Description of soil BCKLK~~~~~N (KLUK)
| Classification | O.DYB |
|---|---|
| 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 | Never The water table is not present in the soil at any time. |
| Root restrictions | Seventh layer The growth of plant roots is restricted by the seventh layer. |
| Type of root restricting layer | Compact Till Compact (Basal) Till |
| Drainage | Rapidly drained Water is removed from the soil rapidly in relation to supply. Excess water flows downward if underlying material is pervious. Subsurface flow may occur on steep gradients during heavy rainfall. Soils have low available water storage capacity (2.5-4 cm) within the control section, and are usually coarse textured, or shallow, or both. Water source is precipitation. |
| Mode of Deposition | Texture | Chemical properties | |
|---|---|---|---|
| Uppermost | 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:
|
Coarse Skeletal Coarse Skeletal (USDA Texture Classes: VGS, VGLS). |
Medium Acid to Neutral pH 5.6 - 7.4 |
| Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
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 | -3 | 0 | LFH | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 52.8 | -9 | -9 | 4.6 | 5.4 | 46 | 0 | 112 | 0 | 21.0 | 87 | 35 | 20 | 13 | |||
| 2 | 0 | 15 | B | m | 1.5 | 35 | 80 | 15 | 5 | C | 20 | 1.1 | -9 | -9 | 5.0 | 5.9 | 33 | 0 | 9 | 0 | 30.0 | 43 | 15 | 10 | 4 | ||
| 3 | 15 | 25 | BC | 1.5 | 45 | 95 | 3 | 2 | C | 24 | 1.2 | -9 | -9 | 5.4 | 6.4 | 48 | 0 | 8 | 0 | 60.0 | 43 | 10 | 6 | 2 | |||
| 4 | 25 | 43 | C | 1 | 1.5 | 45 | 95 | 3 | 2 | C | 24 | 1.1 | -9 | -9 | 5.4 | 6.3 | 54 | 0 | 5 | 0 | 60.0 | 43 | 10 | 6 | 2 | ||
| 5 | 43 | 66 | C | 2 | 1.5 | 60 | 95 | 3 | 2 | C | 24 | 0.8 | -9 | -9 | 5.5 | 6.3 | 61 | 0 | 5 | 0 | 60.0 | 43 | 7 | 4 | 1 | ||
| 6 | 66 | 125 | C | 3 | 1.5 | 60 | 95 | 3 | 2 | C | 24 | 0.8 | -9 | -9 | 5.4 | 6.2 | 71 | 0 | 6 | 0 | 60.0 | 43 | 7 | 4 | 1 | ||
| 7 | 125 | 150 | 2 | C | 1.7 | 50 | 32 | 39 | 29 | F | 8 | 0.3 | -9 | -9 | 6.7 | 7.8 | 99 | 0 | 12 | 0 | 0.1 | 36 | 16 | 15 | 12 | ||