Description of soil ONFNT~~~~~A (FONTHILL)
| Classification | O.MB |
|---|---|
| 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 | Unspecified period The water table is present in the soil during an unspecified period. |
| Root restrictions | No root restricting layer The growth of plant roots is not restricted by any soil layer. |
| Type of root restricting layer | n/a Not Applicable |
| 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 |
|---|---|---|
| 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). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
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 | 21 | A | p | 1.3 | 0 | 69 | 23 | 8 | VF | 20 | 1.6 | -9 | -9 | 6.3 | 6.6 | 100 | 0 | 20 | 0 | 3.828 | 51 | 40 | 23 | 7 | ||
| 2 | 21 | 54 | B | m | 1 | 1.39 | 0 | 72 | 22 | 6 | C | 8 | 0.2 | -9 | -9 | 6.2 | 6.8 | 100 | 0 | 10 | 0 | 4.474 | 48 | 40 | 19 | 7 | |
| 3 | 54 | 74 | B | m | 2 | 1.39 | 0 | 85 | 11 | 4 | C | 3 | 0.1 | -9 | -9 | 4.9 | 5.8 | 52 | 0 | 9 | 0 | 6.336 | 48 | 40 | 14 | 5 | |
| 4 | 74 | 100 | B | m | 3 | 1.39 | 0 | 86 | 10 | 4 | C | 3 | 0.1 | -9 | -9 | 5.0 | 6.1 | 60 | 0 | 9 | 0 | 6.371 | 48 | 40 | 14 | 5 | |