Description of soil NTOSB3~~~~N (OSBORN)
Classification | R.SC |
---|---|
Profile | Native soil profile The soil is in native condition (undisturbed by agriculture). |
Kind of material | Unclassified This material was not classified due to an absence of information or an unusual situation, such as rockland or an extremely shallow soil. |
Water table | Not applicable Not applicable. |
Root restrictions | Not applicable Non-applicable (e.g. rock, ice). |
Type of root restricting layer | n/a Not Applicable |
Drainage | Not applicable Drainage not applicable (rock, ice, etc) |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Marine Unconsolidated deposits of clay, silt, sand, or gravel that are well to moderately well sorted and well to moderately well stratified (in some places containing shells). The deposits have settled from suspension in salt or brackish water bodies or have accumulated at their margins through shoreline processes such as wave action and longshore drift. Nonfossiliferous deposits may be judged marine if they are located in an area that may reasonably be considered to have contained salt water at the time the deposits were formed. |
Not Applicable Not Applicable |
Not Applicable Not Applicable |
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 | 33 | C | k | 1 | 9.0 | 30 | 90 | 1 | 9 | M | 1 | 0.6 | -9 | -9 | 7.3 | -9.0 | -9 | 4 | -9 | 1 | -9.0 | -9 | -9 | -9 | -9 | |
2 | 33 | 40 | 2 | C | k | - | 9.0 | -9 | 23 | 73 | 4 | F | 1 | 1.3 | -9 | -9 | 7.3 | -9.0 | -9 | 14 | -9 | 1 | -9.0 | -9 | -9 | -9 | -9 |
3 | 40 | 50 | 2 | C | kz | - | 9.0 | -9 | 7 | 58 | 35 | F | 1 | 1.4 | -9 | -9 | 7.0 | -9.0 | -9 | 16 | -9 | 1 | -9.0 | -9 | -9 | -9 | -9 |