Description of soil MBWEK~~~~~N (Wekusko)

General Characteristics
Classification TY.M

Typic Mesisol

Profile Native soil profile

The soil is in native condition (undisturbed by agriculture).

Kind of material Unclassified

This material was not classified due to an absence of information or an unusual situation, such as rockland or an extremely shallow soil.

Water table Always

The water table is always present in the soil.

Root restrictions No root restricting layer

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

Type of root restricting layer n/a

Not Applicable

Drainage Very poorly drained

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.

Parent Materials
Mode of Deposition Texture Chemical properties
Uppermost Forest Peat

This class is used for forest peatcovered or forest peat-filled areas where the water table is at or above the peat surface. The dominant peat materials are shallow to deep mesic to humic forest and fen peat formed in a eutrophic environment resulting from strong water movement from the margins or other mineral sources.

Mesic

Mesic

Medium Acid to Neutral

pH 5.6 - 7.4

Below Till (Morainal)

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

Not Applicable

Not Applicable

Not Applicable

Not Applicable

Soil Layer Characteristics

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