Description of soil PEGWBBC~~~A (Gowanbrae)
| Classification | O.HFP |
|---|---|
| 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 | Never The water table is not present in the soil at any time. |
| Root restrictions | Sixth layer The growth of plant roots is restricted by the sixth layer. |
| Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
| 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 | 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. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | p | 1.3 | 1 | 83 | 12 | 5 | F | 8 | 1.3 | -9 | -9 | 4.1 | 4.6 | 80 | 0 | 2 | 0 | 25.0 | 50 | 42 | 31 | 4 | ||
| 2 | 20 | 28 | A | e | 1.49 | 1 | 74 | 21 | 5 | F | 14 | 0.2 | -9 | -9 | 3.9 | 4.4 | 18 | 0 | 1 | 0 | 2.4 | 39 | 27 | 14 | 3 | ||
| 3 | 28 | 36 | B | f | 1.13 | 4 | 69 | 23 | 8 | F | 12 | 1.5 | -9 | -9 | 4.1 | 4.6 | 25 | 0 | 1 | 0 | 19.0 | 54 | 37 | 31 | 6 | ||
| 4 | 36 | 54 | B | m | 1 | 1.51 | 10 | 63 | 31 | 6 | F | 15 | 0.5 | -9 | -9 | 4.5 | 5.0 | 34 | 0 | 1 | 0 | 4.0 | 38 | 29 | 24 | 7 | |
| 5 | 54 | 80 | B | m | 2 | 1.66 | 7 | 56 | 31 | 13 | F | 13 | 0.1 | -9 | -9 | 4.2 | 4.7 | 24 | 0 | 1 | 0 | 2.7 | 33 | 26 | 23 | 8 | |
| 6 | 80 | 100 | R | 2.45 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||