Description of soil MBRLL~~~~~N (Rochelle)
Classification | R.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). |
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 | -10 | 0 | O | mk | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 27.0 | 5 | 0 | 7.2 | 7.6 | 100 | 2 | 75 | 0 | 3.0 | 90 | 70 | 60 | 15 | ||
2 | 0 | 15 | C | kg | 1.25 | 0 | 19 | 49 | 32 | F | 6 | 1.0 | -9 | -9 | 7.6 | 7.9 | 100 | 5 | 30 | 0 | 3.0 | 51 | 36 | 29 | 15 | ||
3 | 15 | 30 | A | hkb | 1.4 | 0 | 20 | 50 | 30 | F | 0 | 1.2 | -9 | -9 | 7.8 | 8.1 | 100 | 10 | 28 | 0 | 1.0 | 45 | 36 | 29 | 15 | ||
4 | 30 | 70 | C | kg | 1 | 1.4 | 0 | 15 | 59 | 26 | VF | 10 | 0.9 | -9 | -9 | 7.8 | 8.1 | 100 | 19 | 24 | 0 | 3.0 | 47 | 35 | 28 | 14 | |
5 | 70 | 100 | C | kg | 2 | 1.4 | 0 | 23 | 51 | 26 | VF | 15 | 0.9 | -9 | -9 | 7.8 | 8.1 | 100 | 20 | 20 | 0 | 3.0 | 47 | 35 | 26 | 10 |