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Distribution of Chlorinated Hydrocarbon Pesticides and PCBs in the ...

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temperatures rose above 0°C. Our values <strong>of</strong> HCH <strong>in</strong> melted snow<br />

samples <strong>in</strong> June were similar to Patton & a. Is (1988) values for<br />

'toldM snow. The ratio <strong>of</strong> a1pha:gamma-HCH was 1.5 <strong>in</strong> June-<br />

L<strong>in</strong>dane (gamma-HCH) values <strong>in</strong> June were <strong>the</strong> same as <strong>in</strong> <strong>the</strong><br />

previous August/September samples while alpha-HCH, concentrations<br />

were 3 times lower. Reported vapour pressures for <strong>the</strong> two<br />

isomers are similar <strong>and</strong> an <strong>in</strong>crease <strong>in</strong> <strong>the</strong> alpha isomer relative<br />

to <strong>the</strong> gamma isomer would be expected on <strong>the</strong> basis <strong>of</strong> <strong>the</strong> IJV<br />

<strong>in</strong>duced transformation <strong>of</strong> l<strong>in</strong>dane to alpha-HCH. The lower<br />

concentration <strong>of</strong> alpha-HCH <strong>the</strong>refore <strong>in</strong>dicates a mechanism which<br />

produces a more rapid loss <strong>of</strong> alpha-HCH than transformation <strong>of</strong><br />

l<strong>in</strong>dane or is <strong>in</strong>dicative <strong>of</strong> a difference <strong>in</strong> source material <strong>in</strong><br />

1987. Gregor (personal communication) <strong>in</strong>dicated that values for<br />

organochlor<strong>in</strong>es <strong>in</strong> snow samples throughout <strong>the</strong> Canadian ~rctic<br />

were lower <strong>in</strong> 1987 compared to 1986.<br />

HCH concentrations are lower <strong>in</strong> ice than <strong>in</strong> seawater<br />

probably as a result <strong>of</strong> loss through br<strong>in</strong>e explusion dur<strong>in</strong>g <strong>the</strong><br />

w<strong>in</strong>ter.<br />

Concentrations <strong>of</strong> HCH1s measured <strong>in</strong> coastal <strong>and</strong> oceanic<br />

waters have been reviewed by Hard<strong>in</strong>g (1986). HCH isomer5 are<br />

<strong>the</strong> most water soluble <strong>of</strong> <strong>the</strong> organochlor<strong>in</strong>es monitored (Table<br />

5.1) <strong>and</strong> this property along with <strong>the</strong>ir abundance <strong>in</strong> air is<br />

reflected <strong>in</strong> high levels <strong>of</strong> <strong>the</strong>se compounds <strong>in</strong> seawater. ~evels<br />

<strong>of</strong> aipha <strong>and</strong> gamma-HCH > 10 ng L-l occur <strong>in</strong> some coastal waters<br />

near urban areas but values for oceanic surface waters are up to<br />

an order-<strong>of</strong>-magnitude lower. Concentrations for C-HCH <strong>in</strong> <strong>the</strong> NW<br />

Pacific <strong>and</strong> Ber<strong>in</strong>g Sea (1.3 <strong>and</strong> 7.3 ng L-I) span <strong>the</strong> range <strong>of</strong><br />

values observed at <strong>the</strong> Ice Isl<strong>and</strong> (5.1 + 0.5 ng L-I) (Table 4 -51<br />

Concentrations <strong>of</strong> alpha-HCH <strong>and</strong> gamma-HCH <strong>of</strong> 7.1 <strong>and</strong> 0.8 r , g L-'<br />

reported from 10 m depth <strong>in</strong> samples collected from <strong>the</strong> Ice :$l<strong>and</strong><br />

<strong>in</strong> June 1987 (Patton & d. 1988) are about 40% higher than<br />

average values for <strong>the</strong> mixed layer we measured <strong>in</strong> June 1986 [Table<br />

4.5) . Differences <strong>in</strong> extraction methods used <strong>in</strong> each stud1 must<br />

account for this variance.<br />

There is a large reservoir <strong>of</strong> HCH <strong>in</strong> Arctic s~zface<br />

water. Assum<strong>in</strong>g a surface area <strong>of</strong> 1.3 x 1013m2 <strong>and</strong> an average 5

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