Description of soil ONWLLO~~~~N (WELLAND)
| 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 |
|---|---|---|
| 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:
|
Very Fine Very Fine (USDA Texture Classes: HC (more than 60% clay). |
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 | -20 | 0 | O | m | 0.1 | 0 | -9 | -9 | -9 | - | -9 | 17.0 | 6 | 0 | 5.5 | 5.0 | 100 | 0 | 122 | 0 | 3.455 | 97 | 80 | 70 | 50 | ||
| 2 | 0 | 15 | A | h | 1.23 | 0 | 7 | 45 | 48 | VF | 0 | 2.4 | -9 | -9 | 5.2 | 5.9 | 76 | 0 | 46 | 0 | 0.341 | 54 | 50 | 42 | 25 | ||
| 3 | 15 | 34 | B | tg | 1 | 1.47 | 0 | 3 | 28 | 69 | M | 0 | 0.6 | -9 | -9 | 6.5 | 6.7 | 100 | 0 | 45 | 0 | 0.2 | 45 | 40 | 38 | 36 | |
| 4 | 34 | 43 | B | tg | 2 | 1.47 | 0 | 1 | 22 | 77 | M | 0 | 0.6 | -9 | -9 | 7.3 | 7.4 | 100 | 1 | 50 | 0 | 0.2 | 45 | 42 | 41 | 36 | |
| 5 | 43 | 100 | C | kg | 1.49 | 0 | 1 | 26 | 73 | M | 0 | 0.0 | -9 | -9 | 7.7 | 7.8 | 100 | 11 | 44 | 1 | 0.193 | 44 | 42 | 40 | 35 | ||