Fracture effects in the shallow groundwater zone in weathered Sarnia-area clay

The Sarnia area of southwestern Ontario is underlain by thick deposits of clay-rich glacial till. From ground surface to between 4 and 6 m depth the clay till is fractured, oxidized, and penetrated by root holes. The water table fluctuates seasonally between the ground surface and the bottom of the...

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Veröffentlicht in:	Canadian geotechnical journal 1989-02, Vol.26 (1), p.43-56
Hauptverfasser:	D'Astous, A. Y, Ruland, W. W, Bruce, J. R. G, Cherry, J. A, Gillham, R. W
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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