Description of soil BCALZ~~~~~N (ALEZA)
| Classification | O.LG |
|---|---|
| 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 | Unspecified period The water table is present in the soil during an unspecified period. |
| Root restrictions | Fourth layer The growth of plant roots is restricted by the fourth layer. |
| Type of root restricting layer | Undifferentiated Undifferentiated |
| 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 |
|---|---|---|
| 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). |
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 | -8 | 0 | LFH | 0.11 | 0 | -9 | -9 | -9 | - | -9 | 30.1 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 72 | 0 | 21.0 | 96 | 35 | 21 | 14 | |||
| 2 | 0 | 8 | A | h | 1.08 | 0 | 25 | 60 | 15 | F | 6 | 12.2 | -9 | -9 | 4.6 | 5.1 | 67 | 0 | 69 | 0 | 1.0 | 59 | 41 | 35 | 10 | ||
| 3 | 8 | 18 | A | eg | 1.19 | 0 | 10 | 40 | 50 | F | 0 | 1.7 | -9 | -9 | 4.9 | 5.4 | 72 | 0 | 43 | 0 | 0.3 | 55 | 42 | 39 | 26 | ||
| 4 | 18 | 36 | B | tg | 1 | 1.35 | 0 | 1 | 29 | 70 | F | 0 | 1.0 | -9 | -9 | 5.4 | 5.9 | 76 | 0 | 60 | 0 | 0.3 | 49 | 32 | 29 | 15 | |
| 5 | 36 | 56 | B | tg | 2 | 1.44 | 0 | 1 | 29 | 70 | F | 0 | 0.6 | -9 | -9 | 5.9 | 6.4 | 82 | 0 | 48 | 0 | 0.3 | 46 | 32 | 29 | 15 | |
| 6 | 56 | 76 | B | tg | 3 | 1.31 | 0 | 0 | 30 | 70 | F | 0 | 0.5 | -9 | -9 | 6.3 | 6.7 | 83 | 0 | 43 | 0 | 0.3 | 51 | 32 | 29 | 15 | |
| 7 | 76 | 100 | C | gj | 1.35 | 0 | 1 | 24 | 75 | F | 0 | 0.4 | -9 | -9 | 6.5 | 7.0 | 70 | 0 | 37 | 0 | 0.3 | 49 | 32 | 29 | 15 | ||