The time trend of
α- and γ-hexachlorocyclohexane (HCH)
isomers in Lake Superior water was followed from 1986 to 2016, the
longest record for any persistent organic pollutant (POP) in Great
Lakes water. Dissipation of α-HCH and γ-HCHs was first
order, with halving times (
t
1/2
) of 5.7
and 8.5 y, respectively. Loss rates were not significantly different
starting a decade later (1996–2016). Concentrations of β-HCH
were followed from 1996–2016 and dissipated more slowly (
t
1/2
= 16 y). In 1986, the lake contained an
estimated 98.8 tonnes of α-HCH and 13.2 tonnes of γ-HCH;
by 2016, only 2.7% and 7.9% of 1986 quantities remained. Halving times
of both isomers in water were longer than those reported in air, and
for γ-HCH, they were longer in water than those reported in
lake trout. Microbial degradation was evident by enantioselective
depletion of (+)α-HCH, which increased from 1996 to 2011. Volatilization
was the main removal process for both isomers, followed by degradation
(hydrolytic and microbial) and outflow through the St. Mary’s
River. Sedimentation was minor. Major uncertainties in quantifying
removal processes were in the two-film model for predicting volatilization
and in microbial degradation rates. The study highlights the value
of long-term monitoring of chemicals in water to interpreting removal
processes and trends in biota.