Geochemical and Geotechnical Features of Terra Rossa in Karst Areas Of

Document Type

Conference Proceeding

Publication Date

8-25-2011

Description

A sequence of siliceous dolomite and magnesian limestone, known as Knox group rock are prevalent in karst landforms of Southern Appalachians. Thick blanket of clay-rich red soils (terra rossa) are common along fractures, cavities, and between bedding planes of these calcareous, cavernous rocks. The red soil causes serious environmental and geotechnical hazards, hence proper understanding of the soil's pedology, geochemistry and engineering behavior can lead to better site characterization for safer development. Twenty four terra rossa samples were collected and laboratory analysis was performed such as: geochemistry (mineral content using X-Ray diffraction, and geotechnical characterization (grain size distribution, porosity, hydraulic conductivity, and shrink-swell potential). The soil profile above Knox rock exhibits distinct vertical variation in geochemical and geotechnical characteristics. The soils are well drained in the upper horizon and exhibit slight reduction in porosity and hydraulic conductivity with depth. The analysis indicate that these soils overall are good foundation materials, however proper drainage should be installed to prevent foundation damage, soil erosion and landslides in slopes.

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