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3 - Esk
Soil Properties
| Parent material |
Water deposit (alluvium) from sandstone and/or greywacke |
| Characteristic site and soil features |
Flood plain or low terrace, with deposits of sand laid down since 1867, especially large deposits in 1937 floods Sands overlying permeable older deposits, often stones but maybe heavier textures. If the sands bury impermeable old topsoils they must be deep (>75cm) to be included in this mapping unit |
| Associated soils not shown within map unit at map scale but separated out in more detailed maps. - Sample Location |
1, 4,
H, L |
| Natural drainage and depth to gley and hence to water table after wet periods |
Good
>60cm |
| Potential rooting depth, texture, and limiting layer |
3, >45cm sand on permeable sediments (maybe stones or heavier textures): >75cm sand if on slowly permeable old buried topsoil
3g, 30-45 sand on stones |
| Available water capacity (AWC) |
3, 30-50mm
3g, 20-30mm |
| Infiltration rate |
Rapid |
| Permeability rate |
Rapid, but slow if old buried topsoil |
| Susceptibility to pugging and compaction when wet |
Very low |
| Susceptibility to wind erosion when dry |
Very high |
| Unfavourable soil characteristics |
3, sand topsoil susceptible to wind erosion
rapid infiltration
rapid permeability
3g, <45cm to stones
low AWC |
Soil Management
| Artificial drainage |
3, 3g, none required |
Cultivate when moist to avoid:
wind erosion |
3, 3g |
Irrigation:-
Recommended method
Dripper spacing for continuous wetted strip
Amount and frequency |
3, 3g, sprinkler to prevent water loss
3, 3g, 30cm if 3 l/hr drippers used
3, little (15-25mm), often to prevent water loss
3g, little (10-15mm), often to prevent water loss |

Esk sand, sand on gravel (3, 3g) (photo E. Griffiths)
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