See more from this Division: S05 Pedology
See more from this Session: Soil Genesis and Classification
Abstract:
The Torrerts and vertic soils are derived from weathered, or residual deposit of argillaceous rocks in the Cretaceous, Jurassic and Neogene period, of Quaternary basalt, as well as N2 red-clayey palaeosols. Their water transported sediments are agricultural land. The soil clay content (<0.002mm) is between 35.40 and 56.49%. The expansive potential of the Vertisols is high. Angular blocky/wedged-shaped structure, or slickenside, as well as cracks are present. The cracks remain open, but close for less than 60 consecutive days as soil water content increases through rainfall in summer. The Torrerts inherit the expandable clay minerals ,such as montmorilllonite and illite- montmorilllonite from parent materials. This is similar to the Vertisols that were identified in the eastern and southern part of
The Vertisols may also exist in the Xizang Plateau (
The thickness of soil horizon of some Torrerts is more shallow than other suborders of Vertisols in eastern and southern China. But the soils and underlying expansive soft rocks have damaged various constructions in NW China and Inner Monogolia China. Many methods have been used to combat the hazards.
This research provides information for improving the Chinese Soil Taxonomy. Only three suborders of Vertisols were recognized in the edition in 2001.
See more from this Division: S05 Pedology
See more from this Session: Soil Genesis and Classification