Description of soil NTKEL10~~~N (KETTLE LAKE)
| Classification | R.TC |
|---|---|
| Profile | Native soil profile The soil is in native condition (undisturbed by agriculture). |
| Kind of material | Unclassified This material was not classified due to an absence of information or an unusual situation, such as rockland or an extremely shallow soil. |
| Water table | Not applicable Not applicable. |
| Root restrictions | Not applicable Non-applicable (e.g. rock, ice). |
| 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 |
|---|---|---|
| Colluvial Massive to moderately-well stratified, nonsorted to poorly sorted sediments with any range of particle sizes from clay to boulders that have reached their present position only by direct, gravity-induced movement. Processes include slow displacements such as creep and solifluction and rapid movements such as earth flows. |
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 | 0 | 15 | C | k | - | 9.0 | 15 | 61 | 37 | 2 | VF | 19 | 2.2 | -9 | -9 | 7.3 | -9.0 | -9 | 10 | -9 | 1 | -9.0 | -9 | -9 | -9 | -9 | |
| 2 | 15 | 60 | C | ky | - | 9.0 | -9 | 39 | 58 | 3 | VF | 22 | 3.1 | -9 | -9 | 7.4 | -9.0 | -9 | 13 | -9 | 0 | -9.0 | -9 | -9 | -9 | -9 | |
| 3 | 60 | 80 | C | kz | - | 9.0 | -9 | 40 | 55 | 5 | VF | 18 | 2.8 | -9 | -9 | 7.1 | -9.0 | -9 | 7 | -9 | 0 | -9.0 | -9 | -9 | -9 | -9 | |