Description of soil ABKWOaa~~~A (KAWOOD)
|Profile||Agricultural soil profile
The soil has been disturbed by agriculture.
|Kind of material||Mineral
The soil material is primarily composed of mineral particles.
The water table is not present in the soil at any time.
|Root restrictions||Second layer
The growth of plant roots is restricted by the second layer.
|Type of root restricting layer||Solonetzic
Solonetzic B horizon
Water is removed from the soil readily but not rapidly. Excess water flows downward readily into underlying pervious material or laterally as subsurface flow. Soils have intermediate available water storage capacity (4-5 cm) within the control section, and are generally intermediate in texture and depth. Water source is precipitation. On slopes subsurface flow may occur for short durations, but additions are equaled by losses.
|Mode of Deposition||Texture||Chemical properties|
Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock.
Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL).
< 6 CaCO3 equivalent (%)
- Date Modified: