Description of soil NLSLI~~~~~N (Shoal Point)

General Characteristics
Classification O.G

Orthic Gleysol

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.

Water table Non growing season

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

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 Rapidly drained

Water is removed from the soil rapidly in relation to supply. Excess water flows downward if underlying material is pervious. Subsurface flow may occur on steep gradients during heavy rainfall. Soils have low available water storage capacity (2.5-4 cm) within the control section, and are usually coarse textured, or shallow, or both. Water source is precipitation.

Parent Materials
Mode of Deposition Texture Chemical properties
Till (Morainal)

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

Fine Skeletal

Fine Skeletal (USDA Texture Classes: VGC).

Extremely / Strongly Acidic

pH < 5.6

Soil Layer Characteristics

Soil Layer Characteristics
Classification Physical Chemical Water
Layer Number Upper
depth
Lower
depth
hzn_lit hzn_mas hzn_suf hzn_mod bd cofrag tsand tsilt tclay domsand vfsand orgcarb vonpost wood phca ph2 bases caco3 cec ec ksat kp0 kp10 kp33 kp1500
1 -38 -30 O f 0.39 0 -9 -9 -9 - -9 39.0 2 2 2.9 3.2 0 0 120 0 40.0 97 40 30 10
2 -30 -25 O m 0.47 0 -9 -9 -9 - -9 43.0 5 2 3.1 3.4 0 0 130 0 5.0 95 60 50 25
3 -25 -20 O h 1 0.58 0 -9 -9 -9 - -9 48.0 7 4 3.1 3.5 0 0 150 0 0.1 80 75 65 5
4 -20 0 O h 2 0.65 0 -9 -9 -9 - -9 48.0 8 5 3.3 3.7 0 0 150 0 0.1 80 75 65 5
5 0 10 A eg 1.4 0 8 28 64 M 1 5.5 -9 -9 3.8 4.7 12 0 41 0 7.0 41 36 35 30
6 10 23 B g 1.37 0 17 35 48 M 3 0.9 -9 -9 5.1 6.0 99 0 18 0 10.0 39 32 30 22
7 23 51 C 1.52 0 1 77 22 C 0 0.4 -9 -9 6.2 6.8 99 0 10 0 1.0 34 29 27 14
8 51 100 R 2.65 -9 -9 -9 -9 - -9 -9.0 -9 -9 -9.0 -9.0 -9 -9 -9 -9 -9.0 -9 -9 -9 -9
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