Description of soil SKTHI52~~~A (THUNDER HILL SZ.DGC)
| Classification | SZ.DGC |
|---|---|
| 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 | Never The water table is not present in the soil at any time. |
| Root restrictions | Third layer The growth of plant roots is restricted by the third layer. |
| Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
| 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 |
|---|---|---|
| Residual Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock. |
Very Fine Very Fine (USDA Texture Classes: HC (more than 60% clay). |
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 | 0 | 14 | A | p | 1.2 | 0 | 8 | 30 | 62 | VF | 5 | 4.3 | -9 | -9 | 5.8 | 6.1 | 100 | 0 | 40 | 0 | 0.32 | 55 | -9 | 49 | 29 | ||
| 2 | 14 | 47 | B | tnj | 1.3 | 0 | 8 | 32 | 60 | VF | 4 | 1.2 | -9 | -9 | 5.7 | 6.0 | 100 | 0 | 38 | 1 | 0.36 | 51 | -9 | 47 | 29 | ||
| 3 | 47 | 100 | 2 | C | s | 1.3 | 0 | 4 | 27 | 69 | VF | 2 | 0.6 | -9 | -9 | 6.9 | 7.1 | 100 | 2 | 40 | 5 | 0.23 | 51 | -9 | 47 | 29 | |