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Published in Soil Sci Soc Am J 28:773-778 (1964)
© 1964 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Nitrosation of Soil Organic Matter: I. Nature of Gases Evolved During Nitrous Acid Treatment of Lignins and Humic Substances1

F. J. Stevenson and R. J. Swaby2

ABSTRACT

Manometric and infrared studies of the gaseous products formed by reacting HNO2 with humic and fulvic acids, lignins. lignin-building units, and polyphenols showed the presence of N2, N2O, and CO2. In addition, methyl nitrite (CH3ONO) occurred in the gases obtained from lignins and certain phenolic derivatives. The CH3ONO originated through dismutation of phenolic ethers; the CO2 from decarboxylation of aromatic acids and cleavage of ring structures. Aromatic-like substances interfere with the determination of free amino groups in soil organic matter by the Van Slyke nitrous acid method.


NOTES

1 Contribution from the Department of Agronomy, University of Illinois, Urbana, and the Division of Soils, C.S.I.R.O., Adelaide, South Australia. The work was carried out while the senior author was in Australia as a Fulbright Research Scholar. Appreciation is expressed to Miss Grace Banos for performing many of the determinations.

2 Professor of Soil Chemistry, University of Illinois, and Head of Soil Microbiology Section, Division of Soils, C.S.I.R.O., Adelaide, South Australia.

Received for publication April 10, 1964. Accepted for publication May 14, 1964.







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Copyright © 1964 by the Soil Science Society of America.