Description of soil ONFRMX~~~~N (FARMINGTON)
| Classification | O.MB |
|---|---|
| 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 | 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 |
|---|---|---|
| Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Fragmental Fragmental |
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 | 14 | A | h | 1.1 | 2 | 65 | 21 | 14 | M | 6 | 3.6 | -9 | -9 | 6.9 | 6.4 | 100 | 1 | 35 | 0 | 2.635 | 57 | 35 | 34 | 9 | ||
| 2 | 14 | 31 | B | mkj | 1.39 | 27 | 71 | 20 | 9 | M | 6 | 1.4 | -9 | -9 | 7.2 | 6.7 | 100 | 10 | 18 | 0 | 3.025 | 47 | 35 | 23 | 8 | ||
| 3 | 31 | 40 | BC | k | 1.47 | 23 | 83 | 14 | 3 | M | 5 | 0.7 | -9 | -9 | 7.3 | 6.8 | 100 | 18 | 9 | 0 | 6.052 | 44 | 35 | 11 | 4 | ||
| 4 | 40 | 100 | R | -9.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||