Description of soil QCBMP33000A (BROMPTON)
Classification | O.HG |
---|---|
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 | Always The water table is always present in the soil. |
Root restrictions | Fourth layer The growth of plant roots is restricted by the fourth 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). |
Extremely / Strongly Acidic pH < 5.6 |
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 | 13 | A | p | 1.3 | 10 | 41 | 45 | 14 | F | 10 | 11.6 | -9 | -9 | 4.6 | 5.0 | 34 | 0 | 47 | 0 | 3.25 | 46 | 31 | 26 | 10 | ||
2 | 13 | 30 | A | he | 1.35 | 35 | 41 | 47 | 12 | F | 10 | 2.0 | -9 | -9 | 4.8 | 5.2 | 69 | 0 | 13 | 0 | 3.25 | 32 | 22 | 18 | 7 | ||
3 | 30 | 51 | B | g | 1.6 | 25 | 47 | 38 | 15 | F | 12 | 1.1 | -9 | -9 | 5.9 | 6.3 | 79 | 0 | 11 | 0 | 3.25 | 30 | 22 | 20 | 11 | ||
4 | 51 | 100 | C | g | 1.8 | 25 | 44 | 39 | 17 | F | 11 | 0.9 | -9 | -9 | 6.4 | 6.8 | 78 | 0 | 12 | 0 | 0.25 | 24 | 20 | 19 | 13 |