Description of soil ONMOYB~~~~A (MORLEY)
| 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 | 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 |
|---|---|---|
| Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Fragmental Fragmental |
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 | 20 | A | p | 1.12 | 20 | 5 | 59 | 36 | VF | 0 | 3.5 | -9 | -9 | 7.2 | 6.7 | 100 | 1 | 46 | 0 | 0.414 | 59 | 50 | 45 | 18 | ||
| 2 | 20 | 49 | B | mgj | 1.39 | 25 | 8 | 61 | 31 | VF | 0 | 0.6 | -9 | -9 | 7.3 | 6.8 | 100 | 1 | 26 | 0 | 0.254 | 48 | 40 | 38 | 21 | ||
| 3 | 49 | 68 | B | g | 1 | 1.47 | 25 | 6 | 67 | 27 | VF | 0 | 0.8 | -9 | -9 | 7.4 | 6.9 | 100 | 1 | 25 | 0 | 0.204 | 45 | 40 | 36 | 20 | |
| 4 | 68 | 100 | B | g | 2 | 1.47 | 30 | 5 | 73 | 22 | VF | 0 | 0.1 | -9 | -9 | 7.5 | 7.0 | 100 | 1 | 18 | 0 | 0.209 | 45 | 40 | 36 | 17 | |