Description of soil MBCRNd~~~~A (Crane)
| Classification | T.M |
|---|---|
| Profile | Agricultural soil profile The soil has been disturbed by agriculture. |
| Kind of material | Organic The soil material is primarily composed of organic particles. |
| Water table | Unspecified period The water table is present in the soil during an unspecified period. |
| 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 | Imperfectly drained Water is removed from the soil sufficiently slowly in relation to supply, to keep the soil wet for a significant part of the growing season. Excess water moves slowly downward if precipitation is the major supply. If subsurface water or groundwater, or both, is the main source, the flow rate may vary but the soil remains wet for a significant part of the growing season. Precipitation is the main source if available water storage capacity is high; contribution by subsurface flow or groundwater flow, or both, increases as available water storage capacity decreases. Soils have a wide range in available water supply, texture, and depth, and are gleyed phases of well drained subgroups. |
| Mode of Deposition | Texture | Chemical properties | |
|---|---|---|---|
| Uppermost | Fen Peat These deposits consist of sedge peat derived primarily from sedges with inclusions of partially decayed stems of shrubs formed in a eutrophic environment due to the close association of the material with mineral-rich waters. |
Mesic Mesic |
Medium Acid to Neutral pH 5.6 - 7.4 |
| Below | Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Extremely Calcareous > 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 | 0 | 15 | O | mp | 0.2 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 5 | 0 | 6.7 | 7.2 | 90 | 0 | 90 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
| 2 | 15 | 95 | O | m | 1 | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 56.3 | 5 | 0 | 6.1 | 6.6 | 89 | 0 | 114 | 0 | 3.0 | 90 | 70 | 60 | 15 | |
| 3 | 95 | 118 | O | m | 2 | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 52.2 | 5 | 0 | 5.4 | 5.9 | 79 | 0 | 137 | 0 | 3.0 | 90 | 70 | 60 | 15 | |
| 4 | 118 | 125 | O | h | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 52.5 | 8 | 0 | 5.7 | 6.2 | 87 | 0 | 124 | 0 | 0.03 | 90 | 75 | 65 | 20 | ||
| 5 | 125 | 160 | C | kg | 1.7 | 0 | 41 | 43 | 16 | F | 14 | 0.3 | -9 | -9 | 7.5 | 7.8 | 100 | 53 | 4 | 0 | 1.91 | 37 | 27 | 22 | 11 | ||