Description of soil BCRYTpodp~N (ROYSTON)
Classification | O.HG |
---|---|
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 | Non growing season The water table is present in the soil during the non growing season. |
Root restrictions | Fifth layer The growth of plant roots is restricted by the fifth layer. |
Type of root restricting layer | Compact Till Compact (Basal) Till |
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. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | 10 | O | h | 0.5 | -9 | -9 | -9 | -9 | - | -9 | 41.2 | 6 | 15 | 6.1 | 6.6 | 68 | 0 | 131 | 0 | 9.0 | 87 | 70 | 54 | 25 | ||
2 | 10 | 25 | B | m | 1.55 | 35 | 37 | 44 | 19 | F | 6 | 2.7 | -9 | -9 | 4.8 | 5.3 | 36 | 0 | 28 | 0 | 1.0 | 42 | 41 | 29 | 16 | ||
3 | 25 | 50 | B | g | 1 | 1.55 | 35 | 35 | 42 | 23 | F | 6 | 2.9 | -9 | -9 | 4.7 | 5.2 | 37 | 0 | 28 | 0 | 1.0 | 42 | 41 | 29 | 16 | |
4 | 50 | 80 | B | g | 2 | 1.6 | 35 | 33 | 53 | 14 | F | 6 | 0.5 | -9 | -9 | 4.3 | 4.8 | 46 | 0 | 11 | 0 | 0.1 | 40 | 30 | 24 | 8 | |
5 | 80 | 100 | BC | g | 1.65 | 30 | 38 | 45 | 17 | F | 6 | 0.5 | -9 | -9 | 4.4 | 4.9 | 56 | 0 | 16 | 0 | 0.1 | 38 | 27 | 20 | 9 |