Description of soil MBPMS~~~~~N (Primes)

Typic Mesisol

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

The soil material is primarily composed of organic particles.

The water table is always present in the soil.

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

Lithic (consolidated bedrock)

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.

These deposits consist of sedge peat derived primarily from sedges with inclusions of partially decayed stems of shrubs formed in a eutrophic environment due to the close association of the material with mineral-rich waters.

Mesic

pH 5.6 - 7.4

These deposits consist of sedge peat derived primarily from sedges with inclusions of partially decayed stems of shrubs formed in a eutrophic environment due to the close association of the material with mineral-rich waters.

Humic

< 6 CaCO₃ equivalent (%)

Limestone bedrock (limestone and dolomite)

Not Applicable

> 40 CaCO₃ equivalent (%)