Description of soil ONHEY~~~~~A (HARNEY)
| 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 | 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. |
Medium Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
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 | 15 | A | p | 1.24 | 0 | 69 | 20 | 11 | M | 9 | 2.3 | -9 | -9 | 7.1 | 7.5 | 100 | 0 | 25 | 0 | 3.066 | 54 | 40 | 28 | 9 | ||
| 2 | 15 | 23 | B | mgj | 1.39 | 0 | 72 | 22 | 6 | M | 8 | 1.3 | -9 | -9 | 7.3 | 7.7 | 100 | 0 | 15 | 0 | 4.371 | 48 | 40 | 19 | 7 | ||
| 3 | 23 | 35 | C | kg | 1.61 | 0 | 73 | 20 | 7 | M | 11 | 0.4 | -9 | -9 | 7.5 | 8.0 | 100 | 0 | 10 | 0 | 2.559 | 39 | 35 | 17 | 8 | ||
| 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 | |||