Annually integrated air concentrations o
f ![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>- and
![](/images/gi<font color=)
fchars/gamma.gi
f" BORDER=0 >-hexachlorocyclohexane (HCH) were determined in 2000/2001 at 40 stations across North America using XAD-based passive air samplers to understand atmosphericdistribution processes on a continental scale. Elevated levelso
f ![](/images/gi<font color=)
fchars/gamma.gi
f" BORDER=0 >-HCH in the atmosphere o
f the Canadian Prairies areconsistent with the ongoing use o
f lindane as a seed treatmenton canola and con
firm the
feasibility o
f detecting theagricultural use o
f a pesticide using long-term integratedpassive air sampling. In contrast to
![](/images/gi<font color=)
fchars/gamma.gi
f" BORDER=0 >-HCH, the atmosphericconcentrations o
f ![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH show a rather uni
form distributionacross Canada and the United States, which is expected
for a chemical with no current use on the continent. Higherlevels in the atmosphere over Atlantic Canada can beexplained by
![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH evaporating
from the waters o
f theLabrador Current, which is supported by the chiral compositiono
f ![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH and the temperature dependence o
f itsatmospheric concentrations along the east coast o
fCanada. Similarly,
![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH is volatilizing
from Lake Superior.Atmospheric HCH levels increase with elevation in theCanadian Rocky Mountains. The results suggest thatevaporation, in particular
from cold water bodies, is animportant source o
f ![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH to the North American atmosphere.Low levels o
f HCHs in Central America hint at e
fficientdegradation under tropical conditions. Chiral analysis showsthat (+)-
![](/images/gi<font color=)
fchars/alpha.gi
f" BORDER=0>-HCH is o
ften enriched in air over continentalareas and at the Paci
fic Coast, which is opposite to theenantiomeric enrichment in the proximity to the Great Lakesand the Atlantic Ocean. Passive air sampling is a power
fultool to discern the large-scale variability o
f semivolatileand persistent organic chemicals in the atmosphere.