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Soil acidification

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Title: Soil acidification  
Author: World Heritage Encyclopedia
Language: English
Subject: Soil, Umbric horizon, Soil chemistry, Southern Appalachian spruce–fir forest, Forests of the Iberian Peninsula
Collection: Environmental Issues, Soil Chemistry
Publisher: World Heritage Encyclopedia

Soil acidification

Soil acidification is the buildup of hydrogen cations, also called protons, reducing the soil pH. This happens when a proton donor gets added to the soil. The donor can be an acid, such as nitric acid and sulfuric acid (these acids are common components of acid rain). It can also be a compound such as aluminium sulfate, which reacts in the soil to release protons. Many nitrogen compounds, which are added as fertilizer, also acidify soil over the long term because they produce nitrous and nitric acid when oxidized in the process of nitrification.

Acidification also occurs when base cations such as calcium, magnesium, potassium and sodium are leached from the soil. This leaching increases with increasing precipitation. Acid rain accelerates the leaching of bases. Plants take bases from the soil as they grow, donating a proton in exchange for each base cation. Where plant material is removed, as when a forest is logged or crops are harvested, the bases they have taken up are permanently lost from the soil.


  • Plant leaves left on soil 1
  • Rocks in the soil 2
  • Pollution 3
  • Acidifying compounds 4
  • See also 5
  • References 6
    • Footnotes 6.1

Plant leaves left on soil

Many plants produce organic acids. Where plant litter accumulates on or is incorporated to the soil, these acids (including acetic acid, humic acid (see , oxalic acid, and tannic acid) are liberated. This is especially acute in soils under coniferous trees such as pine, spruce and fir, which return fewer base cations to the soil than do most deciduous trees.

Rocks in the soil

Certain parent materials also contribute to soil acidification. Granites and their allied igneous rocks are called "acidic" because they have a lot of free quartz, which produces silicic acid on weathering. Also, they have relatively low amounts of calcium and magnesium. Some sedimentary rocks such as shale and coal are rich in sulfides, which, when hydrated and oxidized, produce sulfuric acid which is much stronger than silicic acid. Many coal spoils are too acidic to support vigorous plant growth, and coal gives off strong precursors to acid rain when it is burned. Marine clays are also sulfide-rich in many cases, and such clays become very acidic if they are drained to an oxidizing state.


Acidification may also occur from nitrogen emissions into the air, as the nitrogen may end up deposited into the soil.[1]

Acidifying compounds

See also


  • Fenn, M. E.; Huntington, T. G.; McLaughlin, S. B.; Eagar, C.; Gomez, A.; Cook, R. B. 2006. Status of soil acidification in North America Journal of Forest Science 52:3-13.


  1. ^ USGS. Acid Soils in Slovakia Tell Somber Tale.
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