Description of soil NBGSV125~~N (GLASSVILLE)
| Classification | O.G |
|---|---|
| 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 | 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 Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -19 | 0 | LFH | 0.2 | -9 | -9 | -9 | -9 | - | -9 | 45.0 | -9 | 15 | 4.9 | 5.4 | 23 | 0 | 128 | 0 | 50.0 | 92 | 40 | 30 | 10 | |||
| 2 | 0 | 15 | A | eg | 1.25 | 20 | 27 | 52 | 21 | F | 7 | 1.2 | -9 | -9 | 4.1 | 4.6 | 28 | 0 | 13 | 0 | 7.0 | 42 | 31 | 27 | 11 | ||
| 3 | 15 | 28 | B | g | 1.45 | 23 | 18 | 55 | 27 | VC | 7 | 1.0 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 14 | 0 | 5.0 | 35 | 28 | 26 | 15 | ||
| 4 | 28 | 100 | C | g | 1.6 | 35 | 38 | 43 | 19 | VC | 9 | 0.4 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 10 | 0 | 3.0 | 26 | 20 | 18 | 11 | ||