Description of soil SKBCE34~~~A (BONE CREEK E.BLC)
Classification | E.BLC |
---|---|
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 | Undifferentiated Undifferentiated |
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 | |
---|---|---|---|
Uppermost | Eolian Eolian material deposited by wind: uniform deposit of very fine sand and silt. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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. |
Coarse Coarse (USDA Texture Classes: FS,LCS,LS,LFS,GLS,CBLS). |
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 | 12 | A | p | 1.2 | 0 | 22 | 53 | 25 | VF | 14 | 3.3 | -9 | -9 | 6.3 | 6.6 | 100 | 0 | 29 | 0 | 1.88 | 47 | -9 | 38 | 23 | ||
2 | 12 | 18 | A | e | 1.4 | 0 | 40 | 45 | 15 | VF | 25 | 1.0 | -9 | -9 | 6.3 | 6.6 | 100 | 0 | 20 | 0 | 2.91 | 47 | -9 | 34 | 21 | ||
3 | 18 | 55 | B | t | 1.4 | 0 | 27 | 47 | 26 | VF | 22 | 1.0 | -9 | -9 | 6.2 | 6.5 | 100 | 0 | 20 | 0 | 2.19 | 47 | -9 | 36 | 20 | ||
4 | 55 | 100 | 2 | C | k | 1.5 | 20 | 38 | 38 | 24 | C | 4 | 0.2 | -9 | -9 | 7.7 | 7.8 | 100 | 5 | 14 | 0 | 5.77 | 43 | -9 | 29 | 16 |