Description of soil MBEVL~~~~~N (Evelyn Lake)
| 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 |
|---|---|---|
| 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 | -15 | 0 | LH | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 39.7 | -9 | 0 | 5.1 | 5.5 | 52 | 0 | 58 | 0 | 10.0 | 85 | 70 | 50 | 15 | |||
| 2 | 0 | 7 | A | hej | 1.2 | 0 | 36 | 53 | 11 | VF | 33 | 4.5 | -9 | -9 | 5.0 | 5.4 | 63 | 0 | 20 | 0 | 3.0 | 46 | 24 | 18 | 7 | ||
| 3 | 7 | 12 | AB | 1.25 | 0 | 34 | 44 | 22 | VF | 25 | 1.8 | -9 | -9 | 5.1 | 5.5 | 74 | 0 | 16 | 0 | 3.0 | 45 | 42 | 38 | 16 | |||
| 4 | 12 | 30 | B | g | 1.3 | 0 | 18 | 44 | 38 | VF | 12 | 0.6 | -9 | -9 | 6.6 | 7.0 | 90 | 2 | 21 | 0 | 0.3 | 50 | 47 | 43 | 22 | ||
| 5 | 30 | 44 | BC | 1.35 | 0 | 22 | 50 | 28 | VF | 18 | 0.2 | -9 | -9 | 7.2 | 7.6 | 100 | 6 | 12 | 0 | 0.3 | 47 | 44 | 28 | 14 | |||
| 6 | 44 | 60 | C | kg | 1.5 | 0 | 47 | 38 | 15 | VF | 41 | 0.0 | -9 | -9 | 7.4 | 7.8 | 100 | 28 | 5 | 0 | 3.0 | 42 | 22 | 20 | 10 | ||
| 7 | 60 | 100 | C | kg | 1.5 | 0 | 32 | 50 | 18 | VF | 30 | 0.0 | -9 | -9 | 7.5 | 7.9 | 100 | 33 | 4 | 0 | 3.0 | 42 | 35 | 22 | 11 | ||