Patterns of water movement on a logged Gray Luvisolic hillslope during the snowmelt period

Hillslope flow processes during the snowmelt period were studied at a logged site in the Boreal Plain Ecozone of western Canada. Fine-textured subsoils of Gray Luvisolic soils and soil frost were hypothesized to reduce infiltration capacity and promote interflow. Liquid soil water content, saturated...

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Veröffentlicht in:	Canadian journal of soil science 2004-02, Vol.84 (1), p.71-82
Hauptverfasser:	Whitson, I.R, Chanasyk, D.S, Prepas, E.E
Format:	Artikel
Sprache:	eng
Schlagworte:	collectors frost Luvisols mineral soils saturated conditions saturated flow snow snowmelt soil temperature soil water soil water content subsurface flow thermocouples time domain reflectometry
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