Description of soil ONFMBBR~~~A (FLAMBOROUGH)
| Classification | O.HG |
|---|---|
| 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 | Fourth layer The growth of plant roots is restricted by the fourth 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 |
|---|---|---|
| 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 Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
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 | 22 | A | p | 1.26 | 1 | 56 | 36 | 8 | VF | 48 | 1.3 | -9 | -9 | 6.1 | 6.0 | 100 | 1 | 27 | 0 | 1.583 | 53 | 40 | 33 | 11 | ||
| 2 | 22 | 30 | B | tjgj | 1.47 | 0 | 51 | 39 | 10 | VF | 46 | 0.8 | -9 | -9 | 5.9 | 5.4 | 100 | 0 | 20 | 0 | 0.572 | 45 | 40 | 32 | 18 | ||
| 3 | 30 | 52 | B | g | 1 | 1.47 | 0 | 56 | 36 | 8 | VF | 44 | 0.3 | -9 | -9 | 5.9 | 5.4 | 100 | 0 | 11 | 0 | 3.715 | 45 | 40 | 18 | 8 | |
| 4 | 52 | 72 | B | mgj | 1.49 | 0 | 86 | 9 | 5 | VF | 35 | 0.2 | -9 | -9 | 5.8 | 5.3 | 100 | 0 | 9 | 0 | 3.323 | 44 | 40 | 19 | 6 | ||
| 5 | 72 | 100 | B | g | 2 | 1.49 | 0 | 89 | 7 | 4 | VF | 43 | 0.1 | -9 | -9 | 6.4 | 5.9 | 100 | 0 | 9 | 0 | 3.323 | 44 | 40 | 19 | 6 | |