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Glacial river floodplains are extensive, very dynamic, and constantly renewed with fertile soil material.
The occasional plants growing there often become established in frost cracks that capture blowing snow and finer windblown soil material.
Thus, productive forests often are restricted to portions of the landscape where soil material has been deposited by glaciers.
Combining the sparse soil material data with the dense cone index and landform element data resulted in soil material information covering the entire study area.
Sheet erosion commonly occurs on recently plowed fields or on other sites having poorly consolidated soil material with scant vegetative cover.
Therein, uncertainty in the soil material properties is modelled by non-Gaussian random fields.
Soil material damping properties are estimated through analysis of the field measurements.
Valley and footslope soils showed hydromorphic features and accumulation of soil material from upslope.
The thickness of soil material stored in each terrace is given by DEMst = DEM1 − DEM2.
Generally the outer wall is constructed of hard soil material, distinct from the internal central portion (or nursery), which is composed of softer carton material.
a) organic soil material; b) soil material for constructions.
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