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  • 1
    Publication Date: 2014-11-18
    Description: Atmospheric aerosol samples were collected over the Southern Ocean (SO) and coastal East Antarctica (CEA) during the austral summer of 2010/11. Samples were analysed for trace elements, including Na, Mg, K, Al, Fe, Mn, Ni, Cd and Se, by inductively coupled plasma mass spectrometry (ICP-MS). The mean atmospheric concentrations over the SO were 1100 ng m −3 for Na, 190 ng m −3 for Mg, 150 ng m −3 for Al, 14 ng m −3 for Fe, 0.46 ng m −3 for Mn and 0.25 ng m −3 for Se. Over CEA, the mean concentrations were 990 ng m −3 for Na, 180 ng m −3 for Mg, 190 ng m −3 for Al, 26 ng m −3 for Fe, 0.70 ng m −3 for Mn and 0.29 ng m −3 for Se. Particle size distributions, enrichment factors (EFs) and correlation analysis indicate that Na, Mg and K mainly came from the marine source, while Al, Fe and Mn were mainly from the crustal source, which also contributed to Mg and K over CEA. High EFs were associated with Ni, Cd and Se, suggesting likely contributions from mixed sources from the Antarctic continent, long-range transport, marine biogenic emissions and anthropogenic emissions. Sea-salt elements (Na, Mg, K) were mainly accumulated in the coarse mode, and crustal elements (Al, Fe, Mn) presented a bimodal size distribution pattern. Bioactive elements (Fe, Ni, Cd) were enriched in the fine mode, especially with samples collected over the SO, possibly affecting biogeochemical cycles in this oceanic region. Keywords: Southern Ocean; coastal East Antarctica; trace elements; size distribution; sources (Published: 17 November 2014) Citation: Polar Research 2014, 33 , 23973, http://dx.doi.org/10.3402/polar.v33.23973
    Print ISSN: 0800-0395
    Electronic ISSN: 1751-8369
    Topics: Geography , Geosciences
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  • 2
    Publication Date: 2013-11-15
    Description: [1]  To characterize the concentrations and size distributions of water-soluble organic and inorganic aerosol species, including Na + , non-sea-salt sulfate (nss-SO 4 2- ), methane sulfonate (MSA), oxalate and succinate, over the Southern Ocean (SO) and coastal East Antarctica (CEA), bulk and size-segregated aerosols were collected from 40°S, 100°E to 69°S, 76°E and between 69°S, 76°E and 66°S, 110°E during a cruise from November 2010 to March 2011. Results show that sea salt was the major component of the total aerosol mass, accounting for 72% over the SO and 56% over CEA. The average concentrations of nss-SO 4 2- varied from 420 ng m -3 over the SO to 480 ng m -3 over CEA. The concentrations of MSA ranged from 63 to 87 ng m -3 over the SO and from 46 to 170 ng m -3 in CEA. The average concentrations of oxalate were 3.8 ng m -3 over the SO and 2.2 ng m -3 over CEA. The concentrations of formate, acetate, and succinate were lower than those of oxalate. A bimodal size distribution of aerosol mass existed over CEA, peaking at 0.32-0.56 µm and 3.2-5.6 µm. MSA was accumulated in particles of 0.32-0.56 µm over CEA. High chloride depletion was associated with fine-mode particles enriched with nss-SO 4 2- , MSA and oxalate. Higher cation-to-anion and NH 4 + /nss-SO 4 2- ratios in aerosols over CEA compared to that over the SO imply the higher neutralization capacity of the marine atmosphere over CEA.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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  • 3
    Publication Date: 2017-03-25
    Description: To characterize atmospheric dissolved iron over Newark, a large metropolitan city on US east coast, size-segregated (0.056–18 μm in aerodynamic diameter) aerosols were collected in downtown Newark, New Jersey during August to October 2012. Aerosols samples were analyzed for Fe(II) and total dissolved iron (Fe(TD)) by UV/Visible spectroscopy, and water soluble compounds were analyzed by ion chromatograph (IC). Results from this study showed that Fe(II) concentrations were 2.1 ng m−3 (range: 1.2–4.2 ng m−3), Fe(TD) concentrations were 2.4 ng m−3 (range: 1.3–4.9 ng m−3). Dissolved iron (Fe(II) and Fe(TD)) in general appeared as bi-modal size distribution, was mainly accumulated in the fine mode. The highest concentration of dissolved iron displayed in the fine mode, which was associated with high concentrations of sulfate, oxalate and nitrate, suggesting the potential for Fe–acids interactions. Dissolved iron presented positive correlations with sulfate in the coarse mode, and with nitrate in the fine mode, further suggesting the importance of acid processing in aerosol iron solubility. However, as the oxalate concentration was so low, a good correlation between dissolved iron and oxalate in both the fine and coarse mode was not found.
    Electronic ISSN: 2073-4433
    Topics: Geosciences
    Published by MDPI Publishing
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