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Biogenic and anthropogenic carbonaceous aerosols and their precursors within a forest canopy

Technical Report ·
OSTI ID:7009633
The purpose of this study is to explore the use of thermal evolution techniques, /sup 14/C and /sup 13/C isotopic measurements, and allied approaches for distinguishing carbonaceous aerosol source terms using new data acquired in a forest canopy study - POLlutant - TERpene CAnopy Interaction STudy (POLTERCAIST) - conducted using instrumented towers near Oak Ridge, TN, July 1983 and March 1984. A thermal evolution technique is used to differentiate organic from elemental carbon in aerosol samples. Carbon-14 measurements using gas proportional counting are used to distinguish biogenic carbon (equilibrated with atmospheric /sup 14/CO/sub 2/) from anthropogenic carbon, the latter overwhelmingly fossil fuel-derived and thence containing no /sup 14/C (half-life approx. = 5800 yr). /sup 13/C//sup 12/C isotopic ratios are measured to correct for fractionation but also allow differentiation of C4 and C3 plant material, e.g. slash-burning of crop residues from wood-burning sources. Previous data from a weekly sample taken at the BNL site on Long Island, NY and from a composite sample taken at Barrow, AK (March 1981), indicate about 30% biogenic sources with /sup 13/C//sup 12/C ratios appropriate for a mix of wood-burning and fossil fuel sources. 31 references, 2 figures, 3 tables.
Research Organization:
Brookhaven National Lab., Upton, NY (USA)
DOE Contract Number:
AC02-76CH00016
OSTI ID:
7009633
Report Number(s):
BNL-34740; CONF-840612-7; ON: DE84011845
Country of Publication:
United States
Language:
English