Abstract
Parallel air and water samples were taken on lakes Superior, Huron, Erie and Ontario between 1996 and 2000 to determine the occurrence and levels of hexachlorocyclohexanes (HCHs), trans-chlordane (TC), cis-chlordane (CC), dieldrin (DIEL) and the metabolite heptachlor exo-epoxide (HEPX). Concentrations in the water varied greatly among the lakes, but air concentrations were similar, thus resulting fugacity ratios varied by lake and compound. The enantiomer fraction, EF = (+)/[(+) + (−)], was determined for α-HCH, TC, CC and HEPX. Enantioselective degradation of (+)α-HCH was found in water of all the lakes where the depletion was greatest for Lake Superior, which has the longest water residence time. Preferential loss of (+)TC and enrichment of (+)HEPX were found in lakes Superior and Ontario, with similar EFs in both lakes. CC was racemic in Lake Superior and showed depletion of the (+) enantiomer in Lake Ontario. Depletion of (+)α-HCH, (+)TC and enrichment of (+)HEPX was seen in all air samples. CC varied from depletion of the (+) or (−) enantiomer and was racemic in some cases. Higher concentrations of α-HCH in the air over Lake Superior were correlated with less racemic composition, providing evidence of water-to-air exchange. Fugacity ratios for the HCHs approached equilibrium conditions within a factor of 2, with slight excursions toward net volatilization or deposition, where generally higher excursions were seen for the cyclodienes.
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