Description of soil MBBKRs~~~~A (Basker)
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 | Always The water table is always present in the soil. |
Root restrictions | First layer The growth of plant roots is restricted by the first (uppermost) 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. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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 | 20 | A | pksg | 1.21 | 0 | 8 | 57 | 35 | - | 0 | 4.4 | -9 | -9 | 7.3 | 7.7 | 100 | 4 | 44 | 5 | 2.0 | 54 | 48 | 46 | 24 | ||
2 | 20 | 60 | C | ksg | 1 | 1.42 | 0 | 3 | 60 | 37 | - | 0 | 0.5 | -9 | -9 | 7.4 | 7.8 | 100 | 6 | 37 | 5 | 2.0 | 46 | 40 | 38 | 20 | |
3 | 60 | 100 | C | ksg | 2 | 1.51 | 0 | 2 | 68 | 30 | - | 0 | 0.5 | -9 | -9 | 7.5 | 7.8 | 100 | 12 | 29 | 5 | 2.0 | 43 | 38 | 32 | 18 |