Description of soil MBBKO~~~~~A (Breckon)
Classification | R.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 | Growing season The water table is present in the soil during the growing season. |
Root restrictions | No root restricting layer The growth of plant roots is not restricted by any soil layer. |
Type of root restricting layer | n/a Not Applicable |
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 |
---|---|---|
Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
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 | 0 | 15 | A | p | 1.25 | 0 | 16 | 35 | 49 | F | 0 | 5.0 | -9 | -9 | 6.4 | 6.9 | 82 | 0 | 42 | 0 | 0.3 | 51 | 44 | 42 | 20 | ||
2 | 15 | 37 | A | h | 1.3 | 0 | 16 | 35 | 49 | F | 0 | 1.5 | -9 | -9 | 6.6 | 7.1 | 88 | 0 | 33 | 0 | 0.3 | 48 | 44 | 42 | 20 | ||
3 | 37 | 100 | C | g | 1.35 | 0 | 12 | 33 | 55 | F | 0 | 0.3 | -9 | -9 | 7.0 | 7.4 | 100 | 0 | 32 | 0 | 0.1 | 48 | 43 | 41 | 20 |