Description of soil ABTEP~~~~~N (TEMPEST)
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:
|
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | 0 | 9 | A | hg | 1 | 1.0 | 0 | 19 | 53 | 28 | F | 8 | 5.4 | -9 | -9 | 5.4 | 6.1 | 53 | 0 | 28 | 0 | 30.0 | 61 | -9 | 36 | 23 | |
2 | 9 | 10 | A | hg | 2 | 1.15 | 0 | 20 | 50 | 30 | F | 9 | 4.0 | -9 | -9 | 5.5 | 6.1 | 55 | 0 | 32 | 0 | 10.0 | 55 | -9 | 39 | 25 | |
3 | 10 | 20 | A | eg | 1.3 | 0 | 30 | 50 | 20 | F | 11 | 1.8 | -9 | -9 | 5.6 | 6.2 | 65 | 0 | 18 | 0 | 10.0 | 51 | -9 | 32 | 18 | ||
4 | 20 | 25 | B | tg | 1 | 1.4 | 0 | 15 | 40 | 45 | F | 7 | 1.3 | -9 | -9 | 5.6 | 6.2 | 62 | 0 | 34 | 0 | 1.0 | 47 | -9 | 46 | 28 | |
5 | 25 | 92 | B | tg | 2 | 1.35 | 0 | 15 | 35 | 50 | F | 7 | 0.8 | -9 | -9 | 5.7 | 6.3 | 74 | 0 | 34 | 0 | 1.0 | 49 | -9 | 45 | 28 | |
6 | 92 | 101 | BC | g | 1.35 | 0 | 10 | 50 | 40 | F | 5 | 0.5 | -9 | -9 | 6.0 | 6.5 | 88 | 0 | 23 | 0 | 0.0 | 49 | -9 | 44 | 26 | ||
7 | 101 | 140 | C | kg | 1.35 | 0 | 15 | 50 | 35 | F | 7 | 0.0 | -9 | -9 | 7.4 | 7.6 | 99 | 4 | 20 | 0 | 1.0 | 49 | -9 | 41 | 24 |