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Environmental Health Criteria 214

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HUMAN EXPOSURE ASSESSMENT<br />

Air dermal contact inhalation<br />

Tap water dermal contact ingestion<br />

Food and beverages ingestion<br />

Surface soil dermal contact ingestion<br />

Surface water dermal contact ingestion<br />

6.5.1 Inter-media transfer factors<br />

Transfer of contaminants between media is commonly modelled as<br />

partitioning of a chemical between two or more media. Thus,<br />

multiple-pathway models require the measurement or estimation of<br />

partition coefficients of contaminants between several pairs of<br />

environmental media. There are two general classes of partitioning<br />

coefficients. The first class relies on basic physicochemical<br />

properties of the compounds of interest such as aqueous solubility,<br />

vapour pressure and dipole moment; they describe partitioning due to<br />

diffusive processes. Coefficients in the second class describe<br />

partitioning resulting from what may be considered advective<br />

processes, but also implicitly include diffusive partitioning.<br />

6.5.1.1 Diffusive partition coefficients<br />

The class of diffusive partition coefficients includes those<br />

between soil and water in soil (e.g., groundwater), air and plants,<br />

soil and plants, animal intake and food, surface water and fish,<br />

mother's uptake and breast milk, residential water and indoor air,<br />

soil-gas and indoor air, human skin and soil, and human skin and<br />

water. In many cases, partition coefficients developed from<br />

laboratory-scale experiments are the basis for modelling partitioning<br />

of a compound between environmental media (Lyman et al., 1990). For<br />

example, the octanol-water partition coefficient is often used as a<br />

proxy for partitioning non-polar organic compounds (e.g.,<br />

organochlorine substances) between water and fish lipids. In this<br />

case, n-octanol is considered a good model for fish lipids.<br />

Similarly, the organic carbon-water partition coefficient is used to<br />

characterize partitioning of non-polar substances between organic<br />

matter in soil and water. Finally, Henry's constant describes<br />

partitioning of volatile and non-volatile compounds between air and<br />

water. Connell et al. (1997) provide a comprehensive introduction to<br />

the use of this type of partition coefficient in environmental science<br />

and exposure assessment.<br />

6.5.1.2 Advective partition coefficients<br />

The second class of partitioning coefficients jointly describe<br />

bulk transfer of compounds from one medium to another and diffusive<br />

partitioning. They are often used to model active uptake of<br />

contaminants by animals, principally livestock and game such as fish<br />

or fowl. Factors of this type are used to model transfer of<br />

semi-volatile compounds (SVOCs) such as dioxins from air to soil, soil<br />

to beef and soil to cow's milk (e.g., Nessel et al., 1991; Fries,<br />

1995). Bioaccumulation of lipophilic compounds and some forms of heavy<br />

metals (e.g., methylmercury) in fish from ingestion of contaminated<br />

prey and diffusive uptake through respiration is also modelled using<br />

http://www.inchem.org/documents/ehc/ehc/ehc<strong>214</strong>.htm<br />

Page 102 of 284<br />

6/1/2007

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