Description of soil NSMSW82~~~A (Masstown)
Classification | O.GL |
---|---|
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 | Fourth layer The growth of plant roots is restricted by the fourth 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. |
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 | 0 | 24 | A | p | 1.0 | 0 | 49 | 40 | 11 | F | 24 | 1.0 | -9 | -9 | 4.0 | 5.0 | 100 | 0 | 13 | 0 | 0.0 | 47 | 40 | 36 | 8 | ||
2 | 24 | 54 | B | g | 2.0 | 0 | 63 | 29 | 8 | F | 25 | 0.0 | -9 | -9 | 4.0 | 5.0 | 84 | 0 | 6 | 0 | 0.0 | 35 | 28 | 25 | 7 | ||
3 | 54 | 90 | BC | g | 2.0 | 6 | 55 | 36 | 9 | F | 17 | 1.0 | -9 | -9 | 6.0 | 6.0 | 84 | 0 | 7 | 0 | 0.0 | 30 | 24 | 22 | 6 | ||
4 | 90 | 100 | C | g | 2.0 | 0 | 63 | 30 | 7 | VF | 32 | 0.0 | -9 | -9 | 4.0 | 5.0 | 92 | 0 | 6 | 0 | 0.0 | 35 | 27 | 23 | 10 |