Description of soil NBRCB125~~N (RICHIBUCTO)
| Classification | GLE.DYB |
|---|---|
| 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 |
|---|---|---|
| Glaciomarine Glaciomarine |
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
Extremely / Strongly Acidic pH < 5.6 |
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 | 0 | LFH | 0.22 | -9 | -9 | -9 | -9 | - | -9 | 40.0 | -9 | 15 | 3.5 | 4.0 | 10 | 0 | 100 | 0 | 50.0 | 92 | 40 | 28 | 13 | |||
| 2 | 0 | 17 | A | egj | 1.4 | 1 | 82 | 13 | 5 | M | 5 | 0.4 | -9 | -9 | 3.8 | 4.7 | 12 | 0 | 5 | 0 | 12.0 | 47 | 20 | 15 | 6 | ||
| 3 | 17 | 45 | B | mgj | 1.4 | 1 | 82 | 10 | 8 | M | 5 | 0.3 | -9 | -9 | 4.2 | 4.8 | 36 | 0 | 7 | 0 | 8.0 | 47 | 16 | 14 | 7 | ||
| 4 | 45 | 100 | C | g | 1.6 | 1 | 92 | 5 | 3 | M | 5 | 0.1 | -9 | -9 | 4.8 | 5.4 | 52 | 0 | 5 | 0 | 8.0 | 40 | 11 | 7 | 4 | ||