Description of soil YTHOD~~~~~N (HODNETT)
| Classification | GL.TC |
|---|---|
| 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 | Fifth layer The growth of plant roots is restricted by the fifth layer. |
| Type of root restricting layer | Cryic Cryic (frozen) horizon |
| 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:
|
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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 | -8 | 0 | F | 0.08 | 0 | -9 | -9 | -9 | - | -9 | 60.0 | 3 | 10 | 5.6 | 5.9 | 70 | 0 | 60 | 0 | 20.0 | 85 | 40 | 25 | 15 | |||
| 2 | 0 | 4 | A | hy | 1.1 | 0 | 20 | 74 | 6 | F | 0 | 7.0 | -9 | -9 | 5.8 | 6.0 | 90 | 0 | 35 | 0 | 2.0 | 45 | 40 | 28 | 8 | ||
| 3 | 4 | 20 | B | mgjy | 1.3 | 0 | 22 | 72 | 6 | F | 0 | 2.4 | -9 | -9 | 6.1 | 8.1 | 90 | 0 | 18 | 0 | 2.0 | 45 | 40 | 28 | 8 | ||
| 4 | 20 | 50 | BC | gy | 1.3 | 0 | 28 | 63 | 9 | F | 0 | 0.8 | -9 | -9 | 6.8 | 7.5 | 70 | 3 | 29 | 1 | 2.0 | 45 | 40 | 28 | 8 | ||
| 5 | 50 | 100 | C | kyz | 1.2 | 0 | 32 | 48 | 20 | F | 0 | 0.6 | -9 | -9 | 6.6 | 6.1 | 70 | 5 | 5 | 1 | -9.0 | -9 | -9 | -9 | -9 | ||