Due to long equilibration times, growth of planktonic organisms significantly dilutes cell concentrations of adsorbed highly hydrophobic organic compounds (HOCs). Behavior of polychlorinated biphenyls (PCBs) in field samples of 0.2−2, 2−25, and >100 μm particle size fractions confirmed this. The in-situ log K oc values showed a near linear relationship with hydrophobicity (log K ow ) with a slope of 1.2 for the 0.2−2 μm size fraction, whereas the in-situ log K oc values remained within 1 log unit throughout the entire log K ow interval for the 2−25 μm size fraction. In the largest size fraction, there was a weak positive relationship between log K oc and log K ow with a linear regression slope of 0.28. The results imply that equilibrium concentrations in planktonic organisms cannot be used in food chain modeling. Observed high equilibrium log K oc values relative to log K ow values are discussed in terms of solute−solvent interactions in the octanol−water system as opposed to the organic carbon−water system in the field.
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Axelman et al. (1997) studied this question.
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