Description of soil MBNKL1~~~~N (Nekik Lake 1)
| Classification | FI.OC |
|---|---|
| Profile | Native soil profile The soil is in native condition (undisturbed by agriculture). |
| Kind of material | Organic The soil material is primarily composed of organic 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 | Cryic Cryic (frozen) horizon |
| 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 | Sphagnum Peat These deposits consist of sphagnum or forest peat formed in an ombrotrophic environment caused by the slightly elevated nature of the bog. They tend to be disassociated from nutrient-rich ground water or surrounding mineral soils. |
Fibric Fibric |
Extremely / Strongly Acidic pH < 5.6 |
| Middle | Undifferentiated organic A layered sequence of more than three undifferentiated types of organic material (>30% organic matter by weight). |
Fibric Fibric |
Extremely / Strongly Acidic pH < 5.6 |
| Lowest | Undifferentiated organic A layered sequence of more than three undifferentiated types of organic material (>30% organic matter by weight). |
Undifferentiated Undifferentiated |
Undifferentiated Undifferentiated acidity and/or calcareousness |
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 | 25 | O | f | 1 | 0.05 | 0 | -9 | -9 | -9 | - | -9 | 52.3 | 3 | 0 | 4.3 | 4.8 | 50 | 0 | 132 | 0 | 30.0 | 95 | 40 | 30 | 5 | |
| 2 | 25 | 50 | O | f | 2 | 0.08 | 0 | -9 | -9 | -9 | - | -9 | 48.7 | 5 | 0 | 4.9 | 5.4 | 42 | 0 | 115 | 0 | 30.0 | 95 | 60 | 40 | 12 | |
| 3 | 50 | 65 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 46.5 | 5 | 0 | 5.2 | 5.7 | 60 | 0 | 146 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
| 4 | 65 | 100 | O | fz | 0.08 | 0 | -9 | -9 | -9 | - | -9 | 49.8 | 5 | 0 | 4.8 | 5.2 | 45 | 0 | 167 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 5 | 100 | 140 | O | mz | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 45.8 | 5 | 0 | 5.1 | 5.5 | 57 | 0 | 167 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 6 | 140 | 150 | O | hz | 0.27 | 0 | -9 | -9 | -9 | - | -9 | 38.9 | 8 | 0 | 6.4 | 6.8 | 90 | 0 | 200 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 7 | 150 | 175 | C | kgz | 1.4 | 0 | 6 | 50 | 44 | - | 0 | 0.3 | -9 | -9 | 7.2 | 7.6 | 100 | 8 | 12 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||