Description of soil QCTLY40000A (TILLY)

Orthic Humo-Ferric Podzol

The soil has been disturbed by agriculture.

The soil material is primarily composed of mineral particles.

The water table is present in the soil during the non growing season.

The growth of plant roots is restricted by the seventh layer.

Lithic (consolidated bedrock)

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.

These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand.

Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL).

pH < 5.6

Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock.

Medium Skeletal (USDA Texture Classes: VGSL, VGL).

pH < 5.6

Shale bedrock

Not Applicable

Not Applicable