Details

Autor(en) / Beteiligte

• Yu, Longfei
• Harris, Eliza
• Lewicka-Szczebak, Dominika
• Barthel, Matti
• Blomberg, Margareta R A
• Harris, Stephen J
• Johnson, Matthew S
• Lehmann, Moritz F
• Liisberg, Jesper
• Müller, Christoph
• Ostrom, Nathaniel E
• Six, Johan
• Toyoda, Sakae
• Yoshida, Naohiro
• Mohn, Joachim

Titel

What can we learn from N 2 O isotope data? - Analytics, processes and modelling

Ist Teil von

• Rapid communications in mass spectrometry, 2020-10, Vol.34 (20), p.e8858

Ort / Verlag

England

Erscheinungsjahr

2020

Quelle

Wiley-Blackwell Journals

Beschreibungen/Notizen

• The isotopic composition of nitrous oxide (N O) provides useful information for evaluating N O sources and budgets. Due to the co-occurrence of multiple N O transformation pathways, it is, however, challenging to use isotopic information to quantify the contribution of distinct processes across variable spatiotemporal scales. Here, we present an overview of recent progress in N O isotopic studies and provide suggestions for future research, mainly focusing on: analytical techniques; production and consumption processes; and interpretation and modelling approaches. Comparing isotope-ratio mass spectrometry (IRMS) with laser absorption spectroscopy (LAS), we conclude that IRMS is a precise technique for laboratory analysis of N O isotopes, while LAS is more suitable for in situ/inline studies and offers advantages for site-specific analyses. When reviewing the link between the N O isotopic composition and underlying mechanisms/processes, we find that, at the molecular scale, the specific enzymes and mechanisms involved determine isotopic fractionation effects. In contrast, at plot-to-global scales, mixing of N O derived from different processes and their isotopic variability must be considered. We also find that dual isotope plots are effective for semi-quantitative attribution of co-occurring N O production and reduction processes. More recently, process-based N O isotopic models have been developed for natural abundance and N-tracing studies, and have been shown to be effective, particularly for data with adequate temporal resolution. Despite the significant progress made over the last decade, there is still great need and potential for future work, including development of analytical techniques, reference materials and inter-laboratory comparisons, further exploration of N O formation and destruction mechanisms, more observations across scales, and design and validation of interpretation and modelling approaches. Synthesizing all these efforts, we are confident that the N O isotope community will continue to advance our understanding of N O transformation processes in all spheres of the Earth, and in turn to gain improved constraints on regional and global budgets.