Description of soil MBKLD1p~~~N (Keld)
| 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 | |
|---|---|---|---|
| Uppermost | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Very Fine Very Fine (USDA Texture Classes: HC (more than 60% clay). |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Shale Shale bedrock |
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 | -30 | 0 | O | m | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 30.0 | 5 | 0 | 6.6 | 7.0 | 95 | 0 | 80 | 1 | 3.0 | 86 | 75 | 60 | 15 | ||
| 2 | 0 | 15 | A | hg | 1.2 | 0 | 23 | 38 | 39 | F | 5 | 5.0 | -9 | -9 | 6.6 | 7.0 | 90 | 0 | 40 | 0 | 0.3 | 53 | 50 | 46 | 21 | ||
| 3 | 15 | 25 | AC | 1.3 | 0 | 24 | 33 | 43 | F | 5 | 3.5 | -9 | -9 | 4.9 | 5.3 | 60 | 0 | 40 | 1 | 0.03 | 49 | 47 | 44 | 21 | |||
| 4 | 25 | 50 | C | g | 1.3 | 0 | 20 | 35 | 45 | F | 5 | 1.0 | -9 | -9 | 4.3 | 4.7 | 53 | 0 | 35 | 1 | 0.03 | 49 | 47 | 44 | 19 | ||
| 5 | 50 | 100 | C | g | 1.4 | 0 | 0 | 30 | 70 | - | 0 | 0.2 | -9 | -9 | 6.5 | 6.9 | 95 | 0 | 40 | 2 | 0.03 | 49 | 47 | 45 | 22 | ||