Description of soil ABJVEpt~~~N (JARVIE)
Classification | HU.LG |
---|---|
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 |
---|---|---|
Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
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 | -20 | 0 | O | h | 0.18 | -9 | -9 | -9 | -9 | - | -9 | 35.0 | 7 | 10 | 5.8 | 6.4 | 87 | 0 | 100 | 0 | 1.0 | 80 | 70 | -9 | 30 | ||
2 | 0 | 25 | A | heg | 1.1 | 0 | 20 | 55 | 25 | F | 9 | 4.3 | -9 | -9 | 5.9 | 6.5 | 85 | 0 | 30 | 0 | 30.0 | 57 | -9 | 37 | 23 | ||
3 | 25 | 33 | A | eg | 1.3 | 0 | 25 | 60 | 15 | F | 11 | 0.5 | -9 | -9 | 5.8 | 6.4 | 97 | 0 | 10 | 0 | 10.0 | 51 | -9 | 25 | 12 | ||
4 | 33 | 61 | B | tg | 1.4 | 0 | 16 | 50 | 34 | F | 7 | 0.4 | -9 | -9 | 5.3 | 5.9 | 97 | 0 | 25 | 0 | 3.0 | 47 | -9 | 42 | 24 | ||
5 | 61 | 112 | BC | g | 1.45 | 0 | 25 | 45 | 30 | F | 9 | 0.3 | -9 | -9 | 5.5 | 6.1 | 99 | 0 | 27 | 0 | 1.0 | 45 | -9 | 39 | 22 | ||
6 | 112 | 150 | C | kg | 1.4 | 0 | 30 | 50 | 20 | F | 11 | 0.0 | -9 | -9 | 6.7 | 7.2 | 99 | 2 | 20 | 0 | 3.0 | 47 | -9 | 33 | 18 |