Description of soil ABHCX~~~~~N (HECTOR)
Classification | R.G |
---|---|
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 | 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. |
Moderately Coarse Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL). |
Moderately / Very Strongly Calcareous 6 - 40 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 | -19 | -11 | O | f | 0.06 | 0 | -9 | -9 | -9 | - | -9 | 45.8 | 3 | 3 | 5.1 | 5.6 | 70 | 0 | 110 | 0 | 60.0 | 95 | 50 | -9 | 15 | ||
2 | -11 | 0 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 37.9 | 5 | 3 | 6.2 | 6.6 | 90 | 0 | 92 | 0 | 3.0 | 90 | 65 | -9 | 20 | ||
3 | 0 | 5 | C | kg | 1 | 1.45 | 2 | 3 | 86 | 11 | F | 1 | 0.9 | -9 | -9 | 6.9 | 7.3 | 99 | 7 | 17 | 0 | 10.0 | 45 | -9 | 39 | 19 | |
4 | 5 | 9 | O | hb | 0.18 | 0 | -9 | -9 | -9 | - | -9 | 24.0 | 7 | 3 | 6.6 | 7.0 | 99 | 0 | 200 | 0 | 3.0 | 80 | 70 | -9 | 30 | ||
5 | 9 | 18 | C | kg | 2 | 1.4 | 1 | 25 | 60 | 15 | F | 17 | 0.9 | -9 | -9 | 7.1 | 7.4 | 99 | 18 | 18 | 0 | 10.0 | 47 | -9 | 32 | 17 | |
6 | 18 | 32 | C | kg | 3 | 1.55 | 0 | 53 | 38 | 9 | F | 16 | 0.7 | -9 | -9 | 7.2 | 7.5 | 99 | 11 | 16 | 0 | 30.0 | 42 | -9 | 23 | 12 | |
7 | 32 | 58 | C | kg | 4 | 1.55 | 20 | 74 | 25 | 1 | M | 5 | 2.3 | -9 | -9 | 7.4 | 7.7 | 99 | 17 | 16 | 0 | 30.0 | 42 | -9 | 10 | 5 | |
8 | 58 | 79 | C | kg | 5 | 1.5 | 25 | 48 | 41 | 11 | M | 5 | 0.3 | -9 | -9 | 7.1 | 7.4 | 99 | 12 | 15 | 0 | 10.0 | 43 | -9 | 25 | 13 | |
9 | 79 | 100 | C | kg | 6 | 1.55 | 20 | 75 | 22 | 3 | M | 7 | 0.7 | -9 | -9 | 7.4 | 7.7 | 99 | 19 | 13 | 0 | 30.0 | 42 | -9 | 12 | 6 |