Description of soil NLAGT~~~~~N (Aguathuna)
| Classification | FE.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 | 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. |
Fine Skeletal Fine Skeletal (USDA Texture Classes: VGC). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | -15 | O | f | 0.4 | 0 | -9 | -9 | -9 | - | -9 | 39.0 | 2 | 1 | 2.7 | 4.0 | 0 | 0 | 120 | 0 | 40.0 | 97 | 40 | 30 | 10 | ||
| 2 | -15 | 0 | O | m | 0.37 | 0 | -9 | -9 | -9 | - | -9 | 43.0 | 5 | 1 | 2.7 | 4.0 | 0 | 0 | 130 | 0 | 5.0 | 95 | 60 | 50 | 25 | ||
| 3 | 0 | 8 | A | eg | 1.42 | 3 | 29 | 32 | 39 | F | 8 | 3.0 | -9 | -9 | 3.2 | 4.2 | 0 | 0 | 25 | 0 | 7.0 | 45 | 37 | 34 | 24 | ||
| 4 | 8 | 20 | B | tgf | 1.4 | 6 | 25 | 31 | 44 | F | 9 | 0.7 | -9 | -9 | 4.1 | 5.3 | 28 | 0 | 16 | 0 | 0.2 | 44 | 37 | 34 | 25 | ||
| 5 | 20 | 56 | C | g | 1.35 | 8 | 24 | 43 | 33 | F | 8 | 0.2 | -9 | -9 | 5.9 | 6.8 | 99 | 0 | 12 | 0 | 0.2 | 45 | 36 | 32 | 19 | ||
| 6 | 56 | 100 | C | kg | 1.35 | 9 | 26 | 45 | 29 | F | 6 | 0.2 | -9 | -9 | 6.8 | 7.6 | 99 | 0 | 11 | 0 | 0.2 | 45 | 35 | 31 | 17 | ||