Description of soil ONBCW~~~~~A (BLACKWELL)
| Classification | R.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 | 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 |
|---|---|---|
| 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:
|
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | 14 | A | p | 1.04 | 0 | 0 | 37 | 63 | M | 0 | 4.3 | -9 | -9 | 7.1 | 7.3 | 100 | 1 | 65 | 0 | 0.467 | 62 | 50 | 48 | 25 | ||
| 2 | 14 | 28 | B | g | 1 | 1.47 | 0 | 0 | 35 | 65 | M | 0 | 4.4 | -9 | -9 | 7.1 | 7.5 | 100 | 1 | 67 | 0 | 0.174 | 46 | 40 | 37 | 34 | |
| 3 | 28 | 47 | B | g | 2 | 1.47 | 0 | 0 | 46 | 54 | M | 0 | 1.9 | -9 | -9 | 7.1 | 7.6 | 100 | 3 | 46 | 0 | 0.191 | 45 | 40 | 35 | 32 | |
| 4 | 47 | 64 | C | kg | 1 | 1.49 | 0 | 0 | 51 | 49 | M | 0 | 0.0 | -9 | -9 | 7.3 | 7.7 | 100 | 15 | 31 | 0 | 0.193 | 44 | 40 | 35 | 30 | |
| 5 | 64 | 100 | C | kg | 2 | 1.49 | 0 | 1 | 58 | 41 | M | 0 | 0.0 | -9 | -9 | 7.4 | 7.9 | 100 | 32 | 27 | 0 | 0.193 | 44 | 40 | 35 | 27 | |