Description of soil ABHGTaa~~~N (HAIGHT)
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 |
---|---|---|
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:
|
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
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 | 10 | A | h | 1 | 1.0 | 0 | 8 | 56 | 36 | F | 4 | 5.0 | -9 | -9 | 6.4 | 6.8 | 99 | 0 | 34 | 0 | 10.0 | 61 | -9 | 40 | 26 | |
2 | 10 | 35 | A | h | 2 | 1.0 | 0 | 9 | 48 | 43 | F | 5 | 5.0 | -9 | -9 | 7.3 | 7.5 | 99 | 0 | 37 | 0 | 10.0 | 61 | -9 | 41 | 28 | |
3 | 35 | 45 | BC | g | 1.3 | 0 | 15 | 43 | 42 | F | 7 | 0.5 | -9 | -9 | 7.5 | 7.7 | 99 | 0 | 26 | 0 | 0.0 | 51 | -9 | 42 | 25 | ||
4 | 45 | 80 | C | gk | 1.3 | 0 | 10 | 45 | 45 | F | 5 | 0.0 | -9 | -9 | 7.3 | 7.5 | 99 | 6 | 26 | 0 | 0.0 | 51 | -9 | 44 | 26 | ||
5 | 80 | 90 | 2 | C | gk | 1 | 1.5 | 0 | 47 | 35 | 18 | M | 13 | 0.0 | -9 | -9 | 7.3 | 7.5 | 99 | 3 | 17 | 0 | 10.0 | 43 | -9 | 28 | 16 |
6 | 90 | 100 | 2 | C | gk | 2 | 1.5 | 0 | 43 | 32 | 25 | M | 12 | 0.0 | -9 | -9 | 7.1 | 7.4 | 99 | 4 | 19 | 0 | 3.0 | 43 | -9 | 32 | 19 |