Description of soil YTGRY~~~~~N (GRAY RIDGE)
| 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 |
|---|---|---|
| Colluvial Massive to moderately-well stratified, nonsorted to poorly sorted sediments with any range of particle sizes from clay to boulders that have reached their present position only by direct, gravity-induced movement. Processes include slow displacements such as creep and solifluction and rapid movements such as earth flows. |
Medium Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | -10 | 0 | LF | 0.08 | 0 | -9 | -9 | -9 | - | -9 | 50.0 | 3 | 10 | 5.0 | 5.5 | 70 | 0 | 60 | 0 | 20.0 | 90 | 35 | 20 | 14 | |||
| 2 | 0 | 12 | A | h | 1.0 | 5 | 50 | 36 | 14 | VF | 22 | 7.0 | -9 | -9 | 5.5 | 6.0 | 70 | 0 | 17 | 0 | 4.0 | 50 | 30 | 20 | 12 | ||
| 3 | 12 | 30 | B | g | 1.25 | 20 | 70 | 12 | 18 | C | 10 | 2.0 | -9 | -9 | 5.5 | 6.0 | 70 | 0 | 8 | 0 | 12.0 | 40 | 21 | 20 | 15 | ||
| 4 | 30 | 100 | C | g | 1.3 | 30 | 60 | 20 | 20 | C | 12 | 1.0 | -9 | -9 | 5.7 | 6.2 | 70 | 0 | 2 | 0 | 12.0 | 40 | 21 | 15 | 6 | ||