Description of soil BCCOApod~~N (COMIAKEN)
| Classification | GL.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 |
|---|---|---|
| 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). |
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 | -1 | 0 | L | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 33.5 | -9 | -9 | 5.2 | 5.6 | 32 | 0 | 118 | 0 | 21.0 | 90 | 35 | 21 | 14 | |||
| 2 | 0 | 5 | A | h | 1.1 | 0 | 64 | 29 | 7 | F | 16 | 2.8 | -9 | -9 | 5.2 | 5.7 | 52 | 0 | 12 | 0 | 1.0 | 58 | 31 | 22 | 8 | ||
| 3 | 5 | 15 | B | m | 1.2 | 0 | 67 | 27 | 6 | F | 17 | 0.9 | -9 | -9 | 5.4 | 5.9 | 48 | 0 | 12 | 0 | 1.0 | 55 | 28 | 21 | 8 | ||
| 4 | 15 | 50 | B | g | 1.5 | 0 | 78 | 18 | 4 | F | 20 | 0.7 | -9 | -9 | 5.3 | 5.8 | 46 | 0 | 13 | 0 | 10.0 | 43 | 25 | 17 | 9 | ||
| 5 | 50 | 60 | BC | g | 1 | 1.5 | 0 | 80 | 15 | 5 | F | 20 | 0.6 | -9 | -9 | 5.1 | 5.6 | 59 | 0 | 14 | 0 | 10.0 | 43 | 14 | 12 | 6 | |
| 6 | 60 | 100 | BC | g | 2 | 1.5 | 0 | 81 | 15 | 4 | F | 20 | 0.6 | -9 | -9 | 5.1 | 5.6 | 59 | 0 | 14 | 0 | 10.0 | 43 | 14 | 12 | 6 | |