Description of soil BCABId~~~~A (ALBION)
| Classification | HU.LG |
|---|---|
| Profile | Agricultural soil profile The soil has been disturbed 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 | Third layer The growth of plant roots is restricted by the third layer. |
| Type of root restricting layer | Undifferentiated Undifferentiated |
| 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 |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | 18 | A | p | 0.9 | 1 | 10 | 66 | 24 | F | 5 | 9.0 | -9 | -9 | 4.7 | 5.2 | 35 | 0 | 40 | 0 | 0.3 | 66 | 55 | 44 | 30 | ||
| 2 | 18 | 43 | A | eg | 1.41 | 2 | 10 | 60 | 30 | F | 3 | 5.5 | -9 | -9 | 5.1 | 5.6 | 20 | 0 | 25 | 0 | 0.3 | 47 | 42 | 35 | 19 | ||
| 3 | 43 | 81 | B | tg | 1.56 | 2 | 6 | 44 | 50 | VF | 3 | 0.4 | -9 | -9 | 6.0 | 6.5 | 90 | 0 | 35 | 0 | 0.3 | 41 | 40 | 34 | 20 | ||
| 4 | 81 | 102 | BC | g | 1.55 | 2 | 6 | 46 | 48 | F | 2 | 0.2 | -9 | -9 | 6.5 | 7.0 | 90 | 0 | 27 | 0 | 0.3 | 42 | 40 | 34 | 23 | ||
| 5 | 102 | 132 | C | g | 1.57 | 2 | 6 | 46 | 48 | F | 1 | 0.1 | -9 | -9 | 6.6 | 7.1 | 90 | 0 | 22 | 0 | 0.1 | 41 | 40 | 34 | 21 | ||