The study of fish concentrations and sediment inventories in 19 European hi
gh mountain lakes (40-67 degreesN) shows that a fraction of organochlorine
compounds (OCs), the less volatile compounds (LVC; subcooled liquid vapor p
ressure less than or equal to 10(-2.5) Pa), are trapped in the higher locat
ions. This general trend is not significantly influenced by possible local
sources. Compound distribution is related to average air temperatures. The
phase-change pseudoenthalpies calculated from the sediment inventories clos
ely match the summed theoretical volatilization and dissolution enthalpies.
This fractionation effect is responsible for the accumulation of high conc
entrations of the LVC, the more persistent and toxic according to literatur
e data, in organisms inhabiting sites far from the locations of synthesis o
r use.