Summary
A study of transformations of added nitrate nitrogen in an acid sulfate soil under waterlogged conditions indicated that chemical reduction of NO3−N to NH4−N is effected by high concentrations of ferrous iron, released in the soil following flooding and reduction of ferric to ferrous iron.
References
Asami, T. and Kumada, K. 1959 Soil Plant Food5, 141–146.
Berner, R. A. 1971 Principles of Chemical Sedimentology, Mc Graw-Hill Inc., 240 p.
Bremner, J. M. 1965In Agronomy9. Methods of Soil Analysis. Ed. C. A. Black. pp 1149–1178. Am. Soc. Agron. Madison, Wisconsin.
Bremner, J. M. 1965In Agronomy9. Methods of Soil Analysis. Ed. C. A. Black. pp 1179–1237. Am. Soc. Agron. Madison, Wisconsin.
Bremner, J. M. and Bundy, L. G. 1973 Commun. Soil Sci. Plant Anal.4, 285–291.
Bremner, J. M. and Shaw, K. 1955 Analyst80, 626–627.
Buresh, R. J. and Moraghan, J. T. 1976. J. Environ. Qual.5, 320–325.
Day, P. R. 1965In Agronomy9. Methods of Soil Analysis. Ed. C. A. Black. pp 562–566. Am. Soc. Agron. Madison, Wisconsin.
Sahrawat, K. L. 1979 Plant and Soil51, 143–144.
Walkley, A. and Black, I. A. 1934 Soil Sci.37, 29–38.
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Sahrawat, K.L. Is nitrate reduced to ammonium in waterlogged acid sulfate soil?. Plant Soil 57, 147–149 (1980). https://doi.org/10.1007/BF02139652
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DOI: https://doi.org/10.1007/BF02139652