Description of soil YTPOP~~~~~N (POPES)
| 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 | |
|---|---|---|---|
| Uppermost | Undifferentiated organic A layered sequence of more than three undifferentiated types of organic material (>30% organic matter by weight). |
Fibric Fibric |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Undifferentiated mineral A sequence of more than three types of genetic mineral materials outcropping on a steep erosional escarpment. This complex class is to be used where units relating to individual genetic materials cannot be delimited separately at the scale of mapping. It may include colluvium derived from the various genetic materials and resting upon the scarp slope. |
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
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 | -17 | -7 | O | f | 0.06 | 0 | -9 | -9 | -9 | - | -9 | 36.0 | -9 | 5 | 5.0 | 7.0 | 90 | 0 | 60 | 0 | 15.0 | 93 | 48 | 33 | 13 | ||
| 2 | -7 | 0 | O | fm | 0.07 | 0 | -9 | -9 | -9 | - | -9 | 18.0 | -9 | 5 | 6.0 | 8.0 | 90 | 0 | 70 | 0 | 15.0 | 89 | 65 | 50 | 21 | ||
| 3 | 0 | 30 | A | hy | 0.75 | 0 | 26 | 47 | 27 | F | 15 | 15.8 | -9 | -9 | 6.0 | 8.2 | 70 | 0 | 39 | 0 | 2.0 | 55 | 50 | 32 | 13 | ||
| 4 | 30 | 50 | C | gy | 1.3 | 0 | 95 | 3 | 2 | F | 20 | 0.1 | -9 | -9 | 6.0 | 8.2 | 90 | 0 | 2 | 0 | 2.0 | 40 | 22 | 4 | 2 | ||
| 5 | 50 | 100 | C | z | 1.15 | 0 | 90 | 5 | 5 | F | 20 | 0.1 | -9 | -9 | 5.8 | 5.8 | 90 | 0 | 2 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||