Description of soil MBPMUv~~~~A (Pineimuta)

Rego Humic Gleysol

The soil has been disturbed by agriculture.

The soil material is primarily composed of mineral particles.

The water table is always present in the soil.

The growth of plant roots is not restricted by any soil layer.

Not Applicable

Water is removed from the soil so slowly that the water table remains at or on the surface for the greater part of the time the soil is not frozen. Excess water is present in the soil for the greater part of the time. Groundwater flow and subsurface flow are the major water sources. Precipitation is less important except where there is a perched water table with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are either Gleysolic or Organic.

Sediment, generally consisting of either stratified fine sand, silt, and clay deposited on the lake bed, or moderately-well sorted, stratified sand and coarse materials that consist of near lake shore or beach deposits. These materials have either settled from suspension in bodies of standing fresh water or accumulated at their margins through wave action.

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

> 40 CaCO₃ equivalent (%)

Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay.

Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL).

> 40 CaCO₃ equivalent (%)