Description of soil YTLBG~~~~~N (LABERGE)
| Classification | O.HG |
|---|---|
| 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 | Unspecified period The water table is present in the soil during an unspecified period. |
| 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 |
|---|---|---|
| Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Weakly Calcareous < 6 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 | -20 | 0 | FH | 0.06 | 0 | -9 | -9 | -9 | - | -9 | 50.0 | 3 | 10 | 6.3 | 6.8 | 70 | 0 | 80 | 0 | 20.0 | 90 | 65 | 50 | 21 | |||
| 2 | 0 | 14 | A | h | 0.75 | 0 | 45 | 40 | 15 | F | 20 | 10.0 | -9 | -9 | 6.5 | 7.0 | 70 | 0 | 44 | 0 | 3.0 | 50 | 30 | 25 | 13 | ||
| 3 | 14 | 25 | B | mgj | 1.0 | 0 | 36 | 50 | 14 | F | 20 | 5.0 | -9 | -9 | 6.8 | 7.2 | 70 | 0 | 24 | 0 | 3.0 | 40 | 21 | 15 | 6 | ||
| 4 | 25 | 100 | C | g | 1.2 | 0 | 55 | 30 | 15 | F | 20 | 2.0 | -9 | -9 | 7.0 | 7.5 | 70 | 1 | 11 | 0 | 10.0 | 40 | 21 | 15 | 6 | ||