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Dep. of Agriculture for Northern Ireland, Agricultural and Environmental Science Division, Newforge Lane, Belfast BT9 5PX, UK
Inst. of Soil Science, Chinese Academy of Science, Nanjing, China
*Corresponding author (stevensj{at}dani.gov.uk).
ABSTRACT
Standard procedures for determining 15N in the NH4+ fraction of 2 M KCl soil extracts convert NH4+ to N2 prior to isotope-ratio mass spectrometry. We developed a new gas-phase method for determining 15N in NH4+ by producing N2O. Producing N2O means that atmospheric contamination by N2 at natural abundance is not a problem. The method is more sensitive than other methods at lower enrichments, and as accurate and precise as other methods. Nitrous oxide is produced as a by-product during the oxidation of NH4+ by alkaline OBr–. The reaction is catalyzed by Cu2+ and is pH-dependent. The best practical conditions for producing N2O were when the NH3-absorbing solution contained 0.005 M H2SO4 with 0.5 mM CuSO4, and when the molarity of the NaOH in the NaOBr was 10 M. Background N (0.20 µmol test–1) significantly diluted the theoretical enrichments for amounts of N <10 µmol test–1. Corrected enrichment values were accurate for amounts of NH4+-N
1 µmol test–1. For amounts of NH4+-N
1 µmol test–1, precision was determined with a CV of 5.6% at 0.10 atom % excess and with a CV of 0.3% at 10.00 atom % excess. The method is suitable for any matrix and has the potential for better performance if the background contamination could be lowered.
Received for publication December 6, 1995.
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