Description of soil BCSKW~~~~~N (SPAKWANIKO)
| 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 |
|---|---|---|
| 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. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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 | -5 | 0 | LFH | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 40.6 | -9 | -9 | 4.5 | 5.1 | 43 | 0 | 72 | 0 | 21.0 | 92 | 35 | 21 | 14 | |||
| 2 | 0 | 9 | A | h | 1 | 1.15 | 10 | 31 | 55 | 14 | F | 8 | 11.5 | -9 | -9 | 3.4 | 3.9 | 3 | 0 | 37 | 0 | 10.0 | 57 | 35 | 29 | 9 | |
| 3 | 9 | 16 | A | h | 2 | 1.1 | 10 | 31 | 52 | 17 | F | 8 | 6.8 | -9 | -9 | 3.5 | 4.0 | 4 | 0 | 23 | 0 | 10.0 | 58 | 36 | 30 | 10 | |
| 4 | 16 | 28 | B | g | 1.35 | 15 | 34 | 51 | 15 | F | 9 | 2.8 | -9 | -9 | 3.6 | 4.1 | 4 | 0 | 16 | 0 | 10.0 | 49 | 30 | 26 | 10 | ||
| 5 | 28 | 60 | BC | g | 1.4 | 15 | 35 | 45 | 20 | F | 9 | 0.5 | -9 | -9 | 4.4 | 4.9 | 30 | 0 | 13 | 0 | 10.0 | 47 | 30 | 26 | 13 | ||
| 6 | 60 | 100 | C | g | 1.5 | 20 | 33 | 50 | 17 | F | 8 | 0.5 | -9 | -9 | 4.7 | 5.2 | 56 | 0 | 9 | 0 | 3.0 | 43 | 30 | 26 | 12 | ||