Description of soil ABJOP~~~~~N (JOSEPHINE)
Classification | HU.LG |
---|---|
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 | Unspecified period The water table is present in the soil during an unspecified period. |
Root restrictions | No root restricting layer The growth of plant roots is not restricted by any soil layer. |
Type of root restricting layer | n/a Not Applicable |
Drainage | Poorly drained Water is removed so slowly in relation to supply that the soil remains wet for a comparatively large part of the time the soil is not frozen. Excess water is evident in the soil for a large part of the time. Subsurface flow or groundwater flow, or both, in addition to precipitation are the main water sources; there may also be a perched water table, with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are gleyed subgroups, Gleysols, and Organic soils. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Residual Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock. |
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
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 | -3 | 0 | LH | 0.1 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 4 | 5 | 5.1 | 5.6 | 70 | 0 | 97 | 0 | 30.0 | 80 | 60 | -9 | 20 | |||
2 | 0 | 8 | A | h | 1.0 | 0 | 12 | 53 | 35 | F | 6 | 9.1 | -9 | -9 | 5.1 | 5.6 | 84 | 0 | 43 | 0 | 10.0 | 61 | -9 | 45 | 32 | ||
3 | 8 | 11 | A | eg | 1.3 | 0 | 15 | 61 | 24 | F | 7 | 2.0 | -9 | -9 | 4.8 | 5.3 | 89 | 0 | 24 | 0 | 10.0 | 51 | -9 | 37 | 21 | ||
4 | 11 | 20 | AB | g | 1.35 | 0 | 11 | 57 | 32 | F | 5 | 1.4 | -9 | -9 | 4.7 | 5.2 | 78 | 0 | 25 | 0 | 10.0 | 49 | -9 | 40 | 23 | ||
5 | 20 | 51 | B | tg | 1.35 | 0 | 8 | 35 | 57 | F | 5 | 1.1 | -9 | -9 | 4.0 | 4.6 | 60 | 0 | 33 | 0 | 1.0 | 50 | -9 | 50 | 31 | ||
6 | 51 | 69 | BC | g | 1.3 | 0 | 14 | 32 | 54 | F | 7 | 0.9 | -9 | -9 | 3.9 | 4.5 | 59 | 0 | 31 | 0 | 0.0 | 51 | -9 | 45 | 28 | ||
7 | 69 | 100 | C | g | 1.3 | 0 | 13 | 44 | 43 | F | 6 | 0.7 | -9 | -9 | 4.0 | 4.6 | 59 | 0 | 27 | 0 | 0.0 | 51 | -9 | 43 | 25 |