Description of soil ABRABpt~~~N (RABBIT)
Classification | O.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:
|
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | -20 | 0 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 25.0 | 6 | 3 | 5.2 | 5.7 | 90 | 0 | 95 | 0 | 3.0 | 90 | 65 | -9 | 20 | ||
2 | 0 | 10 | A | e | 1.2 | 0 | 33 | 55 | 12 | F | 12 | 1.0 | -9 | -9 | 5.7 | 6.1 | 90 | 0 | 11 | 0 | 10.0 | 55 | -9 | 23 | 11 | ||
3 | 10 | 18 | AB | gj | 1.3 | 0 | 38 | 42 | 20 | F | 12 | 0.5 | -9 | -9 | 5.8 | 6.2 | 90 | 0 | 14 | 0 | 10.0 | 51 | -9 | 25 | 12 | ||
4 | 18 | 55 | B | tg | 1.45 | 0 | 31 | 39 | 30 | F | 10 | 0.6 | -9 | -9 | 6.0 | 6.4 | 99 | 0 | 20 | 0 | 3.0 | 45 | -9 | 37 | 21 | ||
5 | 55 | 80 | BC | g | 1.4 | 0 | 53 | 22 | 25 | M | 13 | 0.2 | -9 | -9 | 6.2 | 6.6 | 99 | 0 | 16 | 0 | 3.0 | 47 | -9 | 27 | 16 | ||
6 | 80 | 100 | C | kg | 1.4 | 0 | 37 | 34 | 29 | M | 11 | 0.0 | -9 | -9 | 7.4 | 7.6 | 99 | 7 | 17 | 0 | 3.0 | 47 | -9 | 33 | 19 |