TY - JOUR
T1 - Characterization of organic aerosol in Big Bend National Park, Texas
AU - Brown, Steven G.
AU - Herckes, Pierre
AU - Ashbaugh, Lowell
AU - Hannigan, Michael P.
AU - Kreidenweis, Sonia M.
AU - Collett, Jeffrey L.
N1 - Funding Information: We thank Taehyoung Lee, Eli Sherman, Jill Reilly, and Air Resource Specialists for providing assistance and logistical support before and during the BRAVO field study. We are grateful to William Malm, Marc Pitchford, and other members of the BRAVO science team for helpful comments and suggestions. Support for this BRAVO Study-related work was provided by the National Park Service (contract #CA2350-97-001 T098-07). However, the results, findings, and conclusions expressed in this paper are solely those of the authors and are not necessarily endorsed by the management, sponsors, or collaborators of the BRAVO Study. A comprehensive final report for the BRAVO Study is anticipated in 2002.
PY - 2002/12
Y1 - 2002/12
N2 - The Big Bend Regional Aerosol and Visibility Observational (BRAVO) Study was conducted in Big Bend National Park, Texas, July through October 1999. Daily PM2.5 organic aerosol samples were collected on pre-fired quartz fiber filters. Daily concentrations were too low for detailed organic analysis by gas chromatography-mass spectrometry (GC-MS) and were grouped based on their air mass trajectories. A total of 12 composites, each containing 3-10 daily samples, were analyzed. Alkane carbon preference indices suggest primary biogenic emissions were small contributors to primary PM2.5 organic matter (OM) during the first 3 months, while in October air masses advecting from the north and south were more strongly influenced by biogenic sources. A series of trace organic compounds previously shown to serve as particle phase tracers for various carbonaceous aerosol source types were examined. Molecular tracer species were generally at or below detection limits, except for the wood smoke tracer levoglucosan in one composite, so maximum possible source influences were calculated using the detection limit as an upper bound to the tracer concentration. Wood smoke was found not to contribute significantly to PM2.5 OM, with contributions for most samples at <1% of the total organic particulate matter. Vehicular exhaust also appeared to make only minor contributions, with maximum possible influences calculated to be 1-4% of PM2.5 OM. Several factors indicate that secondary organic aerosol formation was important throughout the study, and may have significantly altered the molecular composition of the aerosol during transport.
AB - The Big Bend Regional Aerosol and Visibility Observational (BRAVO) Study was conducted in Big Bend National Park, Texas, July through October 1999. Daily PM2.5 organic aerosol samples were collected on pre-fired quartz fiber filters. Daily concentrations were too low for detailed organic analysis by gas chromatography-mass spectrometry (GC-MS) and were grouped based on their air mass trajectories. A total of 12 composites, each containing 3-10 daily samples, were analyzed. Alkane carbon preference indices suggest primary biogenic emissions were small contributors to primary PM2.5 organic matter (OM) during the first 3 months, while in October air masses advecting from the north and south were more strongly influenced by biogenic sources. A series of trace organic compounds previously shown to serve as particle phase tracers for various carbonaceous aerosol source types were examined. Molecular tracer species were generally at or below detection limits, except for the wood smoke tracer levoglucosan in one composite, so maximum possible source influences were calculated using the detection limit as an upper bound to the tracer concentration. Wood smoke was found not to contribute significantly to PM2.5 OM, with contributions for most samples at <1% of the total organic particulate matter. Vehicular exhaust also appeared to make only minor contributions, with maximum possible influences calculated to be 1-4% of PM2.5 OM. Several factors indicate that secondary organic aerosol formation was important throughout the study, and may have significantly altered the molecular composition of the aerosol during transport.
KW - BRAVO
KW - Organic aerosol
KW - Source apportionment
KW - Visibility
UR - http://www.scopus.com/inward/record.url?scp=0036882578&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0036882578&partnerID=8YFLogxK
U2 - 10.1016/S1352-2310(02)00578-2
DO - 10.1016/S1352-2310(02)00578-2
M3 - Article
SN - 1352-2310
VL - 36
SP - 5807
EP - 5818
JO - Atmospheric Environment
JF - Atmospheric Environment
IS - 38
ER -