Description of soil MBMCC1~~~~N (McClintock 1)
| Classification | ME.OC |
|---|---|
| Profile | Native soil profile The soil is in native condition (undisturbed by agriculture). |
| Kind of material | Organic The soil material is primarily composed of organic 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 | Cryic Cryic (frozen) horizon |
| 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 | Forest Peat This class is used for forest peatcovered or forest peat-filled areas where the water table is at or above the peat surface. The dominant peat materials are shallow to deep mesic to humic forest and fen peat formed in a eutrophic environment resulting from strong water movement from the margins or other mineral sources. |
Mesic Mesic |
Medium Acid to Neutral pH 5.6 - 7.4 |
| Below | 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:
|
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
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 | 0 | 20 | O | f | 1 | 0.05 | 0 | -9 | -9 | -9 | - | -9 | 56.1 | 2 | 0 | 3.1 | 3.5 | 15 | 0 | 103 | 0 | 30.0 | 95 | 45 | 30 | 12 | |
| 2 | 20 | 35 | O | m | 1 | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 38.7 | 4 | 0 | 3.5 | 3.9 | 40 | 0 | 156 | 0 | 3.0 | 90 | 70 | 60 | 15 | |
| 3 | 35 | 50 | O | f | 2 | 0.08 | 0 | -9 | -9 | -9 | - | -9 | 45.8 | 3 | 0 | 3.3 | 3.7 | 19 | 0 | 120 | 0 | 30.0 | 95 | 45 | 30 | 12 | |
| 4 | 50 | 75 | O | mz | 2 | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 5 | 0 | 5.2 | 5.6 | 65 | 0 | 193 | 0 | -9.0 | -9 | -9 | -9 | -9 | |
| 5 | 75 | 90 | O | fz | 0.1 | 0 | -9 | -9 | -9 | - | -9 | 49.9 | 3 | 0 | 5.6 | 6.0 | 77 | 0 | 200 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 6 | 90 | 130 | O | mz | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 42.0 | 6 | 0 | 5.6 | 6.0 | 77 | 0 | 200 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 7 | 130 | 140 | O | hz | 0.34 | 0 | -9 | -9 | -9 | - | -9 | 29.0 | 8 | 0 | 5.8 | 6.2 | 80 | 0 | 200 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||
| 8 | 140 | 160 | C | kgz | 1.3 | 0 | 4 | 33 | 63 | - | 2 | 0.2 | -9 | -9 | 7.4 | 7.8 | 100 | 15 | 24 | 0 | -9.0 | -9 | -9 | -9 | -9 | ||