Soils

Western Australia’s agriculture sector needs access to quality soil that can sustain long-term productivity and growth. The department is leading the way in developing management practices to maximise soil productivity and minimise land degradation. The department also provides technical information on managing soil constraints, including acidity, water repellence, subsoil compaction, erosion along with nutrient management. We also support agriculture through soil and land condition monitoring, condition assessment and providing management strategies and tools to improve soil condition.

Articles

  • The whole farm nutrient mapping procedure described here applies to pastures in the greater than 600mm rainfall zone of south-west Western Australia.

  • Controlled traffic farming (CTF) is a farming system built on permanent wheel tracks where the crop zone and traffic lanes are permanently separated.

  • If you are deep-ripping, ploughing or spading to remove subsurface compaction or another constraint, it is a good idea to incorporate lime in the same operation.

  • This page contains information about managing nutrition in canola crops in Western Australia.

  • Cockchafers belonging to the genus Heteronyx are typically not regarded as a pest of agriculture. However, two have been seen as occasional pests, with H.

  • Extensive wind erosion of field pea stubble often follows grazing over summer and autumn. Semi-leafless field pea varieties have reduced lodging, improved pod-height and reduced pod-shatter.

  • Liming to recover an acidic soil to an appropriate pH can result in significant production benefits, however a response to liming indicates that previous production has been lost due to an acidic t

  • The rate of soil acidification due to agriculture can be reduced but not eliminated. Liming will always be needed to prevent the soil from becoming too acidic.

  • Soil acidification occurs naturally very slowly as soil is weathered, but this process is accelerated by productive agriculture.

  • A small decrease in soil pH represents a large increase in soil acidity.

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