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Soil Properties

Soil is formed from different-sized particles. Soil texture states to the dimensions of the particles that structure the soil and depends on the proportion of sand, silt and clay-sized particles and organic matter within the soil. Sandy soils feel persistent when rubbed between your fingers. Silts feel smooth – a touch like flour. Most clays are adhesive and mouldable. If you’ve ever used pottery clay, you’ll recognise the sense.

 

Soils are made from diverse combinations of sand, silt and clay particles. Soils that are a mixture of sand, silt and clay are called loams. The name of the soil often recognises the dominant particle, for instance , Timaru silt loam describes a soil that features a predominance of silt. Other samples of New Zealand soils are Waikare clay and Te Kopuru sand.

 

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