Description of soil MBWHK~~~~~N (Wuchusk Lake)
| 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 | Always The water table is always present in the soil. |
| 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 |
|---|---|---|
| Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
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 | -13 | 0 | LFH | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 41.9 | -9 | 0 | 3.9 | 4.3 | 42 | 0 | 75 | 0 | 10.0 | 85 | 70 | 50 | 15 | |||
| 2 | 0 | 8 | A | e | 1.1 | 0 | 6 | 23 | 71 | - | 6 | 2.8 | -9 | -9 | 5.8 | 6.2 | 78 | 0 | 31 | 0 | 0.3 | 57 | 49 | 47 | 20 | ||
| 3 | 8 | 23 | B | tgj | 1.3 | 0 | 0 | 9 | 91 | - | 0 | 0.9 | -9 | -9 | 5.6 | 6.0 | 91 | 0 | 32 | 0 | 0.1 | 50 | 49 | 47 | 21 | ||
| 4 | 23 | 36 | B | tg | 1.3 | 0 | 1 | 8 | 91 | - | 1 | 0.8 | -9 | -9 | 6.7 | 7.1 | 100 | 0 | 30 | 0 | 0.1 | 50 | 49 | 47 | 22 | ||
| 5 | 36 | 46 | BC | 1.3 | 0 | 5 | 20 | 75 | - | 5 | 0.6 | -9 | -9 | 7.8 | 8.2 | 100 | 4 | 26 | 0 | 0.1 | 50 | 48 | 46 | 22 | |||
| 6 | 46 | 66 | C | kg | 1 | 1.4 | 0 | 3 | 26 | 71 | - | 3 | 0.0 | -9 | -9 | 7.8 | 8.2 | 100 | 15 | 24 | 0 | 0.3 | 50 | 48 | 46 | 20 | |
| 7 | 66 | 80 | C | kg | 2 | 1.45 | 0 | 5 | 35 | 60 | - | 5 | 0.0 | -9 | -9 | 7.8 | 8.2 | 100 | 18 | 21 | 0 | 0.3 | 48 | 44 | 42 | 20 | |
| 8 | 80 | 100 | R | 2.8 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||