Construct · 1 fields · 1 citations

soil acidification: a standalone construct

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Soil chemistry

the decline in soil pH and buffering as protons from deposition and internal processes such as nitrification and plant uptake displace base cations.

In soil chemistry, soil acidification refers to the decline in soil pH and buffering as protons from deposition and internal processes such as nitrification and plant uptake displace base cations. This meaning comes from Breemen (1984) in Nature.[1]

Unit
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Nearby constructs

base3 fields · 4 citationsjingle · one word, three constructs plant1 fields · 1 citationsanchor · a standalone construct uptake3 fields · 3 citationsjingle · one word, three constructs

References

Breemen, N. v., Driscoll, C. T., & Mulder, J. (1984). Acidic deposition and internal proton sources in acidification of soils and waters. Nature, 307(5952), 599-604. https://doi.org/10.1038/307599a0

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