Article ID Journal Published Year Pages File Type
4443612 Atmospheric Environment 2006 11 Pages PDF
Abstract
Mathematical simulations of the changing equilibrium between particle and gas SVOCs during air sampling show that, in the absence of other artefacts, partition coefficients based on 24-h samples will match those in air at the end of the sampling period under warm conditions as well as cool conditions for the more volatile SVOCs. However, to reflect the average conditions of the sampling period, 24-h samples should be started near one of the two times that the average daily temperature occurs. If conditions are such that the equilibration needs of the collected particles cannot be met at all times during the sampling period, samples should be started at the morning occurrence of the average temperature. For the conditions in a mid-latitude urban area simulated in this study, 24-h samples started in early morning can yield temperature-induced blow-on and blow-off errors in estimated partition coefficients of up to 0.4 log Kp units.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Atmospheric Science
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