Description of soil ABEND~~~~~N (ENILDA)
Classification | O.HG |
---|---|
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 | Always The water table is always present in the soil. |
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 |
---|---|---|
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. |
Medium Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL). |
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 | -5 | 0 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 4 | 2 | 6.1 | 6.5 | 90 | 0 | 120 | 0 | 3.0 | 90 | 65 | -9 | 20 | ||
2 | 0 | 13 | A | h | 1.0 | 0 | 5 | 65 | 30 | VF | 5 | 12.0 | -9 | -9 | 5.9 | 6.2 | 90 | 0 | 30 | 0 | 10.0 | 61 | -9 | 49 | 35 | ||
3 | 13 | 17 | B | g | 1.35 | 0 | 7 | 62 | 31 | VF | 5 | 1.5 | -9 | -9 | 6.1 | 6.5 | 90 | 0 | 23 | 0 | 10.0 | 49 | -9 | 43 | 24 | ||
4 | 17 | 25 | BC | g | 1 | 1.35 | 0 | 4 | 68 | 28 | VF | 4 | 0.8 | -9 | -9 | 6.3 | 6.7 | 90 | 0 | 21 | 0 | 3.0 | 49 | -9 | 43 | 23 | |
5 | 25 | 28 | BC | g | 2 | 1.35 | 0 | 12 | 54 | 34 | VF | 8 | 1.5 | -9 | -9 | 6.0 | 6.4 | 90 | 0 | 23 | 0 | 1.0 | 49 | -9 | 42 | 24 | |
6 | 28 | 40 | BC | g | 3 | 1.3 | 0 | 6 | 44 | 50 | VF | 5 | 0.5 | -9 | -9 | 5.9 | 6.3 | 90 | 0 | 28 | 0 | 0.0 | 51 | -9 | 47 | 28 | |
7 | 40 | 61 | C | g | 1 | 1.55 | 0 | 54 | 27 | 19 | F | 14 | 0.3 | -9 | -9 | 6.5 | 6.9 | 99 | 0 | 17 | 0 | 10.0 | 42 | -9 | 27 | 16 | |
8 | 61 | 76 | C | g | 2 | 1.4 | 0 | 10 | 64 | 26 | VF | 5 | 0.2 | -9 | -9 | 6.5 | 6.9 | 99 | 0 | 20 | 0 | 3.0 | 47 | -9 | 41 | 23 | |
9 | 76 | 100 | C | g | 3 | 1.35 | 0 | 6 | 61 | 33 | VF | 4 | 0.2 | -9 | -9 | 6.5 | 6.9 | 99 | 0 | 22 | 0 | 1.0 | 49 | -9 | 44 | 25 |