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Determination of octanol–air partition coefficients and supercooled liquid vapor pressures of PAHs as a function of temperature: Application to gas–particle partitioning in an urban atmosphere
Octanol–air partition coefficients ( K OA) for 14 polycyclic aromatic hydrocarbons (PAHs) were determined as a function of temperature using the gas chromatographic retention time method. log K OA values at 25° ranged over six orders of magnitude, between 6.34 (acenaphthylene) and 12.59 (dibenz[ a,h...
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Published in: | Atmospheric environment (1994) 2006-11, Vol.40 (34), p.6615-6625 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Octanol–air partition coefficients (
K
OA) for 14 polycyclic aromatic hydrocarbons (PAHs) were determined as a function of temperature using the gas chromatographic retention time method. log
K
OA values at 25° ranged over six orders of magnitude, between 6.34 (acenaphthylene) and 12.59 (dibenz[
a,h]anthracene). The determined
K
OA values were within factor of 0.7 (dibenz[
a,h]anthracene) to 15.1 (benz[
a]anthracene) of values calculated as the ratio of octanol–water partition coefficient to dimensionless Henry's law constant. Supercooled liquid vapor pressures (
P
L) of 13 PAHs were also determined using the gas chromatographic retention time technique. Activity coefficients in octanol calculated using
K
OA and
P
L ranged between 3.2 and 6.2 indicating near-ideal solution behavior.
Atmospheric concentrations measured in this study in Izmir, Turkey were used to investigate the partitioning of PAHs between particle and gas-phases. Experimental gas–particle partition coefficients (
K
p) were compared to the predictions of
K
OA absorption and
K
SA (soot–air partition coefficient) models. Octanol-based absorptive partitioning model predicted lower partition coefficients especially for relatively volatile PAHs. Ratios of measured/modeled partition coefficients ranged between 1.1 and 15.5 (4.5±6.0, average±SD) for
K
OA model.
K
SA model predictions were relatively better and measured to modeled ratios ranged between 0.6 and 5.6 (2.3±2.7, average±SD). |
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ISSN: | 1352-2310 1873-2844 |
DOI: | 10.1016/j.atmosenv.2006.05.051 |