Carbonaceous aerosol characterization in the Amazon basin, Brazil: novel dicarboxylic acids and related compounds.

Abstract High-resolution capillary gas chromatography (GC) and GC/mass spectrometry (MS) were employed for the quantitative determination of dichloromethane-extractable organic compounds in total and size-fractionated aerosol samples which were collected in the Amazon basin, Brazil, during the wet season, as part of the LBA–CLAIRE-98 experiment. Special emphasis was placed on the characterization and identification of several novel unknown dicarboxylic acids and related oxidative degradation products. This class of acidic products was enriched in the fine size fraction, suggesting that they were secondary organic aerosol products formed by gas-to-particle conversion. Some of the unknowns contributed more to the class of dicarboxylic acids than the major known compound, nonadioic acid (azelaic acid). The same unknowns were also observed in urban aerosol samples collected on hot summer days in Gent, Belgium. For the characterization and structure elucidation of the unknowns, various types of derivatizations and fractionation by solid-phase extraction were employed in combination with GC/MS. Four unknowns were identified. The most abundant were two derivatives of glutaric acid, 3-isopropyl pentanedioic acid and 3-acetyl pentanedioic acid. The other two identified unknowns were another oxo homologue, 3-acetyl hexanedioic acid, and, interestingly, 3-carboxy heptanedioic acid. To our knowledge, the occurrence of these four compounds in atmospheric aerosols has not yet been reported. The biogenic precursors of the novel identified compounds could not be pinpointed, but most likely include monoterpenes and fatty acids.

[1]  Glen R. Cass,et al.  Quantification of urban organic aerosols at a molecular level: Identification, abundance and seasonal variation , 1993 .

[2]  Glen R. Cass,et al.  Interpretation of High-Resolution Gas Chromatography and High-Resolution Gas Chromatography / Mass Spectrometry Data Acquired from Atmospheric Organic Aerosol Samples , 1989 .

[3]  R. B. Gagosian,et al.  Mid-chain ketocarboxylic acids in the remote marine atmosphere: Distribution patterns and possible formation mechanisms , 1990 .

[4]  E. Stephanou,et al.  Oxocarboxylic and .alpha.,.omega.-dicarboxylic acids: photooxidation products of biogenic unsaturated fatty acids present in urban aerosols , 1993 .

[5]  Glen R. Cass,et al.  SOURCES OF FINE ORGANIC AEROSOL. 3. ROAD DUST, TIRE DEBRIS, AND ORGANOMETALLIC BRAKE LINING DUST: ROADS AS SOURCES AND SINKS , 1993 .

[6]  K. Kawamura,et al.  Seasonal changes in the distribution of dicarboxylic acids in the urban atmosphere , 1993 .

[7]  B. Simoneit,et al.  Characterization of Organic Constituents in Aerosols in Relation to Their rigin and Transport: A Review , 1986 .

[8]  M. Claeys,et al.  Carbonaceous aerosols and particulate organic compounds in Gent, Belgium, during winter and summer of 1998 , 1999 .

[9]  B. Simoneit,et al.  Composition of extractable organic matter of air particles from Malaysia : Initial study , 1996 .

[10]  Glen R. Cass,et al.  Sources of fine organic aerosol. 1. Charbroilers and meat cooking operations , 1991 .

[11]  R. Gagosian,et al.  Implications of ω-oxocarboxylic acids in the remote marine atmosphere for photo-oxidation of unsaturated fatty acids , 1987, Nature.

[12]  S. Koch,et al.  Formation of new particles in the gas phase ozonolysis of monoterpenes , 2000 .

[13]  J. Cafmeyer,et al.  The ''Gent'' stacked filter unit (SFU) sampler for the collection of atmospheric aerosols in two size fractions: Description and instructions for installation and use , 1994 .

[14]  P. Solomon,et al.  High-Volume Dichotomous Virtual Impactor for the Fractionation and Collection of Particles According to Aerodynamic Size , 1983 .

[15]  K. Kawamura,et al.  Identification of 4-oxoheptanedioic acid in the marine atmosphere by capillary gas chromatography-mass spectrometry , 1994 .

[16]  K. Kawamura Identification of C2-C10 .omega.-oxocarboxylic acids, pyruvic acid, and C2-C3 .alpha.-dicarbonyls in wet precipitation and aerosol samples by capillary GC and GC/MS , 1993 .

[17]  M. Hayashi,et al.  Water soluble dicarboxylic acids and related compounds in Antarctic aerosols , 1996 .

[18]  G. Cass,et al.  Sources of Fine Organic Aerosol. 9. Pine, Oak, and Synthetic Log Combustion in Residential Fireplaces , 1998 .

[19]  D. Grosjean,et al.  Identification of C3-C10 aliphatic dicarboxylic acids in airborne particulate matter , 1978 .

[20]  J. Seinfeld,et al.  Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , 1997 .

[21]  A. Limbeck,et al.  Organic acids in continental background aerosols , 1999 .

[22]  L. Barrie,et al.  Production of dicarboxylic acids in the Arctic atmosphere at polar sunrise , 1995 .

[23]  Glen R. Cass,et al.  Quantitative High - Resolution Gas Chromatography and High - Resolution Gas Chromatography/Mass Spectrometry Analyses of Carbonaceous Fine Aerosol Particles , 1987 .

[24]  John H. Seinfeld,et al.  Gas-Phase Ozone Oxidation of Monoterpenes: Gaseous and Particulate Products , 1999 .

[25]  R. Cary,et al.  Elemental Carbon-Based Method for Monitoring Occupational Exposures to Particulate Diesel Exhaust , 1996 .

[26]  B. Simoneit,et al.  Organic Matter of the Troposphere-II. Natural Background of biogenic lipid matter in aerosols over the rural western United States ††Contribution No. 2088: Institute of Geophysics and Planetary Physics, University of California at Los Angeles. , 2007 .

[27]  M. Facchini,et al.  Cloud albedo enhancement by surface-active organic solutes in growing droplets , 1999, Nature.