Description of soil BCMLF~~~~~N (METCALFE)
| Classification | BR.GL |
|---|---|
| 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 | Moderately well drained Water is removed from the soil somewhat slowly in relation to supply. Excess water is removed somewhat slowly due to low perviousness, shallow water table, lack of gradient, or some combination of these. Soils have intermediate to high water storage capacity (5-6 cm) within the control section and are usually medium to fined textured. Precipitation is the dominant water source in medium to fine textured soils; precipitation and significant additions by subsurface flow are necessary in coarse textured soils. |
| Mode of Deposition | Texture | Chemical properties |
|---|---|---|
| Glaciofluvial Material moved by glaciers and subsequently sorted and deposited by streams flowing from the melting ice. The deposits are stratified and may occur in the form of outwash plains, deltas, kames eskers, and kame terraces. See also glacial drift and till. |
Coarse Coarse (USDA Texture Classes: FS,LCS,LS,LFS,GLS,CBLS). |
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 | -2 | 0 | LF | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 41.0 | -9 | 10 | 4.6 | 5.8 | 33 | 0 | 71 | 0 | 16.0 | 85 | 35 | 15 | 7 | |||
| 2 | 0 | 3 | A | ej | 1.33 | 0 | 55 | 33 | 12 | F | 14 | 3.6 | -9 | -9 | 5.9 | 6.5 | 61 | 0 | 12 | 0 | 17.0 | 50 | 27 | 21 | 8 | ||
| 3 | 3 | 15 | B | f | 1 | 1.44 | 0 | 56 | 36 | 8 | F | 14 | 1.9 | -9 | -9 | 4.9 | 6.4 | 26 | 0 | 16 | 0 | 5.0 | 45 | 28 | 21 | 9 | |
| 4 | 15 | 20 | B | f | 2 | 1.37 | 0 | 42 | 42 | 16 | F | 10 | 0.4 | -9 | -9 | 4.8 | 6.5 | 53 | 0 | 5 | 0 | 5.0 | 48 | 29 | 22 | 10 | |
| 5 | 20 | 28 | C | 1.63 | 0 | 42 | 41 | 17 | F | 11 | 0.4 | -9 | -9 | 5.9 | 6.6 | 73 | 0 | 4 | 0 | 2.0 | 39 | 22 | 19 | 11 | |||
| 6 | 28 | 46 | AB | 1 | 1.42 | 0 | 40 | 42 | 18 | F | 10 | 0.2 | -9 | -9 | 5.6 | 6.5 | 80 | 0 | 4 | 0 | 9.0 | 46 | 28 | 22 | 11 | ||
| 7 | 46 | 58 | AB | 2 | 1.42 | 0 | 40 | 42 | 18 | F | 10 | 0.3 | -9 | -9 | 5.6 | 6.5 | 77 | 0 | 5 | 0 | 9.0 | 46 | 28 | 22 | 11 | ||
| 8 | 58 | 79 | B | t | 1.58 | 0 | 43 | 38 | 19 | F | 11 | 0.4 | -9 | -9 | 6.2 | 6.4 | 71 | 0 | 11 | 0 | 6.0 | 41 | 25 | 21 | 12 | ||
| 9 | 79 | 100 | 2 | C | gj | 1.55 | 0 | 80 | 16 | 4 | F | 20 | 0.2 | -9 | -9 | 6.1 | 6.6 | 81 | 0 | 4 | 0 | 23.0 | 41 | 18 | 10 | 4 | |