Certain implications are discussed of the data in a recent report of a
tmospheric deposition rates to the Great Lakes by Hoff et al. (Atmosph
eric Environment 30, 3505-3527, 1996). An analysis of the data suggest
s that for many persistent, volatile organic chemicals concentrations
in water are close to a state of long term (several years, within a fa
ctor of approximately five) equilibrium with the atmosphere, but are i
n a constant state of short-term seasonal adjustment. Under these near
-equilibrium conditions the actual magnitude of air to water loadings
become relatively unimportant as determinants of lake ecosystem contam
ination, and the significance of land-based loadings is reduced. Succe
ss in decontaminating or restoring the Great Lakes is becoming increas
ingly dependent on atmospheric concentrations and thus on the processe
s which determine these concentrations. (C) 1997 Elsevier Science Ltd.