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

被引:54
作者
Mader, BT [1 ]
Pankow, JF [1 ]
机构
[1] Oregon Grad Inst Sci & Technol, Dept Environm Sci & Engn, Portland, OR 97291 USA
关键词
air; sampling; adsorption; artifacts; SOCs;
D O I
10.1016/S1352-2310(00)00398-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 measured particle-phase concentrations, and negative biases in the measured gas-phase concentrations. When quartz fiber filters (QFFs) are used, surface-area-normalized gas/quartz partition coefficient (K-p,K-s, m(3) m(-2)) values 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 aromatic hydrocarbons (PAHs) and n-alkanes. Gas/QFF K-p,K-s values were measured here for a series of polychlorinated dibenzodioxins (PCDDs) and polychlorinated dibenzofurans (PCDFs), and also for a range of PAKs. Within each of 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 log 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 larger for partitioning to clean QFFs at RH = 25% than for TMFs at RH = 21-52%. 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 adsorption 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 using K-p,K-s values that were obtained with ambient backup QFFs. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
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页码:1217 / 1223
页数:7
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