Publication Details

Category Text Publication
Reference Category Journals
DOI 10.1002/rcm.3098
Title (Primary) A new mathematical approach for calculating the contribution of anammox, denitrification and atmosphere to an N2 mixture based on a 15N tracer technique
Author Spott, O.; Stange, C.F.
Source Titel Rapid Communications in Mass Spectrometry
Year 2007
Department BOPHY
Volume 21
Issue 14
Page From 2398
Page To 2406
Language englisch
Abstract Denitrification and anaerobic ammonium oxidation (anammox) have been identified as biotic key processes of N-2 formation during global nitrogen cycling. Based on the principle of a N-15 tracer technique, new analytical expressions have been derived for a calculation of the fractions of N-2 simultaneously released by anammox and denitrification. An omnipresent contamination with atmospheric N-2 is also taken into account and is furthermore calculable in terms of a fraction. Two different mathematical approaches are presented which permit a precise calculation of the contribution of anammox, denitrification, and atmosphere to a combined N-2 mixture. The calculation is based on a single isotopic analysis of a sampled N-2 mixture and the determination of the N-15 abundance of nitrite and nitrate (simplified approach) or of ammonium, nitrite, and nitrate (comprehensive approach). Calculations are even processable under conditions where all basal educts of anammox and denitrificat! ion (ammonium, nitrite, and nitrate) are differently enriched in N-15. An additional determination of concentrations of dissolved N compounds is unnecessary. Finally, the presented approach is transferable to studies focused on terrestrial environments where N-2 is formed by denitrification and simultaneously by codenitrification or chemodenitrification.
Persistent UFZ Identifier https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=2341
Spott, O., Stange, C.F. (2007):
A new mathematical approach for calculating the contribution of anammox, denitrification and atmosphere to an N2 mixture based on a 15N tracer technique
Rapid Commun. Mass Spectrom. 21 (14), 2398 - 2406 10.1002/rcm.3098