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| SREL Reprint #2832 | ||||||||||||||||||
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ACIDITY
Introduction Soil acidification is a natural process that can either be accelerated by certain plants and human activities or slowed down by careful management practices. Industrial and mining activities lead to soil acidification due to acid produced from pyrite oxidation and from acid precipitation caused by the emission of sulfur (S) and nitrogen (N) gases. In managed ecosystems, soil acidification is mainly caused by the release of protons (H+) quring the transformation and cycling of carbon (C), N, and S, and fertilizer reactions. Soil acidification caused by these processes can have adverse impacts where soils are unable to buffer , against further pH decrease. For example, in parts of North America and Europe, soil acidification caused, by acid precipitation has resulted in forest decline and, in some parts of Australia, continuous legume cultivation and inappropriate use of N fertilizer have generate sufficient soil acidity that ceral crop cultivation has had to be abandoned due to aluminum (AI) and manganese (Mn) toxicity.
SREL Reprint #2832 Bolan, N. S., D. Curtin and D. C. Adriano. 2005. Acidity. p. 11-17. In Encyclopedia of Soils in the Environment, edited by D. Hillel. Elsevier Academic Press. Amsterdam, The Netherlands.
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