Description of soil NLMUP~~~~~N (Musgrave Pond)
Classification | O.G |
---|---|
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 | Poorly drained Water is removed so slowly in relation to supply that the soil remains wet for a comparatively large part of the time the soil is not frozen. Excess water is evident in the soil for a large part of the time. Subsurface flow or groundwater flow, or both, in addition to precipitation are the main water sources; there may also be a perched water table, with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are gleyed subgroups, Gleysols, and Organic soils. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Medium Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -30 | 0 | O | h | 0.38 | 0 | -9 | -9 | -9 | - | -9 | 48.0 | 8 | 0 | 4.2 | 5.1 | 36 | 0 | 150 | 0 | 0.1 | 80 | 75 | 65 | 5 | ||
2 | 0 | 3 | A | eg | 1.45 | 0 | 42 | 41 | 17 | VF | 19 | 1.6 | -9 | -9 | 4.4 | 5.2 | 52 | 0 | 14 | 0 | 7.0 | 37 | 27 | 24 | 12 | ||
3 | 3 | 8 | AB | g | 1.45 | 0 | 44 | 41 | 15 | VF | 20 | 1.0 | -9 | -9 | 4.4 | 5.1 | 52 | 0 | 11 | 0 | 7.0 | 41 | 29 | 25 | 12 | ||
4 | 8 | 60 | B | g | 1.4 | 9 | 48 | 41 | 11 | VF | 23 | 0.6 | -9 | -9 | 4.1 | 5.0 | 28 | 0 | 9 | 0 | 7.0 | 43 | 29 | 24 | 9 | ||
5 | 60 | 100 | C | g | 1.65 | 0 | 75 | 10 | 15 | VF | 25 | 0.1 | -9 | -9 | 4.5 | 5.1 | 60 | 0 | 7 | 0 | 1.0 | 21 | 15 | 12 | 8 |