Description of soil ONBVE~~~~~N (BARRHAVEN)
| 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 |
|---|---|---|
| Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Fragmental Fragmental |
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 | 0 | 2 | A | h | 0.87 | 1 | 53 | 41 | 6 | M | 16 | 6.0 | -9 | -9 | 7.4 | 6.9 | 100 | 0 | 43 | 0 | 7.009 | 66 | 40 | 31 | 4 | ||
| 2 | 2 | 17 | B | mg | 1.39 | 9 | 53 | 40 | 7 | M | 14 | 3.7 | -9 | -9 | 7.3 | 6.8 | 100 | 0 | 30 | 0 | 2.754 | 46 | 40 | 23 | 7 | ||
| 3 | 17 | 30 | C | kg | 1.61 | 35 | 89 | 8 | 3 | M | 4 | 0.3 | -9 | -9 | 7.4 | 6.9 | 100 | 0 | 7 | 0 | 4.72 | 42 | 40 | 10 | 4 | ||
| 4 | 30 | 100 | R | 2.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||