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3 . LITERATURE REVIEW<br />

Leahey (1947) studied some of the soils along the Mackenzie River<br />

and provided a brief analysis and description of<br />

soil samples from<br />

several locations along the route . Wright et al (1959) discussed the<br />

chemical, morphological and mineralogical characteristics of soils<br />

developed on alluvial deposits near the mouth of the Hay River, N .W .T .<br />

Day (1962) and Day and Rice (1964) provided some information concerning<br />

the characteristics of perennially frozen soils occurring along the<br />

Mackenzie River .<br />

Jeffrey (1964) provided valuable soil information<br />

relating to vegetation types occurring along the lower Liard River .<br />

A reconnaissance soil survey was carried out by Day (1966, 1968) along<br />

the Upper Mackenzie River and the Liard River Valley .<br />

These two<br />

reports provided detailed descriptions of soils and a soil map of an<br />

approximately 6,540,700 acre area along these two rivers .<br />

In the<br />

summer of 1971 Lavkulich (1971) carried out soil, vegetation and<br />

landform studies in the Fort Simpson area in cooperation with<br />

Dr . J .S . Rowe of the University of Saskatchewan, Dr . D .S . Lacate of<br />

the University of British Columbia and Dr . N .W . Rutter of the<br />

Geological Survey of Canada .<br />

Some soil information was provided by<br />

Janz (1971) for the eastern part of the Mackenzie Delta along with a<br />

vegetation study on selected sites . For the interpretation of<br />

organic soils the work of Zoltai and Tarnocai (1971) and Tarnocai<br />

(1970, 1972) was used . For the interpretation of cryoturbed subarctic<br />

and arctic soils, Mackay's work (1958) and papers published<br />

in the book "Soils of Eastern Siberia" edited by E .N . Ivanova,<br />

were found to be most useful .

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