Description of soil ABWWO~~~~~N (WILDWOOD)
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:
|
Very Fine Very Fine (USDA Texture Classes: HC (more than 60% clay). |
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 | -10 | 0 | LFH | 0.1 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 4 | 5 | 5.7 | 6.2 | 85 | 0 | 88 | 0 | 30.0 | 85 | 65 | -9 | 20 | |||
2 | 0 | 5 | A | h | 0.95 | 0 | 9 | 31 | 60 | VF | 7 | 9.5 | -9 | -9 | 5.4 | 5.9 | 80 | 0 | 54 | 0 | 3.0 | 63 | -9 | 50 | 38 | ||
3 | 5 | 15 | A | eg | 1.3 | 0 | 16 | 63 | 21 | VF | 12 | 0.7 | -9 | -9 | 5.3 | 5.8 | 75 | 0 | 10 | 0 | 10.0 | 51 | -9 | 31 | 15 | ||
4 | 15 | 20 | AB | g | 1.35 | 0 | 10 | 52 | 38 | VF | 10 | 0.8 | -9 | -9 | 5.2 | 5.7 | 75 | 0 | 21 | 0 | 10.0 | 49 | -9 | 39 | 22 | ||
5 | 20 | 43 | B | tg | 1 | 1.3 | 0 | 7 | 18 | 75 | VF | 4 | 0.8 | -9 | -9 | 4.9 | 5.4 | 70 | 0 | 42 | 0 | 0.0 | 53 | -9 | 53 | 36 | |
6 | 43 | 76 | B | tg | 2 | 1.3 | 0 | 5 | 22 | 73 | VF | 3 | 0.7 | -9 | -9 | 5.9 | 6.4 | 85 | 0 | 40 | 0 | 0.0 | 54 | -9 | 54 | 35 | |
7 | 76 | 102 | BC | g | 1.25 | 0 | 6 | 24 | 70 | VF | 4 | 0.4 | -9 | -9 | 6.5 | 6.9 | 95 | 0 | 38 | 0 | 0.0 | 53 | -9 | 50 | 33 | ||
8 | 102 | 120 | C | kg | 1.25 | 0 | 6 | 27 | 67 | VF | 4 | 0.0 | -9 | -9 | 7.1 | 7.4 | 99 | 4 | 35 | 0 | 0.0 | 53 | -9 | 49 | 32 |