Description of soil ONMATH~~~~A (MALTON)
Classification | O.HG |
---|---|
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 | |
---|---|---|---|
Uppermost | Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
Weakly Calcareous < 6 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 | 0 | 18 | A | p | 1.17 | 0 | 25 | 25 | 50 | VF | 16 | 3.0 | -9 | -9 | 7.4 | 6.9 | 100 | 1 | 38 | 0 | 0.497 | 57 | 50 | 43 | 15 | ||
2 | 18 | 30 | B | mgj | 1.39 | 0 | 20 | 37 | 43 | VF | 9 | 1.1 | -9 | -9 | 7.1 | 6.6 | 100 | 1 | 35 | 0 | 0.263 | 48 | 40 | 38 | 26 | ||
3 | 30 | 60 | BC | kg | 1.47 | 0 | 17 | 35 | 48 | VF | 6 | 0.5 | -9 | -9 | 7.3 | 6.8 | 100 | 6 | 34 | 0 | 0.212 | 45 | 40 | 36 | 30 | ||
4 | 60 | 100 | C | kg | 1.61 | 0 | 11 | 29 | 60 | F | 3 | 0.2 | -9 | -9 | 7.5 | 7.0 | 100 | 30 | 38 | 0 | 0.137 | 39 | 38 | 38 | 32 |