Description of soil MBLTK~~~~~N (Lost Lake)
| Classification | R.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 |
|---|---|---|
| Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Coarse Skeletal Coarse Skeletal (USDA Texture Classes: VGS, VGLS). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | -12 | -6 | O | f | 0.09 | 0 | -9 | -9 | -9 | - | -9 | 54.6 | 2 | 0 | 3.5 | 3.9 | 34 | 0 | 86 | 0 | 10.0 | 95 | 45 | 40 | 12 | ||
| 2 | -6 | 0 | O | m | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 52.4 | 5 | 0 | 5.7 | 6.1 | 56 | 0 | 83 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
| 3 | 0 | 45 | C | g | 1 | 1.6 | 0 | 97 | 1 | 2 | F | 5 | 0.2 | -9 | -9 | 6.8 | 7.2 | 100 | 0 | 2 | 0 | 30.0 | 40 | 10 | 7 | 2 | |
| 4 | 45 | 100 | C | g | 2 | 1.7 | 0 | 95 | 3 | 2 | F | 5 | 0.0 | -9 | -9 | 7.0 | 7.4 | 100 | 0 | 2 | 0 | 30.0 | 36 | 10 | 7 | 2 | |