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Description of soil MBKIA~~~~~N (Kiask Lake)

General Characteristics
Classification OE.TC

Orthic Eutric Turbic Cryosol

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 Never

The water table is not present in the soil at any time.

Root restrictions Seventh layer

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

Type of root restricting layer Cryic

Cryic (frozen) horizon

Drainage Moderately well drained

Water is removed from the soil somewhat slowly in relation to supply. Excess water is removed somewhat slowly due to low perviousness, shallow water table, lack of gradient, or some combination of these. Soils have intermediate to high water storage capacity (5-6 cm) within the control section and are usually medium to fined textured. Precipitation is the dominant water source in medium to fine textured soils; precipitation and significant additions by subsurface flow are necessary in coarse textured soils.

Parent Materials
Mode of Deposition Texture Chemical properties
Lacustrine

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.

Very Fine

Very Fine (USDA Texture Classes: HC (more than 60% clay).

Moderately / Very Strongly Calcareous

6 - 40 CaCO3 equivalent (%)

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 -5 0 O m 0.12 0 -9 -9 -9 - -9 41.5 5 0 4.3 4.8 44 0 127 0 3.0 90 70 60 15
2 0 6 A hy 1.1 0 4 19 77 - 2 12.0 -9 -9 5.6 6.0 70 0 44 1 0.1 52 50 48 20
3 6 18 B my 1.4 0 7 25 68 - 4 1.8 -9 -9 6.2 6.6 80 0 40 1 0.1 51 49 47 21
4 18 25 O bhy 0.45 0 -9 -9 -9 - -9 27.9 9 0 5.5 5.9 70 0 120 1 0.1 90 70 65 20
5 25 38 BC byz 1.3 0 8 27 65 - 6 0.8 -9 -9 6.7 7.2 90 1 28 1 -9.0 -9 -9 -9 -9
6 38 41 A bhyz 1.2 0 2 12 86 - 1 8.8 -9 -9 6.4 6.8 85 0 40 1 -9.0 -9 -9 -9 -9
7 41 100 C kz 1.4 0 6 23 71 - 3 0.3 -9 -9 7.2 7.6 100 6 24 1 -9.0 -9 -9 -9 -9
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