Description of soil ONALLSH~~~N (ALLENDALE)
| Classification | O.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 | Unspecified period The water table is present in the soil during an unspecified period. |
| 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). |
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 | 27 | A | h | 1.32 | 0 | 82 | 10 | 8 | M | 15 | 1.5 | -9 | -9 | 5.3 | 4.8 | 84 | 1 | 18 | 0 | 4.383 | 51 | 40 | 21 | 8 | ||
| 2 | 27 | 41 | B | mg | 1 | 1.39 | 0 | 87 | 9 | 4 | M | 20 | 0.2 | -9 | -9 | 5.6 | 5.1 | 100 | 1 | 7 | 0 | 6.398 | 48 | 40 | 14 | 5 | |
| 3 | 41 | 55 | B | mg | 2 | 1.39 | 0 | 67 | 14 | 19 | F | 28 | 0.2 | -9 | -9 | 5.7 | 5.2 | 100 | 1 | 19 | 0 | 1.197 | 48 | 40 | 31 | 15 | |
| 4 | 55 | 100 | R | 2.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||