Description of soil BCVODpsad~A (VINOD)
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 | Fourth layer The growth of plant roots is restricted by the fourth 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 | |
---|---|---|---|
Uppermost | Fen Peat These deposits consist of sedge peat derived primarily from sedges with inclusions of partially decayed stems of shrubs formed in a eutrophic environment due to the close association of the material with mineral-rich waters. |
Humic Humic |
Extremely / Strongly Acidic pH < 5.6 |
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). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -36 | -18 | O | p | 0.38 | 0 | -9 | -9 | -9 | - | -9 | 58.0 | 8 | 0 | 3.7 | 4.2 | 22 | 0 | 116 | 1 | 0.2 | 88 | 74 | 57 | 35 | ||
2 | -18 | 0 | O | h | 0.4 | 0 | -9 | -9 | -9 | - | -9 | 54.6 | 8 | 0 | 3.5 | 3.9 | 20 | 0 | 120 | 1 | 0.2 | 88 | 74 | 57 | 35 | ||
3 | 0 | 38 | C | gs | 1 | 0.91 | 0 | 7 | 67 | 26 | VF | 7 | 1.9 | -9 | -9 | 3.6 | 4.1 | 37 | 0 | 22 | 4 | 0.3 | 66 | 51 | 48 | 15 | |
4 | 38 | 66 | C | gs | 2 | 0.94 | 0 | 5 | 66 | 29 | VF | 5 | 1.0 | -9 | -9 | 3.2 | 3.7 | 66 | 0 | 20 | 6 | 0.3 | 65 | 51 | 51 | 14 | |
5 | 66 | 100 | C | gs | 3 | 1.1 | 0 | 1 | 79 | 20 | VF | 1 | 0.5 | -9 | -9 | 3.6 | 4.1 | 70 | 0 | 18 | 12 | 0.3 | 58 | 51 | 49 | 12 |