Description of soil BCMNG~~~~~A (MANNING)
Classification | HU.LG |
---|---|
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 | 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 | |
---|---|---|---|
Uppermost | Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Weakly Calcareous < 6 CaCO3 equivalent (%) |
Below | Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Undifferentiated Undifferentiated acidity and/or calcareousness |
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 | 20 | A | p | 1.2 | 5 | 65 | 25 | 10 | F | 16 | 4.0 | -9 | -9 | 6.5 | 7.0 | 98 | 0 | 25 | 0 | 10.0 | 55 | 29 | 22 | 8 | ||
2 | 20 | 30 | A | h | 1.25 | 5 | 60 | 20 | 20 | F | 15 | 3.5 | -9 | -9 | 7.0 | 7.5 | 100 | 0 | 20 | 0 | 10.0 | 53 | 33 | 26 | 13 | ||
3 | 30 | 50 | A | eg | 1.3 | 5 | 60 | 20 | 20 | F | 15 | 0.7 | -9 | -9 | 6.5 | 7.0 | 100 | 0 | 12 | 0 | 3.0 | 51 | 32 | 26 | 13 | ||
4 | 50 | 72 | B | tg | 1.6 | 5 | 35 | 35 | 30 | F | 9 | 0.7 | -9 | -9 | 7.0 | 7.5 | 100 | 0 | 15 | 0 | 3.0 | 40 | 32 | 30 | 22 | ||
5 | 72 | 90 | C | kg | 1.5 | 5 | 60 | 15 | 25 | F | 15 | 0.3 | -9 | -9 | 7.5 | 8.0 | 100 | 10 | 12 | 1 | 1.0 | 43 | 31 | 27 | 18 | ||
6 | 90 | 100 | 2 | C | g | 1.5 | 60 | 90 | 5 | 5 | F | 23 | 0.1 | -9 | -9 | 7.7 | 8.2 | 100 | 1 | 5 | 1 | 60.0 | 43 | 9 | 6 | 2 |