Description of soil ABZSZzdg~~N (MISC.SOLONETZIC)
Classification | DG.SS |
---|---|
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 | Third layer The growth of plant roots is restricted by the third layer. |
Type of root restricting layer | Solonetzic Solonetzic B horizon |
Drainage | Well drained Water is removed from the soil readily but not rapidly. Excess water flows downward readily into underlying pervious material or laterally as subsurface flow. Soils have intermediate available water storage capacity (4-5 cm) within the control section, and are generally intermediate in texture and depth. Water source is precipitation. On slopes subsurface flow may occur for short durations, but additions are equaled by losses. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Undifferentiated mineral A sequence of more than three types of genetic mineral materials outcropping on a steep erosional escarpment. This complex class is to be used where units relating to individual genetic materials cannot be delimited separately at the scale of mapping. It may include colluvium derived from the various genetic materials and resting upon the scarp slope. |
Undifferentiated Undifferentiated |
Undifferentiated Undifferentiated acidity and/or calcareousness |
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 | h | 1.15 | 5 | 40 | 40 | 20 | M | 12 | 3.9 | -9 | -9 | 6.0 | 6.5 | 90 | 0 | 27 | 0 | 30.0 | 57 | -9 | 32 | 19 | ||
2 | 10 | 15 | A | e | 1.35 | 5 | 40 | 40 | 20 | M | 12 | 2.0 | -9 | -9 | 5.5 | 6.0 | 90 | 0 | 22 | 0 | 10.0 | 49 | -9 | 32 | 18 | ||
3 | 15 | 70 | B | nt | 1.65 | 10 | 40 | 25 | 35 | M | 10 | 1.0 | -9 | -9 | 6.5 | 6.9 | 99 | 2 | 25 | 2 | 0.0 | 40 | -9 | 40 | 24 | ||
4 | 70 | 100 | C | ks | 1.45 | 10 | 40 | 30 | 30 | M | 11 | 0.5 | -9 | -9 | 7.5 | 7.7 | 99 | 5 | 22 | 8 | 1.0 | 45 | -9 | 34 | 20 |