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ENVIRONMENTAL EXPOSURE ASSESSMENT<br />

The area fractions <strong>for</strong> water <strong>and</strong> <strong>for</strong> natural, agricultural <strong>and</strong> industrial/urban soils, are average<br />

values obtained from ECETOC (1994b), supplemented with data received from Sweden <strong>and</strong><br />

Finl<strong>and</strong>. Data <strong>for</strong> Norway <strong>and</strong> Austria are obtained from the FAO statistical databases<br />

(http://apps.fao.org/). The residence time <strong>for</strong> air (defined as the time between air entering <strong>and</strong><br />

leaving the region) of 0.7 days is derived from the wind speed of 3 m/s <strong>and</strong> the area of the<br />

region. The residence time of water of 40 days is selected as a reasonable average <strong>for</strong> the<br />

European situation.<br />

The amount of wastewater discharged, is the product of the amount of wastewater<br />

discharged per person equivalent <strong>and</strong> the number of inhabitants of the system. Using a flow<br />

per capita of 200 l .d -1 (equivalent to the value used in the SimpleTreat model, see Table 9)<br />

<strong>and</strong> a population of 20 million, this results in an additional water flow through the model<br />

environment of 4.0 .10 6 m 3 .d -1 . The inflow caused by inflowing riverwater, is 6.5 .10 7 m 3 .d -1 .<br />

In addition to the environmental characteristics of the region, selected intermedia mass transfer<br />

coefficients are required in the multimedia fugacity model to ensure comparability of the<br />

outcome with other models. These transfer coefficients are summarised in Table 13.<br />

Table 13 Intermedia mass transfer coefficients<br />

Parameter Value<br />

air-water interface: air side partial mass transfer coefficient 1.39 . 10 -3 m . s -1<br />

air-water interface: water side partial mass transfer coefficient 1.39 . 10 -5 m . s -1<br />

Aerosol deposition rate 0.001 m . s -1<br />

air-soil interface: air side partial mass transfer coefficient 1.39 . 10 -3 m . s -1<br />

air-soil interface: soilair side partial mass transfer coefficient 5.56 . 10 -6 m . s -1<br />

air-soil interface: soilwater side partial mass transfer coefficient 5.56 . 10 -10 m . s -1<br />

sediment-water interface: water side partial mass transfer coefficient 2.78 . 10 -6 m . s -1<br />

sediment-water interface: pore water side partial mass transfer coefficient 2.78 . 10 -8 m . s -1<br />

net sedimentation rate 3 mm . yr -1<br />

Model parameters <strong>for</strong> the continental concentration<br />

The continental box covers all 15 EU countries <strong>and</strong> Norway <strong>and</strong> similar percentages <strong>for</strong><br />

water <strong>and</strong> natural, agricultural <strong>and</strong> industrial/urban soils as given in Table 14. All other<br />

parameters are similar to the ones given in the preceding tables. Emission estimation to this<br />

continental box should be based on the EU-wide production volume of the substance. The<br />

resulting concentrations in water <strong>and</strong> air must be used as background concentrations (i.e.<br />

concentrations in water or air that enter the system) in the regional model. When the model is<br />

built according to Figure 1 it is assumed that no inflow of the substance into the continental<br />

system takes place. More recent versions of multimedia models do also contain so-called<br />

global scales <strong>for</strong> different temperature regions, <strong>for</strong> instance moderate, tropic <strong>and</strong> arctic (see e.g.<br />

Br<strong>and</strong>es et al., 1996). In this case the continent is embedded in the moderate scale just like the<br />

region is embedded in the continent. The size of the total global scale is that of the northern<br />

hemisphere. The global scales allow <strong>for</strong> a more accurate estimation of continental concentrations<br />

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