Description of soil QCANA31000A (ANACLET)
| Classification | GL.DYB |
|---|---|
| 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 | Fourth layer The growth of plant roots is restricted by the fourth layer. |
| Type of root restricting layer | Lithic Lithic (consolidated bedrock) |
| Drainage | Moderately well drained Water is removed from the soil somewhat slowly in relation to supply. Excess water is removed somewhat slowly due to low perviousness, shallow water table, lack of gradient, or some combination of these. Soils have intermediate to high water storage capacity (5-6 cm) within the control section and are usually medium to fined textured. Precipitation is the dominant water source in medium to fine textured soils; precipitation and significant additions by subsurface flow are necessary in coarse textured soils. |
| Mode of Deposition | Texture | Chemical properties | |
|---|---|---|---|
| Uppermost | 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. |
Medium Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
Extremely / Strongly Acidic pH < 5.6 |
| Middle | Residual Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock. |
Medium Skeletal Medium Skeletal (USDA Texture Classes: VGSL, VGL). |
Extremely / Strongly Acidic pH < 5.6 |
| Lowest | Shale Shale bedrock |
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 | 36 | A | p | 1.35 | 30 | 54 | 27 | 19 | VC | 3 | 3.4 | -9 | -9 | 6.0 | 6.4 | 100 | 0 | 16 | 0 | 5.0 | 34 | 23 | 20 | 10 | ||
| 2 | 36 | 48 | B | m | 1.4 | 40 | 50 | 33 | 17 | C | 5 | 0.9 | -9 | -9 | 6.1 | 6.8 | 71 | 0 | 13 | 0 | 5.0 | 28 | 20 | 17 | 8 | ||
| 3 | 48 | 59 | C | 1.6 | 40 | 53 | 34 | 13 | C | 6 | 0.6 | -9 | -9 | 6.1 | 6.8 | 89 | 0 | 13 | 0 | 5.0 | 24 | 17 | 15 | 8 | |||
| 4 | 59 | 100 | R | -9.0 | -9 | -9 | -9 | -9 | - | -9 | -9.0 | -9 | -9 | -9.0 | -9.0 | -9 | -9 | -9 | -9 | -9.0 | -9 | -9 | -9 | -9 | |||