Description of soil BCBHRd~~~~A (BEHARREL)
| 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 | Fifth layer The growth of plant roots is restricted by the fifth 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 |
|---|---|---|
| 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. |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
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 | 0 | 17 | A | p | 1.0 | 0 | 10 | 56 | 34 | VF | 3 | 3.6 | -9 | -9 | 5.4 | 5.9 | 50 | 0 | 28 | 0 | 0.3 | 62 | 45 | 33 | 21 | ||
| 2 | 17 | 27 | A | eg | 1.1 | 0 | 13 | 58 | 29 | VF | 3 | 2.9 | -9 | -9 | 5.2 | 5.7 | 46 | 0 | 27 | 0 | 0.3 | 58 | 45 | 33 | 21 | ||
| 3 | 27 | 47 | B | tg | 1.1 | 0 | 6 | 49 | 45 | VF | 1 | 1.7 | -9 | -9 | 4.8 | 5.3 | 53 | 0 | 28 | 0 | 0.3 | 58 | 45 | 33 | 21 | ||
| 4 | 47 | 60 | BC | g | 1.15 | 0 | 10 | 58 | 32 | VF | 3 | 3.0 | -9 | -9 | 4.8 | 5.3 | 51 | 0 | 31 | 0 | 0.3 | 57 | 43 | 33 | 20 | ||
| 5 | 60 | 68 | C | g | 1 | 1.25 | 0 | 18 | 67 | 15 | VF | 13 | 2.5 | -9 | -9 | 4.7 | 5.2 | 38 | 0 | 58 | 0 | 0.1 | 53 | 40 | 30 | 8 | |
| 6 | 68 | 87 | C | g | 2 | 1.3 | 0 | 25 | 65 | 10 | VF | 13 | 2.1 | -9 | -9 | 5.0 | 5.5 | 72 | 0 | 19 | 0 | 0.1 | 51 | 44 | 30 | 8 | |
| 7 | 87 | 150 | C | g | 3 | 1.35 | 0 | 26 | 60 | 14 | F | 7 | 1.7 | -9 | -9 | 4.9 | 5.4 | 66 | 0 | 16 | 0 | 0.1 | 49 | 47 | 30 | 8 | |