Description of soil MBSNT~~~~~N (Sinnott)
Classification | R.HG |
---|---|
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 Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
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 | -12 | 0 | O | m | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 44.1 | 5 | 0 | 5.3 | 5.8 | 73 | 0 | 120 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
2 | 0 | 15 | A | hgj | 1.42 | 3 | 34 | 35 | 31 | F | 9 | 4.6 | -9 | -9 | 7.3 | 7.7 | 100 | 0 | 33 | 3 | 3.0 | 47 | 40 | 31 | 13 | ||
3 | 15 | 25 | AC | 1.5 | 5 | 29 | 33 | 38 | F | 7 | 2.8 | -9 | -9 | 7.5 | 7.8 | 100 | 12 | 32 | 2 | 1.0 | 43 | 43 | 33 | 14 | |||
4 | 25 | 100 | C | kgj | 1.75 | 10 | 36 | 40 | 24 | F | 11 | 0.0 | -9 | -9 | 8.0 | 8.3 | 100 | 26 | 13 | 1 | 1.0 | 34 | 34 | 27 | 12 |