Description of soil NSQUE6~~~~A (Queens)
| Classification | O.LG |
|---|---|
| Profile | Agricultural soil profile The soil has been disturbed 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 | Third layer The growth of plant roots is restricted by the third layer. |
| Type of root restricting layer | Compact Till Compact (Basal) Till |
| 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). |
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 | 0 | 15 | A | p | 1.0 | 10 | 35 | 40 | 25 | F | 10 | 2.0 | -9 | -9 | 5.0 | 6.0 | 100 | 0 | 16 | 0 | 3.0 | 49 | 35 | 30 | 14 | ||
| 2 | 15 | 35 | A | eg | 1.0 | 10 | 35 | 40 | 25 | F | 10 | 0.0 | -9 | -9 | 4.0 | 5.0 | 52 | 0 | 9 | 0 | 7.0 | 49 | 35 | 30 | 14 | ||
| 3 | 35 | 80 | B | tg | 2.0 | 10 | 40 | 35 | 25 | F | 10 | 0.0 | -9 | -9 | 5.0 | 5.0 | 60 | 0 | 10 | 0 | 0.0 | 32 | 27 | 26 | 19 | ||
| 4 | 80 | 100 | C | g | 2.0 | 10 | 35 | 35 | 30 | F | 10 | 0.0 | -9 | -9 | 5.0 | 6.0 | 92 | 0 | 11 | 0 | 0.0 | 29 | 26 | 26 | 23 | ||