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Many growers face a problem of a low pH of their soil. Some soils are acidic by nature and, in other cases, low pH is the result of prolonged and intensive fertilization and irrigation.


Soil pH below 5.5 might result in reduced yields and damages to the crop. Under these pH conditions, the availability of micronutrients such as manganese, aluminium and iron increases and toxicity problem of micronutrients might occur.

On the other hand, at low soil pH, the availability of other essential nutrients, such as K, Ca and Mg decreases and this might result in deficiencies.   

In growing media,  pH changes are much more rapid than in soils. Although various growing media are available with different baseline/starting pH levels, the effect of fertilization and irrigation on their pH levels can be enormous.


The most commonly used technique to raise the soil pH is applying agricultural lime.  The Solubility of lime is relatively low, so if it is applied only to the soil surface, it usually affects only the top layer of the soil, not more than a few centimeters deep.

But which liming material should you use? What should be the lime application rate? Click here to more about how to choose a liming material and application rate.


In soilless media, lime should be incorporated into the media prior planting and the process is usually logistically difficult. Waiting until after planting only makes it more complicated, because the lime should then be individually applied to each growing container or each plant. Again, due to its very low solubility, it's impossible to apply it through irrigation.


lime-lap-top.jpgSMART! Fertilizer Management Software helps growers to manage their soil and crops 





Unlike lime, potassium carbonate is highly soluble and therefore can be applied by drip irrigation. Due to its high solubility, potassium carbonate can be easily distributed throughout the root zone together with irrigation water and reach deeper soil profile.


In both soils and growing media, potassium carbonate can rapidly affect chemical reactions in the root zone, thus elevate root zone pH.


Irrigation with water that have a low buffering capacity (low bicarbonate content) might drastically decrease pH levels in growing media. In this case, and especially when using inert media, pH drop can present a constant problem.

Applying potassium carbonate periodically, or even regularly, as part of the fertilization program, can prevent the pH drop.


Potassium Carbonate as a Fertilizer:

Potassium carbonate also contributes potassium to the nutrient content of the irrigation water.
Therefore, potassium carbonate can be regarded as a fertilizer and its K contribution should be considered.


When applying potassium carbonate through the irrigation water, it is important to keep the pH below 7.0 in order to avoid emitter clogging.


Sometimes growers need to increase the buffer capacity of the irrigation water, while keeping pH levels low enough. In this case, it is possible to add potassium carbonate to water, and at the same time to acidify the water. The acid will neutralize some of the carbonate ions, while the pH level will still be low enough to prevent emitter clogging.




Prior to applying materials that increase pH, make sure that the low pH is not caused by an inappropriate fertilization regime. Often, an adjustment of such a regime may solve the acidity problem. 


This is especially true for growing media (soilless media): ammonium/nitrate ratio is a major factor that can determine the media pH, and it can be controlled by proper a fertilizers application. 


In soils, intensive fertilization with ammonium-based fertilizers or ammonium-forming fertilizers (urea) may lower soil pH


Other factors affecting soil pH include: 


Parent material - type of rocks from which the soil developed.

Rainfall - soils under high rainfall conditions are more acid than soils formed under dry conditions. 


Soil organic matter - soil organisms are continuously decomposing organic matter. The net effect of their activity is that hydrogen ions are released and the soil becomes more acidic.

Native vegetation - the type of the native vegetation under which the soil was formed affects the pH of the soil. Soils formed under forest vegetation tend to be more acidic.


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