Description of soil NSDGC6~~~~N (Diligence)
Classification | O.LG |
---|---|
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 | 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). |
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 | -7 | 0 | LFH | 0.0 | 0 | -9 | -9 | -9 | - | -9 | 28.0 | -9 | 5 | 4.0 | 4.0 | 5 | 0 | 120 | 0 | 50.0 | 90 | 40 | 30 | 10 | |||
2 | 0 | 25 | A | eg | 1.0 | 10 | 35 | 45 | 20 | F | 10 | 0.0 | -9 | -9 | 4.0 | 5.0 | 52 | 0 | 8 | 0 | 7.0 | 53 | 35 | 30 | 11 | ||
3 | 25 | 40 | B | tg | 2.0 | 10 | 30 | 45 | 25 | F | 10 | 0.0 | -9 | -9 | 5.0 | 5.0 | 60 | 0 | 10 | 0 | 0.0 | 32 | 28 | 26 | 19 | ||
4 | 40 | 100 | C | g | 2.0 | 10 | 25 | 45 | 30 | F | 10 | 0.0 | -9 | -9 | 5.0 | 6.0 | 92 | 0 | 11 | 0 | 0.0 | 29 | 26 | 26 | 23 |