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Acidification

What is it?

Acidification is where the pH level of soil decreases and reduces plant vigour. While soil acidification is a natural process (especially in higher rainfall regions), agricultural practices can greatly accelerate the rate of acidification.

Strongly acidic soils are defined as those having a pH less than 4.5 (in water), with a pH of 7 being neutral.

Soil acidity occurs naturally in higher rainfall areas and can vary according to geology, clay mineralogy, soil texture and buffering capacity. Agricultural production also increases acidity through unbalanced nitrogen cycling (excessive use of nitrogen fertilisers and nitrogen leaching) and the continued removal of alkaline plant/animal materials (grain, hay, wool, meat).

Examples of soil degradation - Acidification
A diagrammatic representation of the causes of soil acidity showing the importance of product removal and nitrate leaching in the process

Impact

Acidification of topsoils, and more seriously, subsoils will lead to lower yields, reduced pasture and crop options and contribute to wider catchment problems such as weed infestations, salinity and erosion.

In acidic soils, aluminium, iron and manganese can reach concentrations toxic to the roots and there may be deficiencies in molybdenum, boron, calcium, magnesium and potassium.

The impacts of soil acidity on agriculture and the wider community include: Management

Preventative measures: Corrective measures: Related Links

DPI Information Note AG1182: Acid soils (PDF - 165 KB)
Impact of acid soils in Victoria
Measuring and interpreting soil pH
Soil Acidification in Australia (external link) on the Australian Natural Resources Atlas website