Description of soil BCNWM12~~~N (NEW MEADOW)
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 | 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. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Weakly Calcareous < 6 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 | -21 | 0 | O | m | 0.13 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 5 | 0 | 5.5 | 5.9 | 70 | 0 | 130 | 0 | 5.2 | 89 | 64 | 29 | 21 | ||
2 | 0 | 19 | A | hg | 1.2 | 0 | 10 | 55 | 35 | F | 3 | 2.2 | -9 | -9 | 6.0 | 6.5 | 91 | 0 | 26 | 0 | 3.0 | 55 | 43 | 39 | 19 | ||
3 | 19 | 100 | C | g | 1.4 | 0 | 10 | 55 | 35 | F | 3 | 0.9 | -9 | -9 | 6.5 | 7.0 | 92 | 0 | 24 | 0 | 3.0 | 47 | 39 | 37 | 23 |