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The chemistry, mineralogy, and rates of transport of sediments in the ...

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40<br />

TABLE 4 . Laboratory estimates <strong>of</strong> <strong>the</strong> rate <strong>of</strong> 0 2 consumption<br />

by <strong>sediments</strong> from <strong>the</strong> Harris River . Experiments were<br />

done <strong>in</strong> triplicate at room temperature (20-22 °C .) <strong>in</strong><br />

shaken, sealed bottles <strong>in</strong> <strong>the</strong> dark . Air-bubbled<br />

W<strong>in</strong>nipeg tap water was used . Control bottles (with<br />

no sediment added) were used <strong>in</strong> <strong>the</strong> calculation . <strong>The</strong><br />

Harris River bank sediment conta<strong>in</strong>ed 2 .5 mMoles <strong>of</strong>organic<br />

carbon per gram <strong>of</strong> dry sediment .<br />

Concentration <strong>of</strong><br />

Added Sediment<br />

Duration <strong>of</strong><br />

Incubation<br />

(hr~f -<br />

02 Consumption<br />

(per gram <strong>of</strong><br />

sediment per day)<br />

7 .41 g L-1 16 0 .34 mg 02 9 - lday-1<br />

3 .32 60 1 .1<br />

I<br />

4 .86 60 0 .33<br />

3 .97 60 0 .60

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