Soil acidification

Soil acidification is the buildup of hydrogen cations, which reduces the soil pH. Chemically, this happens when a proton donor gets added to the soil. The donor can be an acid, such as nitric acid, sulfuric acid, or carbonic acid. It can also be a compound such as aluminium sulfate, which reacts in the soil to release protons. Acidification also occurs when base cations such as calcium, magnesium, potassium and sodium are leached from the soil.

Soil acidification naturally occurs as lichens and algae begin to break down rock surfaces. Acids continue with this dissolution as soil develops. With time and weathering, soils become more acidic in natural ecosystems. Soil acidification rates can vary, and increase with certain factors such as acid rain, agriculture, and pollution.^[1]

^ Helyar, K. R.; Porter, W. M. (1989). "2 - Soil Acidification, its Measurement and the Processes Involved". In Robson, A. D. (ed.). Soil Acidity and Plant Growth. Academic Press. p. 61. doi:10.1016/b978-0-12-590655-5.50007-4. ISBN 9780125906555. Retrieved 2020-03-25 – via Google Books.

[1] Helyar, K. R.; Porter, W. M. (1989). "2 - Soil Acidification, its Measurement and the Processes Involved". In Robson, A. D. (ed.). Soil Acidity and Plant Growth. Academic Press. p. 61. doi:10.1016/b978-0-12-590655-5.50007-4. ISBN 9780125906555. Retrieved 2020-03-25 – via Google Books.

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