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Principal component analysis highlights important axes of textural and mineralogical variation among horizons of these soils, often related to parent material properties.
Because of their sensitivity to parent material properties and soil pH, critical MS values must be determined on a site specific basis.
Depending on parent material properties (calcareousness, acidity, texture) and feeding water the peaty soils are divided into two types specified by ESC as peaty gley soils and peaty podzols, and by WRB as Histic Gleysols and Histic Podzols.
The effect of geometry, parent material properties and boundary conditions on the compressive response is explored in detail and models are developed for the stiffness, plastic collapse and elastic buckling strength of the Y-core.
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Continuous lithosequences have parent materials whose properties vary gradually along a transect, the prototypical example being soils formed on loess deposits at increasing distances downwind from their alluvial source.
This study had two objectives: (1) to determine the parent material and landscape properties controlling the formation of the different depressional soils; and (2) to use these controls to identify quantitative, terrain-based predictors of soil type in depressions.
We selected ten old forests along a strong gradient in soil forming factors (especially parent material and climate), soil properties and humus forms.
The spatial distribution and properties of parent material components form the starting point for any soil and ecosystem.
Other soil and landscape properties including parent material composition, colluvium on lower slope positions, C horizon cementation, and depth of soil development also affected Ks of horizons in these soils and should be used to better estimate Ks.
Soil parent material influences the mineral and structural properties of soils, and mycorrhizas help plants adapt to these properties.
We characterize the lap joint using scanning electron microscopy and nanoindentation, exploring potential variations in structure and mechanical properties within the parent material, overlap zone, and gap zone.
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