Description of soil MBATV~~~~~A (Antler River)
| Classification | BL.SO |
|---|---|
| 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 | Second layer The growth of plant roots is restricted by the second layer. |
| Type of root restricting layer | Solonetzic Solonetzic B 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. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Weakly Calcareous < 6 CaCO3 equivalent (%) |
| Below | Shale Shale bedrock |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | 20 | A | p | 1.3 | 0 | 20 | 40 | 40 | F | 5 | 3.0 | -9 | -9 | 6.8 | 7.3 | 98 | 0 | 31 | 0 | 0.3 | 49 | 45 | 43 | 20 | ||
| 2 | 20 | 50 | B | nt | 1.6 | 0 | 10 | 40 | 50 | F | 3 | 1.5 | -9 | -9 | 7.2 | 7.6 | 100 | 0 | 29 | 1 | 0.1 | 40 | 40 | 38 | 21 | ||
| 3 | 50 | 90 | C | ksgj | 1.35 | 0 | 14 | 40 | 46 | F | 3 | 0.2 | -9 | -9 | 8.2 | 8.5 | 100 | 15 | 26 | 3 | 0.1 | 48 | 44 | 42 | 19 | ||
| 4 | 90 | 100 | R | 1.8 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||