Description of soil BCHLNmcm~~A (HOLLINGS)
| Classification | DU.DYB |
|---|---|
| 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 | Fifth layer The growth of plant roots is restricted by the fifth 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 | 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 |
| Below | 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. |
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 | 0 | 13 | A | p | 1.27 | 55 | 55 | 37 | 8 | F | 14 | 2.45 | -9 | -9 | 4.6 | 5.4 | 67 | 0 | 17 | 0 | 4.0 | 52 | 28 | 20 | 8 | ||
| 2 | 13 | 30 | B | m | 1.46 | 55 | 64 | 32 | 4 | F | 14 | 1.0 | -9 | -9 | 4.9 | 5.7 | 66 | 0 | 9 | 0 | 6.0 | 45 | 26 | 19 | 9 | ||
| 3 | 30 | 53 | BC | c | 1.6 | 45 | 54 | 36 | 10 | F | 14 | 0.0 | -9 | -9 | 5.0 | 5.8 | 78 | 1 | 9 | 0 | 6.0 | 40 | 21 | 16 | 7 | ||
| 4 | 53 | 95 | 2 | BC | 1.54 | 75 | 91 | 5 | 4 | C | 19 | 1.0 | -9 | -9 | 4.8 | 5.7 | 45 | 0 | 11 | 0 | 49.0 | 42 | 14 | 6 | 3 | ||
| 5 | 95 | 160 | 2 | BC | c | 1.54 | 65 | 91 | 5 | 4 | C | 19 | 0.0 | -9 | -9 | 5.6 | 6.0 | 45 | 0 | 9 | 0 | 49.0 | 42 | 14 | 9 | 4 | |