Description of soil BCDER~~~~~N (DEERHOLME)
| Classification | DU.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 | Eighth layer The growth of plant roots is restricted by the eighth layer. |
| Type of root restricting layer | Duric Duric horizon |
| Drainage | Well drained Water is removed from the soil readily but not rapidly. Excess water flows downward readily into underlying pervious material or laterally as subsurface flow. Soils have intermediate available water storage capacity (4-5 cm) within the control section, and are generally intermediate in texture and depth. Water source is precipitation. On slopes subsurface flow may occur for short durations, but additions are equaled by losses. |
| Mode of Deposition | Texture | Chemical properties | |
|---|---|---|---|
| Uppermost | Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -1 | 0 | L | 0.21 | -9 | -9 | -9 | -9 | - | -9 | 43.0 | -9 | 0 | 3.9 | 4.4 | 59 | 0 | 100 | 0 | 21.0 | 91 | 35 | 21 | 14 | |||
| 2 | 0 | 3 | A | h | 1.24 | 15 | 63 | 29 | 8 | F | 16 | 17.0 | -9 | -9 | 3.5 | 4.1 | 73 | 0 | 94 | 0 | 9.0 | 53 | 25 | 19 | 8 | ||
| 3 | 3 | 22 | B | f | 1 | 1.44 | 15 | 49 | 45 | 6 | F | 14 | 4.0 | -9 | -9 | 4.3 | 4.7 | 18 | 0 | 22 | 0 | 5.0 | 45 | 33 | 32 | 13 | |
| 4 | 22 | 42 | B | f | 2 | 1.44 | 15 | 50 | 48 | 2 | F | 14 | 4.0 | -9 | -9 | 4.3 | 4.7 | 18 | 0 | 24 | 0 | 5.0 | 45 | 28 | 21 | 9 | |
| 5 | 42 | 55 | B | m | 1.46 | 15 | 64 | 31 | 5 | F | 14 | 1.0 | -9 | -9 | 4.6 | 5.0 | 66 | 0 | 12 | 0 | 6.0 | 45 | 26 | 20 | 8 | ||
| 6 | 55 | 78 | 2 | BC | g | 1.6 | 5 | 54 | 38 | 8 | F | 14 | 0.0 | -9 | -9 | 4.1 | 4.9 | 78 | 0 | 16 | 0 | 6.0 | 40 | 21 | 17 | 6 | |
| 7 | 78 | 98 | 3 | BC | g | 1.6 | 25 | 59 | 35 | 6 | F | 14 | 0.0 | -9 | -9 | 4.4 | 5.2 | 78 | 0 | 12 | 0 | 6.0 | 40 | 21 | 17 | 6 | |
| 8 | 98 | 110 | 3 | BC | gc | 1.6 | 35 | 64 | 32 | 4 | F | 14 | 0.0 | -9 | -9 | 4.7 | 5.3 | 78 | 0 | 10 | 0 | 6.0 | 40 | 21 | 17 | 6 | |