Description of soil ONLICV~~~~A (LINCOLN)
| 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 | Lithic Lithic (consolidated bedrock) |
| 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 | 0 | 20 | A | p | 1.22 | 0 | 76 | 14 | 10 | F | 8 | 1.2 | -9 | -9 | 6.0 | 5.6 | 100 | 1 | 24 | 0 | 3.931 | 54 | 40 | 27 | 7 | ||
| 2 | 20 | 30 | 2 | B | g | 1.42 | 0 | 8 | 23 | 69 | F | 0 | 0.5 | -9 | -9 | 8.0 | 7.5 | 100 | 2 | 67 | 0 | 0.231 | 46 | 40 | 37 | 33 | |
| 3 | 30 | 35 | 2 | C | kg | 1.52 | 0 | 1 | 33 | 66 | F | 0 | 0.4 | -9 | -9 | 9.0 | 8.3 | 100 | 28 | 43 | 0 | 0.175 | 42 | 40 | 36 | 35 | |
| 4 | 35 | 100 | R | 2.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||