Description of soil QCDUA30000A (DUHAMEL)
| 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 | Always The water table is always present in the soil. |
| 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 |
|---|---|---|
| Fluviolacustrine Fluviolacustrine |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Weakly Calcareous < 6 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 | 30 | A | hp | 1.2 | 0 | 0 | 63 | 37 | - | 0 | 3.1 | -9 | -9 | 6.0 | 6.5 | 62 | 0 | 23 | 0 | 10.0 | 55 | 44 | 41 | 20 | ||
| 2 | 30 | 37 | A | egkj | 1.45 | 0 | 0 | 78 | 22 | - | 0 | 0.5 | -9 | -9 | 6.6 | 7.5 | 72 | 5 | 9 | 0 | 1.0 | 45 | 38 | 36 | 17 | ||
| 3 | 37 | 67 | B | gk | 1.6 | 0 | 0 | 70 | 30 | - | 0 | 0.1 | -9 | -9 | 7.0 | 8.0 | 82 | 18 | 16 | 0 | 1.0 | 40 | 35 | 34 | 23 | ||
| 4 | 67 | 100 | C | kg | 1.6 | 0 | 0 | 73 | 27 | - | 0 | 0.1 | -9 | -9 | 7.0 | 8.1 | 82 | 18 | 15 | 0 | 1.0 | 40 | 35 | 33 | 22 | ||