TY - JOUR
T1 - Composition of extractable organic matter of aerosols from the blue mountains and southeast coast of Australia
AU - Simoneit, Bernd R.T.
AU - Crisp, P. T.
AU - Mazurek, M. A.
AU - Standley, L. J.
N1 - Funding Information:
Acknowledgment -- We thank Mrs. Norma Cadet, Packsaddlers Pty. Ltd. and Mr. E.J. Hill for permission to sample, Mrs. E. Crisp for assistance with sampling, Ms. X. Chen for technical assistance and Mr. E. Ruth, Mr. R.N. Leif, and Ms. X. Chen for GC-MS data acquisition. We also thank the National Science Foundation, Atmospheric Research Section (Grants ATM 81-16622, ATM 81-18101, ATM-8509184, and ATM-8717988) for financial support.
PY - 1991
Y1 - 1991
N2 - Extractable organic matter in aerosols from the Australian Blue Mountains and southeastern coast was characterized and compared to a composite sample of the regional vegetation and aerosols collected in New Zealand by Gagosian et al. (1987). The lipid fraction of the aerosols was comprised primarily of n-alkanoic acids, and n-alkanols, with triterpenoids and phytosterols contributing significantly to the signature. Except for one sample, the aerosols were demonstrated to originate mainly from biogenic rather than anthropogenic sources. Two of the aerosol samples correlated well with the n-alkane signature of the plant was extract. The resemblance was less distinct for the n-alkanoic acid and n-alkanol fractions. Of the cyclic terpenoids, only triterpenoids were present in the aerosols. Sesquiterpenoids were found in the plant wax sample but not in the aerosols, most probably due to volatilization. Diterpanes were undetected in both aerosol and wax samples. Based on preliminary comparison, long range transport of these lipids appears to be occurring by the Southern Hemisphere westerlies.
AB - Extractable organic matter in aerosols from the Australian Blue Mountains and southeastern coast was characterized and compared to a composite sample of the regional vegetation and aerosols collected in New Zealand by Gagosian et al. (1987). The lipid fraction of the aerosols was comprised primarily of n-alkanoic acids, and n-alkanols, with triterpenoids and phytosterols contributing significantly to the signature. Except for one sample, the aerosols were demonstrated to originate mainly from biogenic rather than anthropogenic sources. Two of the aerosol samples correlated well with the n-alkane signature of the plant was extract. The resemblance was less distinct for the n-alkanoic acid and n-alkanol fractions. Of the cyclic terpenoids, only triterpenoids were present in the aerosols. Sesquiterpenoids were found in the plant wax sample but not in the aerosols, most probably due to volatilization. Diterpanes were undetected in both aerosol and wax samples. Based on preliminary comparison, long range transport of these lipids appears to be occurring by the Southern Hemisphere westerlies.
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U2 - 10.1016/0160-4120(91)90274-T
DO - 10.1016/0160-4120(91)90274-T
M3 - Article
AN - SCOPUS:0025918958
SN - 0160-4120
VL - 17
SP - 405
EP - 419
JO - Environment international
JF - Environment international
IS - 5
ER -