Description of soil NLWSH~~~~~N (Whetstone Hill)
Classification | GL.HFP |
---|---|
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 | -5 | 0 | LF | 0.38 | 0 | -9 | -9 | -9 | - | -9 | 28.0 | -9 | -9 | 3.2 | 3.6 | 0 | 0 | 120 | 0 | 50.0 | 90 | 40 | 30 | 10 | |||
2 | 0 | 2 | A | egj | 1.45 | 0 | 60 | 31 | 9 | F | 15 | 0.4 | -9 | -9 | 3.4 | 4.0 | 0 | 0 | 7 | 0 | 7.0 | 33 | 20 | 16 | 7 | ||
3 | 2 | 35 | B | fgj | 1.52 | 0 | 65 | 24 | 11 | F | 18 | 1.6 | -9 | -9 | 4.9 | 5.3 | 92 | 0 | 13 | 0 | 7.0 | 28 | 18 | 15 | 7 | ||
4 | 35 | 100 | BC | cgj | 1.62 | 0 | 79 | 10 | 11 | F | 19 | 0.4 | -9 | -9 | 5.0 | 5.5 | 99 | 0 | 8 | 0 | 7.0 | 23 | 15 | 12 | 7 |