Effects of soil acidification and subsequent leaching on levels of extractable nutrients in a soil |
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Authors: | R J Haynes R S Swift |
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Institution: | (1) Agricultural Research Division, Ministry of Agriculture and Fisheries, Lincoln, P.O. Box 24, Canterbury, New Zealand;(2) Department of Soil Science, Lincoln College, Canterbury, New Zealand |
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Abstract: | Summary The effects of soil acidification (pH values from 6.5 to 3.8), and subsequent leaching, on levels of extractable nutrients
in a soil were studied in a laboratory experiment. Below pH 5.5, acidification resulted in large increases in the amounts
of exchangeable Al in the soil. Simultaneously, exchangeable cations were displayed from exchange sites and Ca, Mg, K and
Na in soil solution increased markedly. With increasing soil acidification, increasing amounts of cations were leached; the
magnitude of leaching loss was in the same order as the cations were present in the soil: Ca2+>Mg2+>K+>Na+.
Soil acidification appeared to inhibit nitrification since in the unleached soils, levels of NO
3
−
clearly declined below pH 5.5 and at the same time levels of NH
4
+
increased greatly. Significant amounts of NH
4
+
and larger amounts of NO
3
−
, were removed from the soil during leaching. Concentrations of NaHCO3-extractable phosphate remained unchanged between pH 4.3 and 6.0 but were raised at higher and lower pH values. No leaching
losses of phosphate were detected. For the unleached soils, levels of EDTA-extractable Mn and Zn increased as the soil was
acidified whilst levels of extractable Fe were first decreased and then increased greatly and those for Cu were decreased
slightly between pH 6.5 and 6.0 and then unaffected by further acidification. Significant leaching losses of Mn and Zn were
observed at pH values below 5.5 but losses of Fe were very small and those of Cu were not detectable. |
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Keywords: | Acidification Extractable micronutrients Fe Mn Zn Cu Extractable P Exchangeable cations Ca Mg K Na Mineral N |
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