Description of soil MBCWB~~~~~N (Cowan Bay)
Classification | R.G |
---|---|
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 | Fourth layer The growth of plant roots is restricted by the fourth layer. |
Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
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 | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Weakly Calcareous < 6 CaCO3 equivalent (%) |
Below | Limestone Limestone bedrock (limestone and dolomite) |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | -15 | -5 | O | f | 0.09 | 0 | -9 | -9 | -9 | - | -9 | 54.8 | 2 | 0 | 5.0 | 5.5 | 58 | 0 | 112 | 0 | 30.0 | 95 | 45 | 40 | 12 | ||
2 | -5 | 0 | O | h | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 44.4 | 8 | 0 | 7.0 | 7.4 | 88 | 2 | 200 | 0 | 0.03 | 90 | 75 | 65 | 20 | ||
3 | 0 | 20 | C | kg | 1.7 | 58 | 53 | 30 | 17 | F | 4 | 2.0 | -9 | -9 | 7.4 | 7.8 | 100 | 9 | 30 | 0 | 60.0 | 36 | 15 | 11 | 4 | ||
4 | 20 | 100 | R | 2.8 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 |