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ENVIRONMENTAL EXPOSURE ASSESSMENT<br />

Another difference is that <strong>for</strong> risk assessment, the availability of high quality test data is required<br />

in virtually all cases <strong>and</strong> further testing may there<strong>for</strong>e be required in the case of low quality data.<br />

In distribution models, calculations are per<strong>for</strong>med <strong>for</strong> compartments each consisting of<br />

homogeneous sub-compartments, i.e. surface water containing dissolved organic carbon <strong>and</strong><br />

suspended matter, sediment containing porewater <strong>and</strong> a solid phase, <strong>and</strong> soil containing air,<br />

porewater <strong>and</strong> a solid phase. Since it is assumed that no degradation takes place in the sorbed<br />

phase, the rate constant <strong>for</strong> the surface water, bulk sediment or soil in principle depends on the<br />

suspended matter/water, sediment/water or soil/water partition coefficient of the substance. With<br />

increasing hydrophobicity (sorption) of the substance, the freely dissolved fraction present in the<br />

water phase available <strong>for</strong> degradation decreases, <strong>and</strong> there<strong>for</strong>e the overall rate constant should<br />

also decrease. However, <strong>for</strong> surface waters the influence of sorption is already comprised in the<br />

degradation rates when they are determined <strong>for</strong> bulk water in simulation tests employing the<br />

same conditions as in the aquatic environment. Neither is it needed to consider the influence of<br />

sorption processes when rate constants are established from screening test results due to the<br />

well-established practice to conclude on biodegradability in the environment from such data.<br />

Also <strong>for</strong> assessment of biodegradation in soil or sediment, data from relevant simulation tests are<br />

preferred. Simulation tests such as the OECD 307 “Aerobic <strong>and</strong> anaerobic trans<strong>for</strong>mation in<br />

soil” (OECD, 2000b; EU Annex V draft C.23) <strong>and</strong> the OECD 308 “Aerobic <strong>and</strong> anaerobic<br />

trans<strong>for</strong>mation in aquatic sediment systems” (OECD, 2000c; EU Annex V draft C.24) are<br />

available. The basis <strong>for</strong> these methods was initially developed <strong>for</strong> pesticides, e.g. guidelines of<br />

BBA (BBA, 1986; BBA, 1990a) <strong>and</strong> US EPA. The draft ISO/DIS 14592-1 st<strong>and</strong>ard includes an<br />

option <strong>for</strong> determination of biodegradability in a surface water/sediment suspension. Of course<br />

this test does not directly simulate the conditions in non-disturbed sediment. The measured halflife<br />

in water/sediment tests may be dependent on the relative volume of water <strong>and</strong> sediment<br />

employed in the test.<br />

When such simulation test data are available, the applicability of the results from the tests should<br />

be evaluated on a case-by-case basis employing expert judgement when used in a risk<br />

assessment.<br />

When no data from tests simulating the conditions in soil or sediment are available, the use of<br />

screening test data may be considered. The <strong>guidance</strong> <strong>for</strong> use of such data is based on the general<br />

recognition that <strong>for</strong> substances with low Kp values at present not enough empirical data are<br />

available to assume some sort of dependence of the soil biodegradation half-life on the<br />

solids/water partition coefficient. Nevertheless, <strong>for</strong> substances with high Kp values there is<br />

evidence that some sort of Kp dependence exists. There<strong>for</strong>e degradation half-life classes <strong>for</strong><br />

(bulk) soil, partly based on Kp are presented in Table 8. If a half-life from a surface water<br />

simulation test is available it may, in a similar manner, <strong>for</strong>m the basis <strong>for</strong> the establishment of a<br />

half-life in soil. The half-lives indicated in the table are considered conservative.<br />

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