TY - JOUR
T1 - Chemical characterisation of marine aerosol at Amsterdam Island during the austral summer of 2006-2007
AU - Claeys, M.
AU - Wang, W.
AU - Vermeylen, R.
AU - Kourtchev, I.
AU - Chi, X.
AU - Farhat, Y.
AU - Surratt, J.D.
AU - Gómez-González, Y.
AU - Sciare, J.
AU - Maenhaut, W.
PY - 2010/1
Y1 - 2010/1
N2 - Atmospheric aerosols were collected in separate fine (<2.5 μm) and coarse (>2.5 μm) size fractions in the period December 2006–March 2007 at Amsterdam Island in the southern Indian Ocean. A major objective of the study was to assess biogenic impact on the marine aerosol. The samples were analysed for organic carbon, water-soluble organic carbon, major inorganic ionic species, and organic species, including methanesulphonate (MSA), dicarboxylic acids, and organosulphates. The concentrations of sea salt, non-sea-salt sulphate, and water-soluble and water-insoluble organic matter (WSOM and WIOM) were estimated. Sea salt dominated the composition of the aerosol and accounted for 83% and 91% of the sum of the mass of the four aerosol types in the fine and coarse size fractions, respectively. WSOM, which can serve as a proxy for biogenic secondary organic aerosol (SOA), accounted for only 2.8% of the sum of the mass of the four aerosol types in the fine size fraction. MSA was the dominating organic compound with a median concentration of 47 ng m−3. The organosulphates were characterised as sulphate esters of hydroxyl acids and a dihydroxylaldehyde, which may originate from the oxidation of algal/bacterial unsaturated fatty acid residues. No evidence was found for isoprene SOA.
AB - Atmospheric aerosols were collected in separate fine (<2.5 μm) and coarse (>2.5 μm) size fractions in the period December 2006–March 2007 at Amsterdam Island in the southern Indian Ocean. A major objective of the study was to assess biogenic impact on the marine aerosol. The samples were analysed for organic carbon, water-soluble organic carbon, major inorganic ionic species, and organic species, including methanesulphonate (MSA), dicarboxylic acids, and organosulphates. The concentrations of sea salt, non-sea-salt sulphate, and water-soluble and water-insoluble organic matter (WSOM and WIOM) were estimated. Sea salt dominated the composition of the aerosol and accounted for 83% and 91% of the sum of the mass of the four aerosol types in the fine and coarse size fractions, respectively. WSOM, which can serve as a proxy for biogenic secondary organic aerosol (SOA), accounted for only 2.8% of the sum of the mass of the four aerosol types in the fine size fraction. MSA was the dominating organic compound with a median concentration of 47 ng m−3. The organosulphates were characterised as sulphate esters of hydroxyl acids and a dihydroxylaldehyde, which may originate from the oxidation of algal/bacterial unsaturated fatty acid residues. No evidence was found for isoprene SOA.
KW - Marine aerosols
KW - Water-soluble organic carbon
KW - Secondary organic aerosol
KW - Organosulphates
KW - Isoprene
UR - http://www.scopus.com/inward/record.url?eid=2-s2.0-73649140296&partnerID=MN8TOARS
U2 - 10.1016/j.jaerosci.2009.08.003
DO - 10.1016/j.jaerosci.2009.08.003
M3 - Article
SN - 0021-8502
VL - 41
SP - 13
EP - 22
JO - Journal of Aerosol Science
JF - Journal of Aerosol Science
IS - 1
ER -