Dc. Ballentine et al., VARIABILITY OF STABLE CARBON ISOTOPIC COMPOSITIONS IN INDIVIDUAL FATTY-ACIDS FROM COMBUSTION OF C4 AND C3 PLANTS - IMPLICATIONS FOR BIOMASSBURNING, Chemical geology, 152(1-2), 1998, pp. 151-161
The isotopic characterization of trace organic species produced during
biomass burning may allow a better understanding of the source and fa
te of combustion-derived organic matter. In order to assess the utilit
y of compound specific isotope analysis (CSIA) of fatty acids as a mea
ns to distinguish the sources of these species in atmospheric aerosols
, the isotopic signatures of fatty acids extracted from unburned C-4 a
nd C-3 vegetation have been determined. Carbon isotopic signatures of
fatty acids from unburned C-4 vegetation ranged from -21.1 parts per t
housand to -28.2 parts per thousand, whereas those from C-3 vegetation
ranged from -32.4 parts per thousand to - 38.5 parts per thousand. Fa
tty acids isolated from aerosols produced during controlled laboratory
burns of C-4 vegetation showed an isotopic depletion of 2 parts per t
housand to 6 parts per thousand relative to those extracted from the u
nburned plant. However, the opposite relationship was observed for C-3
vegetation, with the aerosol fatty acids exhibiting and isotopic enri
chment of 2 parts per thousand to 7 parts per thousand relative to tho
se from the unburned plant. Combustion-derived fatty acids may be dist
inguished from those species that arise from erosion of unburned plant
debris. CSIA of fatty acids produced during field burns of C-4 and C-
3 vegetation suggests that isotopic characterization of these species
in atmospheric aerosols may be useful in determining the fate of organ
ic matter produced during biomass burning. (C) 1998 Elsevier Science B
.V. All rights reserved.