Description of soil MBTUB~~~~~N (Tuber 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 | Fourth layer The growth of plant roots is restricted by the fourth layer. |
| Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
| 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 | |
|---|---|---|---|
| Uppermost | 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). |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Igneous, acidic Igneous, acidic bedrock (dominantly granite) |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | -10 | 0 | O | m | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 30.0 | 5 | 0 | 6.2 | 6.6 | 90 | 0 | 115 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
| 2 | 0 | 8 | A | hg | 1.48 | 15 | 69 | 21 | 10 | M | 15 | 2.4 | -9 | -9 | 6.5 | 6.9 | 95 | 0 | 15 | 0 | 25.0 | 43 | 11 | 9 | 5 | ||
| 3 | 8 | 60 | C | kg | 1.7 | 15 | 77 | 21 | 2 | M | 19 | 0.1 | -9 | -9 | 7.0 | 7.4 | 100 | 0 | 3 | 0 | 50.0 | 35 | 7 | 5 | 2 | ||
| 4 | 60 | 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 | |||