Description of soil NBRCB280~~N (RICHIBUCTO)
Classification | O.HFP |
---|---|
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 | Rapidly drained Water is removed from the soil rapidly in relation to supply. Excess water flows downward if underlying material is pervious. Subsurface flow may occur on steep gradients during heavy rainfall. Soils have low available water storage capacity (2.5-4 cm) within the control section, and are usually coarse textured, or shallow, or both. Water source is precipitation. |
Mode of Deposition | Texture | Chemical properties |
---|---|---|
Glaciomarine Glaciomarine |
Very Coarse Very Coarse (USDA Texture Classes: VCS,CS,S,GS,CBS). |
Extremely / Strongly Acidic pH < 5.6 |
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 | -4 | 0 | LFH | 0.22 | -9 | -9 | -9 | -9 | - | -9 | 40.0 | -9 | 15 | 3.5 | 4.0 | 10 | 0 | 100 | 0 | 50.0 | 92 | 40 | 28 | 13 | |||
2 | 0 | 10 | A | e | 1.2 | 1 | 82 | 13 | 5 | M | 6 | 0.6 | -9 | -9 | 3.8 | 4.7 | 12 | 0 | 5 | 0 | 30.0 | 54 | 21 | 16 | 6 | ||
3 | 10 | 30 | B | f | 1.0 | 1 | 80 | 10 | 10 | M | 4 | 1.5 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 15 | 0 | 50.0 | 61 | 27 | 22 | 11 | ||
4 | 30 | 43 | B | fj | 1.25 | 1 | 84 | 10 | 6 | M | 4 | 0.8 | -9 | -9 | 4.5 | 5.0 | 60 | 0 | 7 | 0 | 40.0 | 52 | 16 | 13 | 7 | ||
5 | 43 | 75 | BC | 1.45 | 1 | 87 | 8 | 5 | M | 4 | 0.4 | -9 | -9 | 4.7 | 5.1 | 76 | 0 | 2 | 0 | 50.0 | 45 | 11 | 7 | 4 | |||
6 | 75 | 100 | C | 1.5 | 1 | 92 | 5 | 3 | M | 4 | 0.1 | -9 | -9 | 4.8 | 5.4 | 52 | 0 | 2 | 0 | 50.0 | 43 | 11 | 7 | 4 |