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26-27 - Meeanee
Soil Properties
| Parent material |
Water deposit (alluvium) of Tutaekuri from greywacke and/or sandstone on lagoon deposits |
| Characteristic site and soil features |
low lying areas on margins of old lagoon which was covered by water in floods and high tides before the 1931 earthquake; silty and clayey alluvium on shelly lagoon sediments |
| Associated soils not shown within map unit at map scale but separated out in more detailed maps. - Sample Location |
23, 24, 25
M |
| Natural drainage and depth to gley and hence to water table after wet periods |
26 poor - <30cm
27 very poor to poor - 0-30 |
| Potential rooting depth, texture, and limiting layer |
26 >45cm silt loam on shelly sandy loam
27 30-45cm clay loam on shelly silt loam |
| Available water capacity |
26 75-100mm
27 35-50mm |
| Infiltration rate |
26 moderate
27 slow
|
| Permeability rate |
26,27 slow |
| Susceptibility of topsoil to pugging and compaction when wet |
26 very high
27 extremely high |
| Unfavourable soil characteristics |
26 slowly permeable lagoon sediments free lime,
high pH (alkaline)
saline
27 as above but heavy topsoil easily compacted and
difficult to manage in wet conditions
slow infiltration
shallow clay loam to shelly sediment |
Soil Management
| Artificial drainage: drain spacing |
26, 27
10 - 20m |
| Cultivate when moist to avoid: compaction |
26, 27 |
Irrigation:-
Recommended method
application rate
Dripper spacing for continuous wetted strip
Amount and frequency |
26, 27 sprinkler to prevent waterlogging
27 slow <4mm/hr if 4 l/hr drippers used
26 60cm
27 70cm27 little (15-25mm), often to prevent
waterlogging |

Meeanee (26,27) (photo D. Bloomer)
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