Description of soil NLMLV~~~~~N (Millville)
| Classification | O.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 | Non growing season The water table is present in the soil during the non growing season. |
| 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. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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 | -25 | -20 | O | m | 0.32 | 0 | -9 | -9 | -9 | - | -9 | 43.0 | 4 | 4 | 5.5 | 5.8 | 99 | 0 | 130 | 0 | 5.0 | 95 | 60 | 50 | 25 | ||
| 2 | -20 | 0 | O | h | 0.49 | 0 | -9 | -9 | -9 | - | -9 | 48.0 | 7 | 5 | 5.3 | 5.6 | 99 | 0 | 150 | 0 | 0.1 | 80 | 75 | 65 | 5 | ||
| 3 | 0 | 12 | A | eg | 1.5 | 8 | 71 | 25 | 4 | F | 19 | 2.8 | -9 | -9 | 5.5 | 6.4 | 99 | 0 | 17 | 0 | 7.0 | 40 | 21 | 15 | 5 | ||
| 4 | 12 | 28 | B | mgj | 1.39 | 9 | 53 | 41 | 6 | VF | 17 | 3.9 | -9 | -9 | 5.2 | 6.6 | 99 | 0 | 22 | 0 | 7.0 | 43 | 26 | 21 | 6 | ||
| 5 | 28 | 58 | B | g | 1.4 | 9 | 55 | 39 | 6 | VF | 18 | 1.5 | -9 | -9 | 5.1 | 6.2 | 99 | 0 | 12 | 0 | 7.0 | 43 | 26 | 20 | 6 | ||
| 6 | 58 | 100 | C | g | 1.4 | 0 | 59 | 33 | 8 | VF | 21 | 0.1 | -9 | -9 | 5.2 | 6.4 | 99 | 0 | 6 | 0 | 0.2 | 42 | 25 | 20 | 7 | ||