Description of soil ABBRRpt~~~N (BEAR RIVER)
Classification | O.LG |
---|---|
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 | Sixth layer The growth of plant roots is restricted by the sixth layer. |
Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
Drainage | Poorly drained Water is removed so slowly in relation to supply that the soil remains wet for a comparatively large part of the time the soil is not frozen. Excess water is evident in the soil for a large part of the time. Subsurface flow or groundwater flow, or both, in addition to precipitation are the main water sources; there may also be a perched water table, with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are gleyed subgroups, Gleysols, and Organic soils. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
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 | -25 | 0 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 4 | 5 | 5.0 | 5.5 | 67 | 0 | 120 | 0 | 3.0 | 90 | 65 | -9 | 20 | ||
2 | 0 | 5 | A | hg | 1.15 | 5 | 20 | 50 | 30 | F | 9 | 5.4 | -9 | -9 | 5.2 | 5.7 | 70 | 0 | 33 | 0 | 10.0 | 55 | -9 | 42 | 27 | ||
3 | 5 | 13 | A | eg | 1.3 | 5 | 30 | 55 | 15 | F | 11 | 1.5 | -9 | -9 | 5.0 | 5.5 | 70 | 0 | 20 | 0 | 10.0 | 51 | -9 | 29 | 15 | ||
4 | 13 | 35 | B | tg | 1.35 | 5 | 15 | 35 | 50 | F | 7 | 1.1 | -9 | -9 | 5.9 | 6.3 | 90 | 0 | 30 | 0 | 1.0 | 49 | -9 | 45 | 28 | ||
5 | 35 | 50 | BC | g | 1.3 | 5 | 20 | 35 | 45 | F | 9 | 0.8 | -9 | -9 | 7.4 | 7.6 | 99 | 2 | 28 | 1 | 0.0 | 51 | -9 | 41 | 25 | ||
6 | 50 | 100 | C | skg | 1.3 | 5 | 20 | 35 | 45 | F | 9 | 0.3 | -9 | -9 | 7.6 | 7.8 | 99 | 8 | 27 | 8 | 0.0 | 51 | -9 | 41 | 25 |