Manage soil acidity – South West Victoria (Lower)

The issue

Acid soils result in serious and significant losses in production on Australian farms. Figure 1 highlights the varying degrees to which Victorian soils are affected by acidity.

Figure 1: Surface soil pH across Victoria. (Source: Victorian Resources Online
Figure 1: Surface soil pH across Victoria. (Source: Victorian Resources Online

Acidity not only affects the farming land itself but can result in off-site impacts that affect the wider community. With increasing acidity causing reduced plant growth, water use by the plant population is likely to decrease, increasing the risk of salinity.

Increased run off, removing water soluble nutrients and possible soil movement due to erosion can have detrimental impacts on streams and water quality. The increase in nutrient leaching due to the decreased water use by plants may pollute ground water.

The leaching of nutrients and increased availability of clay minerals such as aluminium and iron can result in soil structure decline with irreversible damage. Clay soils will no longer have the characteristics of a typical clay, being quite plastic, rather they may appear to crumble.

Monitoring the acidity level of your soil by measuring the pH level and applying lime strategically, should be part of routine farm management. This should ensure that the pH is maintained above critical levels. When the pH drops below 5.0 (CaCl2) in the pasture system, productivity starts to decline.

Symptoms of soil acidity

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The symptoms of soil acidity include:

  • Poor plant vigour and therefore reduced growth and yields
  • Uneven pasture growth (especially in acid sensitive plants)
  • Poor establishment and persistence of pasture species
  • Poor nodulation of legumes
  • Stunted root growth
  • Persistence of acid tolerant weeds (eg sorrel)
  • Increased incidence of diseases in the pastures
Acid soils will restrict root access to water and nutrients. Figure 2 indicates the availability of plant nutrients at varying levels of soil acidity. When soil pH drops, aluminium generally becomes more soluble, compounding the problem. As low pH affects microbial activity, some pasture legumes may fail to persist due to the inability of rhizobia to successfully nodulate roots under these conditions. Manganese can also become toxic as pH continues to drop, resulting in further pasture decline.
Figure 2. The effect of pH on the availability of plant nutrients. (Source: Understanding soil pH, NSW Agriculture)
Figure 2. The effect of pH on the availability of plant nutrients. (Source: Understanding soil pH, NSW Agriculture)

Causes of soil acidity

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Soil acidification is a natural process that is accelerated by agricultural practices. Improving soil organic matter levels has many benefits for the agricultural system, but also will also increase the soil pH over time as microbial activity breaks down the organic matter to humus and humic acid. Using nutrients, in particular nitrogen, can have acidifying effects on the soil. The greatest acidifying effect is not utilising the extra feed that is grown by the additions of nutrients. The extra feed that is not utilised, becomes organic matter and slowly breaks down to humic acids.

Most plant material is slightly alkaline, so continual removal of plant material off the farm (removing calcium, magnesium and potassium in particular) either via hay or silage making or by grazing will slowly acidify the soil over time. Hay, especially lucerne hay and legume crops can be major contributors to acidification. Grazing has a lower impact due to many nutrients being returned via urine and dung.

Factors affecting the rate of soil acidification

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Soil type impacts on the rate of soil acidification – pH drops faster in sandy soils. Clay soils have a greater cation exchange capacity and a greater water holding capacity, and so, buffer better against soil acidification.Higher rainfall areas will have faster soil acidification rates as the higher rainfall can increase the rate and intensity of leaching the alkaline nutrients (magnesium, potassium, calcium and nitrate nitrogen) down the soil profile.

The higher use of nitrogen fertilisers and the removal of higher levels of farm produce per hectare (particularly grain and hay) will increase the rate of acidification.

What are the options?

  • Liming
  • Using tolerant species/varieties
  • Reducing the rate of acidification


Liming is the most economical method of addressing soil acidification. The amount of lime required will depend on the acidity of the soil, the quality of the lime being used, and the soil type.

Calculating your lime requirement

(Target pH – soil test pH)/conversion factor = t/ha lime required

Conversion factors

  • 0.26 for clay
  • 0.37 for clay loam
  • 0.47 for sandy clay loam
  • 0.57 for sandy loam

If your soil test shows organic matter level is above 2%, then add an extra 0.4t/ha

Note: the lime rates calculated assume a pure limestone product.

If the neutralising value of the lime is not 100%, then:

Lime to spread (t/ha) = (lime required (t/ha) x 100)/ neutralising value

The neutralising value of a lime is expressed as a percentage of pure calcium carbonate which is given a value of 100%. With a higher neutralising value, less lime can be used. Lime with a higher proportion of small particles will react more quickly to neutralise the acid in the soil.

Using tolerant species/varieties

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Using tolerant species or varieties is only a short term option. Table 1 indicates the acid tolerance of some common pasture species. Although you will get improved production in the short term from these species compared to plants with a lower tolerance, the soil will continue to acidify with associated consequences and eventually may become too acidic for these plants also.

Table 1. Preferred pH range for some common pasture species (Source: Making More From Sheep, tool 6.5 soil health benchmarks and guidelines for managing problem soils)

Plant species

Soil pH (water)

Soil pH (CaCl2)

White clover

6.0 – 7.0

5.3 – 6.3

Sub clover

5.2 – 7.0

4.5 – 6.3

Perennial ryegrass

5.3 – 7.0

4.6 – 6.3

Annual ryegrass

5.3 – 7.0

4.6 – 6.3


5.7 – 7.5

5.0 – 7.8


5.0 – 7.5

4.3 – 6.8


6.0 – 8.0

5.3 – 7.3

Reducing the rate of acidification

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There are a number of actions that will help to reduce the rate of acidification

  • Sow perennial pasture that is deep rooted and has some summer activity. Perennial pastures also help reduce nitrogen leaching through the profile
  • Apply fertilisers wisely. Apply at a rate that matches plant requirements.

Monitor the soil fertility levels to ensure levels are either not building up above plant requirements (more nutrients are then available for leaching from the root zone) or that they are dropping below what is required by the pastures. Use the additional feed that is grown to minimise additions of humic acid to the soil system

  • Feed hay or silage onto the paddock from which it was cut. This helps to recycle the nutrients and alkalinity back from where they were removed
  • Rotate grazing paddocks – this helps remove and distribute alkaline products more evenly around the farm and encourages better pasture growth

Regional Information


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