Description of soil MBPUOs~~~~A (Paulson)
| Classification | R.G |
|---|---|
| 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 | Second layer The growth of plant roots is restricted by the second layer. |
| Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
| 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 |
|---|---|---|
| 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). |
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 | 25 | A | p | 1.25 | 0 | 4 | 36 | 60 | - | 0 | 7.5 | -9 | -9 | 7.5 | 7.8 | 100 | 2 | 61 | 3 | 0.3 | 51 | 46 | 44 | 21 | ||
| 2 | 25 | 50 | C | ksg | 1 | 1.35 | 0 | 2 | 20 | 78 | - | 0 | 2.0 | -9 | -9 | 7.2 | 7.6 | 100 | 0 | 50 | 4 | 0.1 | 48 | 44 | 42 | 21 | |
| 3 | 50 | 100 | C | ksg | 2 | 1.35 | 0 | 6 | 24 | 70 | - | 0 | 1.5 | -9 | -9 | 7.5 | 7.8 | 100 | 16 | 45 | 5 | 0.1 | 48 | 44 | 42 | 21 | |