Description of soil NBWAS375~~N (WAASIS)
| Classification | R.HG |
|---|---|
| Profile | Native soil profile The soil is in native condition (undisturbed 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 |
|---|---|---|
| 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). |
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 | -5 | 0 | LFH | 0.16 | -9 | -9 | -9 | -9 | - | -9 | 35.0 | -9 | 15 | 4.5 | 5.0 | 22 | 0 | 186 | 0 | 50.0 | 94 | 40 | 30 | 10 | |||
| 2 | 0 | 15 | A | h | 1.0 | 0 | 40 | 47 | 13 | VF | 15 | 6.0 | -9 | -9 | 5.4 | 5.9 | 99 | 0 | 33 | 0 | 25.0 | 62 | 46 | 38 | 14 | ||
| 3 | 15 | 100 | C | g | 1.5 | 0 | 22 | 51 | 27 | VF | 18 | 0.9 | -9 | -9 | 5.4 | 5.9 | 99 | 0 | 13 | 0 | 0.2 | 43 | 40 | 35 | 23 | ||