Description of soil SKCNAS~~~~N (CARON O.R)
Classification | O.R |
---|---|
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 | First layer The growth of plant roots is restricted by the first (uppermost) layer. |
Type of root restricting layer | Salinity Salinity (conductivity > 4 dS/m) |
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 |
---|---|---|
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. |
Coarse Coarse (USDA Texture Classes: FS,LCS,LS,LFS,GLS,CBLS). |
Calcareous and Saline Calcareous and Saline |
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 | pksa | 1.3 | 0 | 55 | 27 | 18 | M | 8 | 2.2 | -9 | -9 | 7.5 | 7.6 | 100 | 6 | 22 | 6 | 4.69 | 51 | -9 | 31 | 18 | ||
2 | 10 | 100 | C | ksa | 1.5 | 0 | 69 | 18 | 13 | F | 10 | 0.3 | -9 | -9 | 8.5 | 8.5 | 100 | 16 | 11 | 8 | 15.71 | 43 | -9 | 19 | 11 |