Description of soil SKAQARE~~~A (ASQUITH O.DBC)
Classification | O.DBC |
---|---|
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 | Fourth layer The growth of plant roots is restricted by the fourth layer. |
Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
Drainage | Rapidly drained Water is removed from the soil rapidly in relation to supply. Excess water flows downward if underlying material is pervious. Subsurface flow may occur on steep gradients during heavy rainfall. Soils have low available water storage capacity (2.5-4 cm) within the control section, and are usually coarse textured, or shallow, or both. Water source is precipitation. |
Mode of Deposition | Texture | Chemical properties | |
---|---|---|---|
Uppermost | Fluvial These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
Below | 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). |
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 | 0 | 10 | A | p | 1.4 | 0 | 77 | 13 | 10 | M | 28 | 1.0 | -9 | -9 | 6.8 | 7.0 | 100 | 0 | 12 | 0 | 23.25 | 47 | -9 | 16 | 8 | ||
2 | 10 | 57 | B | m | 1.4 | 0 | 77 | 12 | 11 | F | 26 | 0.8 | -9 | -9 | 7.0 | 7.2 | 100 | 0 | 12 | 0 | 22.52 | 47 | -9 | 14 | 8 | ||
3 | 57 | 70 | C | k | 1.5 | 0 | 84 | 7 | 9 | F | 10 | 0.2 | -9 | -9 | 7.9 | 8.0 | 100 | 6 | 8 | 4 | 31.1 | 43 | -9 | 12 | 7 | ||
4 | 70 | 100 | R | -9.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 |