Description of soil BCLDRd~~~~A (LADNER)
Classification | HU.LG |
---|---|
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 | Non growing season The water table is present in the soil during the non growing season. |
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. |
Moderately Fine Moderately Fine (USDA Texture Classes: SCL,FSCL,VFSCL,CL,SICL,GSCL,GL,CBCL). |
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 | 0 | 15 | A | p | 1.18 | 0 | 5 | 68 | 27 | VF | 3 | 10.9 | -9 | -9 | 4.7 | 5.6 | 28 | 0 | 36 | 1 | 0.3 | 55 | 39 | 36 | 14 | ||
2 | 15 | 20 | A | eg | 1.25 | 0 | 5 | 72 | 23 | VF | 3 | 1.8 | -9 | -9 | 4.9 | 6.0 | 74 | 0 | 18 | 1 | 0.3 | 53 | 38 | 36 | 14 | ||
3 | 20 | 25 | AB | g | 1.25 | 0 | 5 | 70 | 25 | VF | 3 | 1.0 | -9 | -9 | 5.0 | 5.9 | 72 | 0 | 19 | 1 | 0.3 | 53 | 41 | 36 | 15 | ||
4 | 25 | 42 | B | tg | 1.43 | 0 | 4 | 69 | 27 | VF | 3 | 0.8 | -9 | -9 | 5.4 | 6.3 | 77 | 0 | 21 | 1 | 0.3 | 46 | 40 | 36 | 15 | ||
5 | 42 | 57 | B | tg | 1.43 | 0 | 12 | 65 | 23 | F | 3 | 0.5 | -9 | -9 | 5.4 | 6.1 | 85 | 0 | 21 | 1 | 0.3 | 46 | 40 | 38 | 11 | ||
6 | 57 | 75 | BC | g | 1.4 | 0 | 15 | 65 | 20 | F | 3 | 0.2 | -9 | -9 | 4.2 | 4.9 | 62 | 0 | 18 | 2 | 0.3 | 47 | 45 | 36 | 9 | ||
7 | 75 | 100 | C | g | 1.24 | 0 | 11 | 67 | 22 | F | 1 | 0.2 | -9 | -9 | 3.9 | 4.2 | 54 | 0 | 18 | 3 | 0.3 | 53 | 41 | 36 | 9 | ||
8 | 100 | 140 | C | gs | 1.14 | 0 | 9 | 71 | 20 | F | 3 | 0.0 | -9 | -9 | 3.0 | 3.5 | 34 | 0 | 35 | 6 | 0.3 | 57 | 44 | 39 | 17 |