Subsurface acidity: how far has the research advanced? – SA (Webpage)

This Grains Research and Development Corporation (GRDC) webpage explains the difference between soil pH and soil acidification, and the causes of subsurface acidity. Subsurface acidity and stratification (below the top 10 cm) are emerging as serious constraints to crop production across NSW, Victoria, SA and WA. Subsurface acidity cannot be detected with conventional topsoil sampling methods (0-10cm), and targeted sampling to depths at suitable increments is required. Lime rates need to be adjusted to account for subsurface pH, changes in soil texture and organic carbon content down the profile. The efficacy of lime application for treating subsurface issues can be improved by strategic cultivation, deep tillage and soil mixing in sandy soils, and adding organic amendments. Other subsoil constraints (e.g. compaction) should be taken into consideration to maximise treatment impact, along with the risks associated with soil disturbance. While this webpage focuses on South Australian soils, the information is relevant for other southern grain-growing regions. #

Resource Last Updated: March 17, 2026

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