Description of soil MBHCH~~~~~N (Holditch)
| Classification | TY.M |
|---|---|
| Profile | Native soil profile The soil is in native condition (undisturbed by agriculture). |
| Kind of material | Organic The soil material is primarily composed of organic particles. |
| Water table | Always The water table is always present in the soil. |
| Root restrictions | Fifth layer The growth of plant roots is restricted by the fifth layer. |
| Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
| Drainage | Very poorly drained Water is removed from the soil so slowly that the water table remains at or on the surface for the greater part of the time the soil is not frozen. Excess water is present in the soil for the greater part of the time. Groundwater flow and subsurface flow are the major water sources. Precipitation is less important except where there is a perched water table with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are either Gleysolic or Organic. |
| Mode of Deposition | Texture | Chemical properties | |
|---|---|---|---|
| Uppermost | Undifferentiated organic A layered sequence of more than three undifferentiated types of organic material (>30% organic matter by weight). |
Mesic Mesic |
Medium Acid to Neutral pH 5.6 - 7.4 |
| Below | Limestone Limestone bedrock (limestone and dolomite) |
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 | 15 | O | m | 1 | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 48.2 | 5 | 0 | 6.7 | 7.2 | 83 | 0 | 114 | 0 | 3.0 | 90 | 70 | 60 | 15 | |
| 2 | 15 | 75 | O | m | 2 | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 60.0 | 5 | 0 | 6.4 | 6.9 | 92 | 0 | 116 | 0 | 3.0 | 90 | 70 | 60 | 15 | |
| 3 | 75 | 90 | O | m | 3 | 0.14 | 0 | -9 | -9 | -9 | - | -9 | 60.0 | 5 | 0 | 6.2 | 6.7 | 86 | 0 | 143 | 0 | 3.0 | 90 | 70 | 50 | 15 | |
| 4 | 90 | 100 | O | h | 0.15 | 0 | -9 | -9 | -9 | - | -9 | 38.7 | 8 | 0 | 6.3 | 6.8 | 84 | 0 | 136 | 0 | 0.03 | 90 | 75 | 65 | 20 | ||
| 5 | 100 | 110 | R | 2.8 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||