Description of soil BCGOS~~~~~N (GOOSE)
| 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 | 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 |
|---|---|---|
| Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | -5 | 0 | O | m | 0.2 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 6 | 2 | 6.0 | 6.4 | 95 | 0 | 120 | 0 | 3.0 | 90 | 65 | 49 | 20 | ||
| 2 | 0 | 15 | A | h | 1.0 | 1 | 5 | 65 | 30 | F | 1 | 8.1 | -9 | -9 | 5.8 | 6.2 | 90 | 0 | 40 | 0 | 3.0 | 62 | 55 | 38 | 29 | ||
| 3 | 15 | 25 | AB | 1.4 | 5 | 6 | 44 | 50 | F | 2 | 1.2 | -9 | -9 | 5.5 | 6.0 | 88 | 0 | 25 | 0 | 3.0 | 47 | 42 | 34 | 23 | |||
| 4 | 25 | 45 | B | g | 1.5 | 3 | 5 | 35 | 60 | F | 1 | 0.9 | -9 | -9 | 6.1 | 6.5 | 95 | 0 | 28 | 0 | 1.0 | 43 | 42 | 37 | 28 | ||
| 5 | 45 | 55 | BC | 1.5 | 3 | 7 | 36 | 57 | F | 2 | 0.7 | -9 | -9 | 7.1 | 7.4 | 100 | 1 | 27 | 1 | 0.3 | 43 | 42 | 36 | 26 | |||
| 6 | 55 | 100 | C | skg | 1.5 | 2 | 8 | 38 | 54 | F | 2 | 0.4 | -9 | -9 | 7.3 | 7.6 | 100 | 4 | 24 | 4 | 1.0 | 43 | 42 | 35 | 25 | ||