Description of soil MBMWTs~~~~A (Mowat)
| 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 | First layer The growth of plant roots is restricted by the first (uppermost) layer. |
| Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
| 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 | Fluviolacustrine Fluviolacustrine |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
| Below | 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 Calcareous > 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 | 20 | A | pks | 1.0 | 0 | 7 | 24 | 69 | - | 3 | 10.0 | -9 | -9 | 6.8 | 7.3 | 90 | 0 | 80 | 5 | 1.0 | 60 | 50 | 47 | 20 | ||
| 2 | 20 | 30 | AC | 1.35 | 0 | 10 | 39 | 51 | VF | 5 | 2.4 | -9 | -9 | 7.4 | 7.8 | 100 | 9 | 48 | 5 | 0.1 | 49 | 44 | 42 | 20 | |||
| 3 | 30 | 60 | C | ksg | 1.35 | 0 | 8 | 39 | 53 | - | 0 | 1.3 | -9 | -9 | 7.7 | 8.0 | 100 | 7 | 47 | 5 | 0.1 | 49 | 44 | 42 | 20 | ||
| 4 | 60 | 100 | 2 | C | ksg | 1.7 | 15 | 29 | 53 | 18 | F | 9 | 0.3 | -9 | -9 | 7.8 | 8.1 | 100 | 56 | 6 | 5 | 1.2 | 37 | 27 | 22 | 11 | |