Description of soil PEEGMEFK~~A (Egmont)
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. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | 0 | 15 | A | pg | 1.2 | 1 | 37 | 38 | 25 | F | 10 | 4.1 | -9 | -9 | 5.7 | 6.2 | 96 | 0 | 26 | 0 | 1.4 | 55 | 44 | 43 | 29 | ||
2 | 15 | 25 | B | g | 1.75 | 1 | 43 | 34 | 23 | F | 10 | 0.1 | -9 | -9 | 6.9 | 7.4 | 96 | 0 | 14 | 0 | 0.6 | 34 | 31 | 29 | 16 | ||
3 | 25 | 56 | B | tg | 1.75 | 2 | 31 | 40 | 29 | F | 9 | 0.1 | -9 | -9 | 7.2 | 7.7 | 100 | 0 | 16 | 0 | 0.1 | 34 | 31 | 29 | 20 | ||
4 | 56 | 71 | BC | 1 | 1.88 | 11 | 1 | 43 | 56 | F | 0 | 0.0 | -9 | -9 | 7.3 | 7.8 | 100 | 0 | 21 | 0 | 0.1 | 33 | 31 | 28 | 22 | ||
5 | 71 | 91 | BC | 2 | 1.88 | 6 | 3 | 54 | 43 | F | 0 | 0.0 | -9 | -9 | 7.3 | 7.8 | 100 | 0 | 20 | 0 | 0.05 | 34 | 30 | 28 | 18 | ||
6 | 91 | 100 | C | k | 1.87 | 5 | 2 | 55 | 43 | F | 0 | 0.0 | -9 | -9 | 7.3 | 7.8 | 100 | 0 | 20 | 0 | 0.02 | 33 | 31 | 28 | 17 |