default.
- W2897277687 cites W2105080505 @default.
- W2897277687 cites W2108369371 @default.
- W2897277687 cites W2116507044 @default.
- W2897277687 cites W2123349141 @default.
- W2897277687 cites W2127702924 @default.
- W2897277687 cites W2130886472 @default.
- W2897277687 cites W2131152032 @default.
- W2897277687 cites W2131283510 @default.
- W2897277687 cites W2132006389 @default.
- W2897277687 cites W2132436820 @default.
- W2897277687 cites W2141039410 @default.
- W2897277687 cites W2144923407 @default.
- W2897277687 cites W2145320782 @default.
- W2897277687 cites W2146815278 @default.
- W2897277687 cites W2149915184 @default.
- W2897277687 cites W2160704419 @default.
- W2897277687 cites W2162923152 @default.
- W2897277687 cites W2163498389 @default.
- W2897277687 cites W2192126173 @default.
- W2897277687 cites W2221393733 @default.
- W2897277687 cites W2307767342 @default.
- W2897277687 cites W2332603821 @default.
- W2897277687 cites W2334249942 @default.
- W2897277687 cites W2335180093 @default.
- W2897277687 cites W2345846299 @default.
- W2897277687 cites W2493908473 @default.
- W2897277687 cites W2518443403 @default.
- W2897277687 cites W2535547627 @default.
- W2897277687 cites W2568189012 @default.
- W2897277687 cites W2586062202 @default.
- W2897277687 cites W2586412290 @default.
- W2897277687 cites W2589323886 @default.
- W2897277687 cites W2742134980 @default.
- W2897277687 cites W2753420673 @default.
- W2897277687 cites W2756472362 @default.
- W2897277687 cites W2774163323 @default.
- W2897277687 cites W2774391179 @default.