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Skip to Search Results- 2Fort Saskatchewan
- 2Ground thermal regime
- 2Phosphogypsum tailing
- 2Seasonally frozen soils
- 2Snowmelt infiltration
- 2Water and heat dynamics
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In situ measurement of snowmelt infiltrationunder various topsoil cap thicknesses on a reclaimed site.
Download2013
Christensen, A. F., Dyck, M. F., Turner, L. E., Chanasyk, D. S., Naeth, M. A., He, H., Nichol, C.
Understanding the soil and climatic conditions affecting the partitioning of snowmelt to runoff and infiltration during spring snow ablation is a requisite for water resources management and environmental risk assessment in cold semi-arid regions. Soil freezing and thawing processes, snowmelt...
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In-situ measurement of snowmelt infiltration under various topsoil cap thicknesses on a reclaimed site.
Download2012
Dyck, M. F., Naeth, M. A., Christensen, A. F., He, H., Chanasyk, D. S., Nichol, C., Turner, L. E.
Understanding the soil and climatic conditions affecting the partitioning of snowmelt to runoff and infiltration during spring snow ablation is a requisite for water resources management and environmental risk assessment in cold semi-arid regions. Soil freezing and thawing processes, snowmelt...
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Scale-dependent covariance of soil physical properties above and below a soil horizon interface: Pedogenic versus anthropogenic influences on total porosity
Download2011
Dyck, M. F., Kachanoski, R. G.
The basic unit of soil – the pedon – is described as the minimum, three-dimensional unit of soil representative of the variability of soil horizon dimensions and morphology. Pedogenic processes responsible for soil horizon and soil profile formation are primarily hydrologic in nature. The...