Description of soil NBHPN125~~A (HAMPTON)
| Classification | O.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 | 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. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
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 | 0 | 18 | A | p | 1.19 | 0 | 60 | 29 | 11 | F | 19 | 2.6 | -9 | -9 | 5.2 | 5.8 | 99 | 0 | 17 | 0 | 7.0 | 55 | 46 | 42 | 17 | ||
| 2 | 18 | 35 | C | g | 1 | 1.25 | 0 | 60 | 29 | 11 | F | 19 | 1.5 | -9 | -9 | 5.4 | 6.0 | 99 | 0 | 13 | 0 | 3.0 | 53 | 42 | 39 | 15 | |
| 3 | 35 | 100 | C | g | 2 | 1.4 | 0 | 65 | 25 | 10 | VF | 25 | 1.2 | -9 | -9 | 5.2 | 5.8 | 99 | 0 | 11 | 0 | 2.0 | 47 | 37 | 36 | 15 | |