Description of soil BCDEMlop~~A (DENMAN ISLAND)
| 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 | 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 | 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 |
|---|---|---|
| Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Medium Acid to Neutral pH 5.6 - 7.4 |
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 | -22 | 0 | O | p | 0.23 | 0 | -9 | -9 | -9 | - | -9 | 34.0 | 8 | 7 | 4.9 | 5.5 | 51 | 0 | 100 | 0 | 1.0 | 88 | 78 | 35 | 15 | ||
| 2 | 0 | 13 | A | h | 1.33 | 0 | 42 | 42 | 16 | M | 10 | 5.0 | -9 | -9 | 4.8 | 5.3 | 73 | 0 | 32 | 0 | 14.0 | 50 | 31 | 30 | 14 | ||
| 3 | 13 | 27 | A | egj | 1.41 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 4.8 | 5.3 | 59 | 0 | 6 | 0 | 15.0 | 46 | 22 | 15 | 6 | ||
| 4 | 27 | 38 | B | g | 1 | 1.49 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 5.0 | 5.9 | 57 | 0 | 8 | 0 | 17.0 | 43 | 18 | 12 | 5 | |
| 5 | 38 | 52 | B | g | 2 | 1.46 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 4.9 | 5.6 | 66 | 0 | 11 | 0 | 6.0 | 45 | 26 | 12 | 5 | |
| 6 | 52 | 67 | B | g | 3 | 1.46 | 15 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 5.3 | 6.1 | 66 | 0 | 12 | 0 | 6.0 | 45 | 26 | 20 | 8 | |
| 7 | 67 | 77 | B | g | 4 | 1.49 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 5.4 | 5.9 | 57 | 0 | 10 | 0 | 17.0 | 43 | 18 | 12 | 5 | |
| 8 | 77 | 87 | 2 | CB | g | 1.6 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 5.4 | 6.0 | 78 | 0 | 16 | 0 | 6.0 | 40 | 21 | 16 | 7 | |
| 9 | 87 | 108 | CB | g | 1.6 | 0 | 42 | 42 | 16 | M | 10 | 0.0 | -9 | -9 | 5.6 | 6.2 | 78 | 0 | 14 | 0 | 6.0 | 40 | 21 | 16 | 7 | ||