Nitrite fixation by humic substances: Nitrogen-15 nuclear magnetic resonance evidence for potential intermediates in chemodenitrification

Citation
Ka. Thorn et Ma. Mikita, Nitrite fixation by humic substances: Nitrogen-15 nuclear magnetic resonance evidence for potential intermediates in chemodenitrification, SOIL SCI SO, 64(2), 2000, pp. 568-582
Citations number
65
Categorie Soggetti
Environment/Ecology
Journal title
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
ISSN journal
03615995 → ACNP
Volume
64
Issue
2
Year of publication
2000
Pages
568 - 582
Database
ISI
SICI code
0361-5995(200003/04)64:2<568:NFBHSN>2.0.ZU;2-K
Abstract
Studies have Suggested that NO,, produced during nitrification and denitrif ication, can become incorporated into soil organic matter and, in one of th e processes associated with chemodenitrification, react with organic matter to form trace N gases, including N2O. To gain an understanding of the nitr osation chemistry on a molecular level, soil and aquatic humic substances w ere reacted with N-15-labeled NaNO2, and analyzed by liquid phase N-15 and UC nuclear magnetic resonance (NMR). The International Humic Substances Soc iety (IHSS) Pahokee peat and peat humic acid were also reacted with (NaNO2) -N-15 and analyzed by solid-state N-15 NMR. In Suwannee River, Armadale, an d Laurentian fulvic acids, phenolic rings and activated methylene groups un derwent nitrosation to form nitrosophenols (quinone monoximes) and ketoxime s, respectively. The oximes underwent Beckmann rearrangements to 2 degrees amides, and Beckmann Fragmentations to nitriles. The nitriles in turn under went hydrolysis to 1 degrees amides. Peaks tentatively identified as imine, indophenol, or azoxybenzene nitrogens were clearly present in spectra of s amples nitrosated at pH 6 but diminished at pH 3. The N-15 NMR spectrum of the peat humic acid exhibited peaks corresponding with N-nitroso groups in addition to nitrosophenols, ketoximes, and secondary Beckmann reaction prod ucts. Formation of N-nitroso groups was more significant in the whole peat compared with the peat humic acid. Carbon-13 NMR analyses also indicated th e occurrence of nitrosative demethoxylation in peat and soil humic acids. R eaction of N-15-NH3 fixated fulvic acid with unlabeled NO2- resulted in nit rosative deamination of aminohydroquinone N, suggesting a previously unreco gnized pathway for production of N-2 gas in soils fertilized with NH3.