Description of soil NBLRV374~~N (LORNEVILLE)
| 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 | Always The water table is always present in the soil. |
| Root restrictions | Fifth layer The growth of plant roots is restricted by the fifth layer. |
| Type of root restricting layer | Undifferentiated Undifferentiated |
| Drainage | Very poorly drained Water is removed from the soil so slowly that the water table remains at or on the surface for the greater part of the time the soil is not frozen. Excess water is present in the soil for the greater part of the time. Groundwater flow and subsurface flow are the major water sources. Precipitation is less important except where there is a perched water table with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are either Gleysolic or Organic. |
| Mode of Deposition | Texture | Chemical properties |
|---|---|---|
| Marine Unconsolidated deposits of clay, silt, sand, or gravel that are well to moderately well sorted and well to moderately well stratified (in some places containing shells). The deposits have settled from suspension in salt or brackish water bodies or have accumulated at their margins through shoreline processes such as wave action and longshore drift. Nonfossiliferous deposits may be judged marine if they are located in an area that may reasonably be considered to have contained salt water at the time the deposits were formed. |
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 | -35 | -30 | O | f | 0.08 | -9 | -9 | -9 | -9 | - | -9 | 44.1 | 3 | 15 | 3.9 | 4.4 | 16 | 0 | 125 | 0 | 20.0 | 97 | 60 | 25 | 12 | ||
| 2 | -30 | 0 | O | m | 0.2 | -9 | -9 | -9 | -9 | - | -9 | 48.1 | 5 | 15 | 4.0 | 4.5 | 20 | 0 | 150 | 0 | 2.0 | 92 | 75 | 38 | 18 | ||
| 3 | 0 | 8 | A | eg | 1.2 | 0 | 23 | 48 | 29 | VF | 4 | 1.5 | -9 | -9 | 4.0 | 4.5 | 20 | 0 | 16 | 0 | 20.0 | 55 | 48 | 38 | 17 | ||
| 4 | 8 | 18 | B | g | 1.35 | 7 | 23 | 31 | 46 | VF | 5 | 1.2 | -9 | -9 | 3.9 | 4.4 | 16 | 0 | 19 | 0 | 11.0 | 49 | 42 | 33 | 20 | ||
| 5 | 18 | 28 | B | tg | 1 | 1.67 | 4 | 14 | 30 | 56 | VF | 3 | 0.1 | -9 | -9 | 3.6 | 4.1 | 3 | 0 | 16 | 0 | 0.05 | 35 | 31 | 29 | 23 | |
| 6 | 28 | 100 | B | tg | 2 | 1.65 | 0 | 18 | 35 | 47 | VF | 3 | 0.1 | -9 | -9 | 5.5 | 6.0 | 99 | 0 | 14 | 0 | 0.01 | 38 | 33 | 32 | 23 | |