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

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9<br />

Q<br />

TABLE 16 . A comparison <strong>of</strong> annual <strong>rates</strong> <strong>of</strong> sediment <strong>transport</strong> <strong>in</strong> large <strong>and</strong><br />

small Mackenzie <strong>and</strong> Porcup<strong>in</strong>e River watersheds with o<strong>the</strong>r Arctic,<br />

Subarctic <strong>and</strong> Temperate Zone watersheds . Ad - watershed area <strong>in</strong><br />

km 2 , Q a - annual discharge <strong>in</strong> m3 yr- 1, SSw = annual sediment<br />

<strong>transport</strong> per unit watershed area <strong>in</strong> metric tons km -2 yr-1 . .<br />

I<br />

River Ad Q A<br />

SSw Reference<br />

(km2 ) (m 3 vr-1 ) (metric tons<br />

km- 2 yr" 1)<br />

Yukon, Alaska 955 x 10 3 173 x 109 1n3 Mat<strong>the</strong>ws, 1973<br />

Colville, Alaska 50 x 10 3 16 x In 9 15n Arnborg et al ., 1966, 1967<br />

Chena River, Alaska 5 .1 x 1n 3 -1 .7 x 1n 9 17 Prey et al ., 1970<br />

Mississippi 3 .2 x 10 6 563 x <strong>in</strong>9 85 Ritter, 1967<br />

Colorado 357 x 10 3 -- 378' Ritter, 1967<br />

St . Lawrence 936 x 10 3 315 x 10 9 0 .64 D'Anglejan <strong>and</strong> Smith, 1973<br />

Columbia 265 x 10 3 -- 35 Ritter, 1967<br />

Large Rivers <strong>in</strong><br />

Mackenzie Valley,<br />

Group 1 <strong>in</strong> Table 1 14-1570 x to 3 4-285 x 1n9<br />

36-126 This study<br />

Mackenzie & Peel 1 .-69 x 1n~ 313 x 109 68 This study<br />

Char Lake streams,<br />

Cornwallis Is ., N .W .T . 3 .5 49 x 10 4<br />

,5 .5 de March, 1974, 1975<br />

Hubbard Brook (W6) 0 .13 1n0 1 .n 3 2 .5 Aormann et al ., 1969<br />

Small Rivers <strong>in</strong> Mackenzie<br />

Valley, Croup 2 i n<br />

Table 1<br />

0.4-21 x<br />

W ,<br />

10 3 17-20no x 10 6 0 .17 - 11 .5 This study

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