Description of soil SKYKDHS43~A (YORKTON R.BLC)
Classification | R.BLC |
---|---|
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 | Second layer The growth of plant roots is restricted by the second layer. |
Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
Drainage | Moderately well drained Water is removed from the soil somewhat slowly in relation to supply. Excess water is removed somewhat slowly due to low perviousness, shallow water table, lack of gradient, or some combination of these. Soils have intermediate to high water storage capacity (5-6 cm) within the control section and are usually medium to fined textured. Precipitation is the dominant water source in medium to fine textured soils; precipitation and significant additions by subsurface flow are necessary in coarse textured soils. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Calcareous and Saline Calcareous and Saline |
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 | 19 | A | pksa | 1.4 | 0 | 38 | 32 | 30 | F | 8 | 4.0 | -9 | -9 | 7.4 | 7.5 | 100 | 5 | 34 | 4 | 2.97 | 51 | -9 | 33 | 20 | ||
2 | 19 | 100 | C | ksa | 1.5 | 0 | 35 | 32 | 33 | F | 11 | 0.3 | -9 | -9 | 7.9 | 8.0 | 100 | 21 | 21 | 6 | 2.35 | 43 | -9 | 38 | 22 |