Gas/solid partitioning of semivolatile organic compounds (SOCs) to air filters. 2. Partitioning of polychlorinated dibenzodioxins, polychlorinated dibenzofurans, and polycyclic aromatic hydrocarbons to quartz fiber filters
Bt. Mader et Jf. Pankow, Gas/solid partitioning of semivolatile organic compounds (SOCs) to air filters. 2. Partitioning of polychlorinated dibenzodioxins, polychlorinated dibenzofurans, and polycyclic aromatic hydrocarbons to quartz fiber filters, ATMOS ENVIR, 35(7), 2001, pp. 1217-1223
Gas/particle distributions of atmospheric semi-volatile organic compounds (
SOCs) are often measured using filter/sorbent samplers. Unfortunately, the
adsorption of gaseous SOCs onto a filter can cause positive biases in the m
easured particle-phase concentrations, and negative biases in the measured
gas-phase concentrations. When quartz fiber filters (QFFs) are used, surfac
e-area-normalized gas/quartz partition coefficient (K-p,K-s, m(3) m(-2)) va
lues will be useful when estimating the magnitudes of these errors. Gas/QFF
K-p,K-s values have been reported in the literature only for polycyclic ar
omatic hydrocarbons (PAHs) and n-alkanes. Gas/QFF K-p,K-s values were measu
red here for a series of polychlorinated dibenzodioxins (PCDDs) and polychl
orinated dibenzofurans (PCDFs), and also for a range of PAKs. Within each o
f the three individual compound classes, plots of log K-p,K-s vs. log P-L(o
) (sub-cooled liquid vapor pressure) were found to be linear with slopes of
approximately - 1. At relative humidity (RH) = 25%, the pooled log K-p,K-s
data at 25 degreesC for the three compound classes were correlated with lo
g p(L)(o) nearly as well (r(2) = 0.95) as were the data for the individual
compound classes (r(2) approximate to 0.97). In general, the K-p,K-s values
for the PAHs and PCDD/PCDFs studied were found to be about a factor of 2 l
arger for partitioning to clean QFFs at RH = 25% than for TMFs at RH = 21-5
2%. Backup QFFs used in filter/sorbent sampling in a suburban area yielded
K-p,K-s values for PAHs at RH = 37% that were significantly lower than for
clean QFFs at the same RH. (This may have been the result of the adsorption
of ambient organic compounds that at least partially blocked the direct ad
sorption of the SOCs to the QFF surface). Therefore, when QFFs are used to
separate atmospheric gas- and particle-phase SOCs, corrections for compound
-dependent gas adsorption artifacts for QFFs may need to be carried out usi
ng K-p,K-s values that were obtained with ambient backup QFFs. (C) 2001 Els
evier Science Ltd. All rights reserved.