Description of soil ABALGxt~~~N (ALGAR LAKE)
Classification | O.LG |
---|---|
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 | 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 | |
---|---|---|---|
Uppermost | Glaciolacustrine Used where there is evidence that the lacustrine materials were deposited in contact with glacial ice. One of the following characteristics must be present:
|
Fine Fine (USDA Texture Classes: SC,SIC,C,GSIC). |
Moderately / Very Strongly Calcareous 6 - 40 CaCO3 equivalent (%) |
Below | 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). |
Undifferentiated Undifferentiated acidity and/or calcareousness |
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 | -15 | 0 | O | m | 0.12 | 0 | -9 | -9 | -9 | - | -9 | 40.0 | 5 | 5 | 4.8 | 5.4 | 60 | 0 | 97 | 0 | 3.0 | 90 | 65 | -9 | 20 | ||
2 | 0 | 7 | A | eg | 1.3 | 0 | 32 | 60 | 8 | VF | 20 | 1.0 | -9 | -9 | 4.5 | 5.2 | 53 | 0 | 6 | 0 | 30.0 | 51 | -9 | 23 | 10 | ||
3 | 7 | 25 | B | tg | 1.35 | 0 | 10 | 35 | 55 | F | 5 | 0.5 | -9 | -9 | 4.8 | 4.9 | 73 | 0 | 27 | 0 | 1.0 | 49 | -9 | 49 | 30 | ||
4 | 25 | 40 | BC | g | 1 | 1.3 | 0 | 9 | 34 | 57 | F | 3 | 0.5 | -9 | -9 | 4.6 | 4.8 | 80 | 0 | 30 | 0 | 0.0 | 51 | -9 | 48 | 30 | |
5 | 40 | 70 | BC | g | 2 | 1.25 | 2 | 2 | 34 | 64 | F | 2 | 0.5 | -9 | -9 | 4.4 | 4.7 | 76 | 0 | 35 | 0 | 0.0 | 53 | -9 | 50 | 32 | |
6 | 70 | 85 | C | g | 1.3 | 2 | 8 | 35 | 57 | F | 3 | 0.0 | -9 | -9 | 7.2 | 7.4 | 99 | 0 | 19 | 0 | 0.0 | 51 | -9 | 48 | 30 | ||
7 | 85 | 100 | 2 | C | kg | 1.45 | 5 | 34 | 28 | 38 | F | 7 | 0.0 | -9 | -9 | 7.4 | 7.8 | 99 | 6 | 10 | 0 | 1.0 | 45 | -9 | 38 | 23 |