Description of soil BCTWA04~~~N (TWAIN)
Classification | HU.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 | Always The water table is always present in the soil. |
Root restrictions | Sixth layer The growth of plant roots is restricted by the sixth 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 | -13 | 0 | O | h | 0.17 | 0 | -9 | -9 | -9 | - | -9 | 18.7 | 8 | 0 | 5.1 | 5.7 | 45 | 0 | 75 | 0 | 0.2 | 88 | 70 | 57 | 35 | ||
2 | 0 | 10 | A | h | 1.1 | 15 | 25 | 57 | 18 | F | 6 | 6.5 | -9 | -9 | 4.5 | 5.1 | 29 | 0 | 51 | 0 | 10.0 | 58 | 35 | 30 | 9 | ||
3 | 10 | 20 | A | he | 1.3 | 15 | 25 | 57 | 18 | F | 6 | 4.5 | -9 | -9 | 4.4 | 5.3 | 29 | 0 | 35 | 0 | 3.0 | 51 | 32 | 28 | 11 | ||
4 | 20 | 46 | A | eg | 1.35 | 35 | 53 | 37 | 10 | F | 13 | 0.6 | -9 | -9 | 4.9 | 5.5 | 46 | 0 | 7 | 0 | 0.1 | 49 | 20 | 16 | 6 | ||
5 | 46 | 61 | B | tg | 1.6 | 35 | 41 | 31 | 28 | F | 10 | 0.2 | -9 | -9 | 6.5 | 6.8 | 100 | 0 | 15 | 0 | 0.1 | 40 | 21 | 20 | 14 | ||
6 | 61 | 100 | C | g | 1.7 | 35 | 42 | 30 | 28 | F | 11 | 0.1 | -9 | -9 | 6.4 | 6.7 | 92 | 0 | 8 | 0 | 0.1 | 36 | 20 | 19 | 15 |