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Description of soil NTHAZ10~~~N (HAZEN)

General Characteristics
Classification R.TC

Regosolic Turbic Cryosol

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 Not applicable

Not applicable.

Root restrictions Not applicable

Non-applicable (e.g. rock, ice).

Type of root restricting layer n/a

Not Applicable

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.

Not Applicable

Not Applicable

Not Applicable

Not Applicable

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 0 14 C k - 9.0 -9 18 80 2 VF 13 1.2 -9 -9 7.3 -9.0 -9 11 -9 1 -9.0 -9 -9 -9 -9
2 14 35 C ky - 9.0 -9 39 59 2 VF 18 1.0 -9 -9 7.4 -9.0 -9 10 -9 0 -9.0 -9 -9 -9 -9
3 35 40 C kyz - 9.0 -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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