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MARINE RISK ASSESSMENT<br />

sediment, <strong>for</strong> example in the sediment fraction of particles < 63 µm. The organic carbon content<br />

of this fraction is typically 15-30% <strong>for</strong> marine sediment while <strong>for</strong> whole marine sediments it is<br />

generally less than 2%. It is important, <strong>for</strong> reasons of comparability of PEC <strong>and</strong> PNEC values,<br />

that the organic carbon content of sediment used <strong>for</strong> toxicity tests are comparable with those of<br />

actual marine sediments. If not there are likely to be concerns regarding the relative<br />

bioavailability of a substance in the different sediments.<br />

4.3.2.3 Calculations of PNEC <strong>for</strong> marine sediment using the equilibrium method<br />

In the absence of any ecotoxicological data <strong>for</strong> sediment-dwelling organisms, but with measured<br />

data to predict the PECmarine sediment, the PNECmarine sediment may provisionally be calculated using<br />

the equilibrium partitioning method. This method uses the PNECsaltwater <strong>for</strong> aquatic organisms<br />

<strong>and</strong> the marine suspended matter/water partitioning coefficient. The assumptions that are made<br />

in this method are described in Section 3.5.3. Based on the equilibrium partitioning the following<br />

equation is applied:<br />

Explanation of symbols<br />

K susp−water<br />

PNEC marine−se<br />

dim ent = ⋅ PNECsaltwater<br />

⋅1000<br />

(88)<br />

RHO<br />

susp<br />

PNECsaltwater Predicted No Effect Concentration in saltwater [mg . l -1 ]<br />

RHOsusp bulk density of suspended matter [kg . m -3 ] eq. (18)<br />

Ksusp water partition coefficient suspended matter water [m 3. m -3 ] eq. (24)<br />

PNECmarine sediment Predicted No Effect Concentration in marine sediment [mg . kg -1 ]<br />

In Section 3.5.2 a remark is made with respect to the calculation of PNECmarine sediment using the<br />

equilibrium partitioning method. The equilibrium partitioning method considers uptake via the<br />

water phase, while uptake may also occur via other exposure pathways such as ingestion of<br />

sediment or direct contact with sediment. This may be important, especially <strong>for</strong> chemicals that<br />

have a tendency to adsorb to sediment organic matter, <strong>for</strong> example those with a log Kow greater<br />

than 3. Direct uptake from marine sediment is also observed in studies with marine benthic<br />

organisms <strong>and</strong> may significantly contribute to the uptake of organic contaminants such as PAHs<br />

(Kaag, 1998). There is also however evidence from studies in soil <strong>and</strong> in marine sediment that<br />

the proportion of the total dose taken up through intake of sediment particles remains low <strong>for</strong><br />

chemicals with a log Kow up to 5. From other studies it is obvious that feeding mode also<br />

influences uptake of substances (via water or ingestion of sediment). Furthermore the absorption<br />

of contaminants in the gastrointestinal tract has been found to be increased compared with<br />

absorption from the surrounding water (Mayer et al., 1996; Voparil <strong>and</strong> Mayer, 2000). However,<br />

no quantitative conclusions can be drawn from these studies regarding uptake of substances from<br />

sediment.<br />

For substances with a log Kow greater than 5 (or with a corresponding Kpsed) the equilibrium<br />

partitioning method is used in a modified way in order to take account of possible uptake via<br />

ingestion of sediment. Thus the resulting PEC/PNEC ratio is increased by a factor of 10 <strong>for</strong> these<br />

compounds. It should be borne in mind that this approach is considered as a screening level<br />

assessment of the risk to sediment dwelling organisms. If with this method a PEC/PNEC ratio ><br />

1 is derived then tests, preferably long-term, with benthic organisms using spiked sediment have<br />

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