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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.
The morphology of the terraces and corresponding stocks of soil material and chemical elements are assessed through a microtopographic study.
Generally, the consequences of soil material damping on the displacement demands are greater than those on the force demands.
In addition, the occurrence of Fe Mn nodules showing a sharp boundary indicates mixing of soil material.
Variations of soil material properties were investigated at four different initial dry bulk densities of 1410, 1520, 1610 and 1670 kg/m3.
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The spatial distribution of soil materials was visualized using a three-dimensional soil layer model.
Domestic animals, however, can have a deleterious impact by trampling and compacting the soil; this activity can reduce the infiltration of water and damage vegetation, leading to erosion and redistribution of soil materials.
We developed a method to create 3-dimensional (3-D) continuous soil layer models describing the distribution of soil materials, reworked loess vs. glacial till.
In young glaciated landscapes the variability of soil materials imparts a major control on crop growth and yield and environmental quality associated with production agriculture.
Silica is also released from silicate minerals during sulfuricization, which can reprecipitate as opal-CT, to cause cementation of soil materials into duripan-like formations.
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