Description of soil NLCKE~~~~~N (Crooked Feeder)
Classification | R.G |
---|---|
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 | Always The water table is always present in the soil. |
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 |
---|---|---|
Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -23 | -5 | O | f | 0.47 | 0 | -9 | -9 | -9 | - | -9 | 39.0 | 3 | 5 | 3.4 | 3.8 | 0 | 0 | 120 | 0 | 40.0 | 97 | 40 | 30 | 10 | ||
2 | -5 | 0 | O | m | 0.54 | 0 | -9 | -9 | -9 | - | -9 | 43.0 | 6 | 0 | 3.4 | 3.8 | 0 | 0 | 130 | 0 | 5.0 | 95 | 60 | 50 | 25 | ||
3 | 0 | 18 | A | eg | 1.3 | 0 | 59 | 39 | 2 | F | 17 | 0.9 | -9 | -9 | 3.6 | 4.3 | 3 | 0 | 8 | 0 | 7.0 | 31 | 15 | 10 | 2 | ||
4 | 18 | 36 | B | g | 1.45 | 0 | 57 | 34 | 9 | F | 15 | 1.2 | -9 | -9 | 3.9 | 4.8 | 16 | 0 | 11 | 0 | 7.0 | 26 | 16 | 13 | 5 | ||
5 | 36 | 100 | C | g | 1.47 | 0 | 40 | 37 | 23 | F | 12 | 0.2 | -9 | -9 | 4.2 | 4.9 | 36 | 0 | 9 | 0 | 0.2 | 24 | 19 | 17 | 10 |