Description of soil NLHGPE3~~~N (Hungry Grove Pond)
Classification | GL.FHP |
---|---|
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 | Unspecified period The water table is present in the soil during an unspecified period. |
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 Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
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 | -2 | 0 | FH | 0.05 | 0 | -9 | -9 | -9 | - | -9 | 28.0 | -9 | -9 | 3.5 | 4.0 | 0 | 0 | 120 | 0 | 50.0 | 90 | 40 | 30 | 10 | |||
2 | 0 | 6 | A | e | 1.44 | 5 | 80 | 19 | 1 | C | 13 | 1.4 | -9 | -9 | 4.0 | 4.5 | 20 | 0 | 10 | 0 | 25.0 | 43 | 16 | 9 | 2 | ||
3 | 6 | 14 | B | f | 1.46 | 5 | 50 | 44 | 6 | F | 12 | 1.4 | -9 | -9 | 4.4 | 4.9 | 52 | 0 | 11 | 0 | 10.0 | 43 | 27 | 22 | 7 | ||
4 | 14 | 23 | B | fc | 1.46 | 0 | 94 | 0 | 6 | VC | 7 | 2.2 | -9 | -9 | 5.0 | 5.5 | 99 | 0 | 15 | 0 | 15.0 | 40 | 21 | 14 | 6 | ||
5 | 23 | 35 | BC | c | 1.5 | 0 | 60 | 35 | 5 | F | 8 | 0.6 | -9 | -9 | 4.9 | 5.4 | 92 | 0 | 7 | 0 | 7.0 | 37 | 22 | 17 | 5 | ||
6 | 35 | 46 | BC | 1.47 | 0 | 60 | 35 | 5 | F | 15 | 0.3 | -9 | -9 | 4.6 | 5.1 | 68 | 0 | 6 | 0 | 7.0 | 40 | 23 | 18 | 5 | |||
7 | 46 | 100 | C | 1.48 | 0 | 65 | 30 | 5 | F | 13 | 0.6 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 7 | 0 | 0.2 | 38 | 21 | 16 | 5 |