Description of soil BCSYSvl~~~N (SAYRES)
| Classification | O.FHP |
|---|---|
| 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 | Sixth layer The growth of plant roots is restricted by the sixth layer. |
| Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
| 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 | |
|---|---|---|---|
| Uppermost | Colluvial Massive to moderately-well stratified, nonsorted to poorly sorted sediments with any range of particle sizes from clay to boulders that have reached their present position only by direct, gravity-induced movement. Processes include slow displacements such as creep and solifluction and rapid movements such as earth flows. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Extremely / Strongly Acidic pH < 5.6 |
| Below | Igneous, acidic Igneous, acidic bedrock (dominantly granite) |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | -15 | 0 | LFH | 0.25 | 5 | -9 | -9 | -9 | - | -9 | 50.5 | -9 | -9 | 2.8 | 3.9 | 13 | 0 | 143 | 0 | 21.0 | 92 | 35 | 21 | 14 | |||
| 2 | 0 | 5 | A | e | 1.4 | 40 | 75 | 21 | 4 | F | 18 | 3.0 | -9 | -9 | 3.5 | 3.7 | 5 | 0 | 14 | 0 | 1.0 | 47 | 30 | 21 | 11 | ||
| 3 | 5 | 22 | B | hf | 1 | 1.4 | 40 | 65 | 27 | 8 | F | 16 | 9.0 | -9 | -9 | 3.7 | 4.2 | 2 | 0 | 46 | 0 | 1.0 | 47 | 30 | 21 | 11 | |
| 4 | 22 | 38 | B | hf | 2 | 1.45 | 40 | 65 | 27 | 8 | F | 16 | 11.6 | -9 | -9 | 4.0 | 4.6 | 1 | 0 | 58 | 0 | 1.0 | 45 | 30 | 21 | 11 | |
| 5 | 38 | 42 | H | b | 0.9 | 40 | -9 | -9 | -9 | - | -9 | 19.9 | -9 | -9 | 4.2 | 4.8 | 1 | 0 | 93 | 0 | 1.0 | 92 | 77 | 37 | 17 | ||
| 6 | 42 | 100 | R | 2.65 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||