Description of soil ABSKF~~~~~N (SKIFF)
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 | |
---|---|---|---|
Uppermost | 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 (%) |
Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Undifferentiated Undifferentiated acidity and/or calcareousness |
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 | -6 | 0 | O | h | 0.18 | 0 | -9 | -9 | -9 | - | -9 | 22.9 | 7 | 3 | 5.3 | 5.8 | 80 | 0 | 65 | 0 | 3.0 | 80 | 70 | -9 | 30 | ||
2 | 0 | 22 | A | eg | 1.35 | 0 | 33 | 49 | 18 | F | 11 | 5.2 | -9 | -9 | 5.3 | 5.8 | 80 | 0 | 27 | 0 | 10.0 | 47 | -9 | 41 | 25 | ||
3 | 22 | 45 | B | tg | 1.55 | 0 | 24 | 43 | 33 | F | 9 | 1.6 | -9 | -9 | 5.9 | 6.4 | 90 | 0 | 23 | 0 | 3.0 | 43 | -9 | 43 | 25 | ||
4 | 45 | 90 | C | kg | 1.35 | 0 | 19 | 48 | 33 | F | 9 | 0.0 | -9 | -9 | 7.6 | 7.8 | 99 | 1 | 22 | 0 | 1.0 | 49 | -9 | 39 | 23 | ||
5 | 90 | 120 | 2 | C | kg | 1.45 | 5 | 33 | 38 | 29 | M | 10 | 0.0 | -9 | -9 | 8.0 | 8.2 | 99 | 9 | 21 | 1 | 3.0 | 45 | -9 | 36 | 21 |