Description of soil MBMKL~~~~~N (Moak Lake)
| Classification | O.GL |
|---|---|
| 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 | Never The water table is not present in the soil at any time. |
| 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 | Moderately well drained Water is removed from the soil somewhat slowly in relation to supply. Excess water is removed somewhat slowly due to low perviousness, shallow water table, lack of gradient, or some combination of these. Soils have intermediate to high water storage capacity (5-6 cm) within the control section and are usually medium to fined textured. Precipitation is the dominant water source in medium to fine textured soils; precipitation and significant additions by subsurface flow are necessary in coarse textured soils. |
| Mode of Deposition | Texture | Chemical properties |
|---|---|---|
| Lacustrine Sediment, generally consisting of either stratified fine sand, silt, and clay deposited on the lake bed, or moderately-well sorted, stratified sand and coarse materials that consist of near lake shore or beach deposits. These materials have either settled from suspension in bodies of standing fresh water or accumulated at their margins through wave action. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
Weakly Calcareous < 6 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 | -5 | 0 | LH | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 19.7 | -9 | 0 | 5.1 | 5.5 | 52 | 0 | 58 | 0 | 10.0 | 85 | 70 | 50 | 15 | |||
| 2 | 0 | 5 | A | e | 1.4 | 0 | 36 | 53 | 11 | VF | 33 | 0.1 | -9 | -9 | 5.0 | 5.4 | 63 | 0 | 58 | 0 | 3.0 | 46 | 24 | 18 | 7 | ||
| 3 | 5 | 10 | AB | 1.45 | 0 | 15 | 51 | 34 | VF | 15 | 0.3 | -9 | -9 | 5.1 | 5.5 | 74 | 0 | 15 | 0 | 3.0 | 45 | 42 | 38 | 16 | |||
| 4 | 10 | 23 | B | t | 1.3 | 0 | 8 | 57 | 35 | VF | 8 | 0.6 | -9 | -9 | 6.6 | 7.0 | 100 | 2 | 23 | 0 | 0.3 | 50 | 47 | 43 | 22 | ||
| 5 | 23 | 37 | BC | 1.35 | 0 | 12 | 50 | 38 | VF | 12 | 0.0 | -9 | -9 | 7.5 | 7.9 | 100 | 26 | 21 | 0 | 0.3 | 47 | 44 | 38 | 17 | |||
| 6 | 37 | 50 | C | k | 1 | 1.5 | 0 | 67 | 28 | 5 | VF | 51 | 0.0 | -9 | -9 | 7.4 | 7.8 | 100 | 28 | 2 | 0 | 3.0 | 42 | 22 | 13 | 5 | |
| 7 | 50 | 100 | C | k | 2 | 1.5 | 0 | 32 | 50 | 18 | VF | 32 | 0.0 | -9 | -9 | 7.5 | 7.9 | 100 | 33 | 4 | 0 | 3.0 | 42 | 35 | 22 | 11 | |