Description of soil BCBVM08~~~N (BEAVERDAM)
| Classification | O.G |
|---|---|
| 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 |
|---|---|---|
| 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). |
Moderately / Very Strongly Calcareous 6 - 40 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 | 0 | 5 | A | hk | 1.0 | 0 | 37 | 52 | 11 | F | 9 | 6.7 | -9 | -9 | 7.0 | 7.5 | 100 | 3 | 32 | 0 | 30.0 | 62 | 38 | 31 | 7 | ||
| 2 | 5 | 13 | B | gk | 1 | 1.0 | 0 | 42 | 54 | 4 | F | 11 | 1.6 | -9 | -9 | 7.0 | 7.5 | 100 | 10 | 19 | 1 | 10.0 | 62 | 34 | 26 | 4 | |
| 3 | 13 | 33 | B | gk | 2 | 1.45 | 0 | 36 | 59 | 5 | F | 9 | 0.9 | -9 | -9 | 7.5 | 8.0 | 100 | 10 | 22 | 1 | 10.0 | 45 | 30 | 25 | 6 | |
| 4 | 33 | 61 | BC | gca | 1.37 | 0 | 31 | 61 | 8 | F | 8 | 0.6 | -9 | -9 | 8.5 | 9.0 | 100 | 20 | 22 | 1 | 10.0 | 48 | 34 | 29 | 8 | ||
| 5 | 61 | 127 | C | gk | 1.65 | 0 | 33 | 64 | 3 | F | 8 | 0.1 | -9 | -9 | 8.2 | 8.7 | 100 | 10 | 22 | 1 | 10.0 | 38 | 26 | 22 | 5 | ||