Description of soil ONPPPZ~~~~A (PHIPPS)
| Classification | O.HG |
|---|---|
| Profile | Agricultural soil profile The soil has been disturbed 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 |
|---|---|---|
| Till (Morainal) Morainal material (till) deposited by glacial ice: a mixture of boulders, sand, silt, and clay. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | 0 | 20 | A | p | 1.25 | 15 | 18 | 55 | 27 | VF | 9 | 2.2 | -9 | -9 | 7.0 | 7.3 | 100 | 0 | 34 | 0 | 0.379 | 53 | 50 | 42 | 17 | ||
| 2 | 20 | 25 | A | e | 1.41 | 20 | 15 | 48 | 37 | VF | 6 | 0.9 | -9 | -9 | 6.8 | 7.2 | 100 | 1 | 31 | 0 | 0.247 | 47 | 40 | 37 | 24 | ||
| 3 | 25 | 60 | B | t | 1.47 | 20 | 16 | 38 | 46 | F | 5 | 0.3 | -9 | -9 | 7.1 | 7.5 | 100 | 0 | 32 | 0 | 0.213 | 45 | 40 | 36 | 29 | ||
| 4 | 60 | 100 | C | k | 1.61 | 25 | 17 | 44 | 39 | VF | 6 | 0.2 | -9 | -9 | 7.6 | 8.0 | 100 | 40 | 27 | 0 | 0.146 | 39 | 35 | 31 | 28 | ||