Description of soil BCOHUsa~~~N (OLHAUSEN)
|Profile||Native soil profile
The soil is in native condition (undisturbed 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||Sixth layer
The growth of plant roots is restricted by the sixth layer.
|Type of root restricting layer||Salinity
Salinity (conductivity > 4 dS/m)
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|
Eolian material deposited by wind: uniform deposit of very fine sand and silt.
Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL).
< 6 CaCO3 equivalent (%)
Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL).
|Calcareous and Saline
Calcareous and Saline
- Date Modified: