Description of soil NSTUOX2~~~A (Truro)
| Classification | OT.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 | Non growing season The water table is present in the soil during the non growing season. |
| Root restrictions | Second layer The growth of plant roots is restricted by the second layer. |
| Type of root restricting layer | Ortstein Ortstein 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 |
|---|---|---|
| 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). |
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 | 26 | A | p | 1.0 | 1 | 70 | 25 | 5 | F | 17 | 3.0 | -9 | -9 | 5.0 | 6.0 | 100 | 0 | 11 | 0 | 10.0 | 48 | 31 | 28 | 11 | ||
| 2 | 26 | 55 | B | fc | 2.0 | 2 | 89 | 6 | 5 | F | 19 | 1.0 | -9 | -9 | 5.0 | 6.0 | 84 | 0 | 10 | 0 | 4.0 | 45 | 16 | 12 | 5 | ||
| 3 | 55 | 100 | C | 2.0 | 1 | 89 | 8 | 3 | F | 16 | 0.0 | -9 | -9 | 5.0 | 5.0 | 92 | 0 | 5 | 0 | 7.0 | 38 | 20 | 15 | 5 | |||