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

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TABLE 14 . Mean concentrations <strong>of</strong> selected major <strong>and</strong> m<strong>in</strong>or elements <strong>in</strong> suspended <strong>sediments</strong>, <strong>and</strong> mean<br />

annual rate <strong>of</strong> transp ort <strong>of</strong> <strong>the</strong>se elements <strong>in</strong> particulate material from selected Mackenzie<br />

Valley watersheds . I'Xw = mean rate <strong>of</strong> <strong>transport</strong> <strong>of</strong> element X <strong>in</strong> particulate phase, per<br />

unit watershed area per year, <strong>in</strong> 10 3 Moles km-2 yr - l . PX,j - mean concentration <strong>of</strong> element<br />

X <strong>in</strong> particulate phase per gram dry weight <strong>of</strong> suspended sediment, <strong>in</strong> moles g-1 . <strong>The</strong>se .<br />

data are based on small numbers <strong>of</strong> analyses for <strong>the</strong> elements (1-4 measurementsfelement)<br />

<strong>and</strong> large numbers <strong>of</strong> suspended sediment determ<strong>in</strong>ations (10-40) for each river .<br />

Ca Si Al Cu<br />

River<br />

a ix V a f 1 ; 10 f i PA I x 10 FCu x 10 Muw PZn- x 10 nw<br />

Arctic Red 1 .14* 140 0 .91 1140 2 .59 330 5 .65 0 .07 1 .26 0 .13<br />

Liard (Ft . Liard) 1 .74 74 1 .00 440 2 .50 110 5 .26 0.02 1 .38 0 .06<br />

Liard (Ft . Simpson) 0.94 120 1 .07 1350 2 .75 350 7 .26 0 .09 1 .08 0 .14<br />

Peel 0 .92 82 1 .06 940 2 .88 260 4 .98 0.04 1 .04 0 .09<br />

South Nahanni<br />

(Virg<strong>in</strong>ia Falls) 2 .67 98 1 .21 380 2 .08 76 -- -- - --<br />

Harris -- -- -- -- 17 .0 0.0008 3 .43 0 .004<br />

1<br />

Z st<strong>and</strong>ard deviation<br />

<strong>of</strong> mean annual concentrations<br />

for 1971-73 .<br />

50 38 14 55 51<br />

* <strong>The</strong> mean concentration <strong>of</strong> Ca <strong>in</strong> particulate phase Is 1 .14 x 10-3 Moles per gram dry weight (110°)<br />

<strong>of</strong> suspended sediment .<br />

L L

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