Marginal land and problem soil of Thailand
Skeletal Soils |
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| Skeletal soils refer to soils that contain 35 percent or more (by volume) of rock fragments, cobbles, gravel and laterite concretions or ironstones having diameters greater than 2 mm, within shallow depths (less than 50 cm). These soils occur in a number of landscapes ranging from alluvial terraces, fans, erosional surfaces, peneplains, hill slopes, and mountainous areas. Skeletal soils contain laterite at some period of time on erosional surfaces or as remnants of a peneplain surface. Soils with cobblestones often develop on alluvial terraces. On the other hand, soils shallow to bed rock or soils containing rock fragments are common on areas where the parent rocks are subject to continuous erosion or weathering. They occupy mostly foothill slopes, mountains, and partial peneplains or erosional surfaces. Due to a much different mode of soil formation, the skeletal soils are relatively variable in physical and chemical properties. However, these soils are usually shallow, prone to erosion, and low in natural fertility status. | ||||||||
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