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11 - Otane Soil Properties | Parent material | Water and slope deposit (colluvium) of hill streams from muddy siltstone | | Characteristic site and soil features | Fan extending from base of Havelock hills with silty topsoils over clay | | Associated soils not shown within map unit at map scale but separated out in more detailed maps. - Sample Location | 12, 32 B | | Natural drainage and depth to gley and hence to water table after wet periods | Poor >30cm | | Potential rooting depth, texture, and limiting layer | 30-45cm silt loam on clay from mudstone | | Available water capacity (AWC) | 30-50mm | | Infiltration rate | if not compacted - moderate if compacted - slow | | Permeability rate | Very slow | | Susceptibility to pugging and compaction when wet | Very high | | Unfavourable soil characteristics | Topsoil easily compacted and difficult to manage in wet conditions perched gley on clay pan at <45cm very slow permeability | Soil Management | Artificial drainage: drain spacing | 11 - 10-20m mole drains above the clay pan may also be used | | Cultivate when moist to avoid: compaction | 11 | Irrigation:-
Recommended method
Dripper spacing for continuous wetted strip
Amount and frequency | 11, sprinkler to prevent waterlogging
11 - 60cm if 4 l/hr drippers used
little, (15-25mm), often to prevent waterlogging |  Otane (11) (photo G. Wood)
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