Production, isotopic composition, and atmospheric fate of biologically produced nitrous oxide

Abstract

The anthropogenic production of greenhouse gases and their consequent effects on global climate have garnered international attention for years. A remaining challenge facing scientists is to unambiguously quantify both sources and sinks of targeted gases. Microbiological metabolism accounts for the largest source of nitrous oxide (N₂O), mostly due to global conversion of land for agriculture and massive usage of nitrogen-based fertilizers. A most powerful method for characterizing the sources of N₂O lies in its multi-isotope signature. This review summarizes mechanisms that lead to biological N₂O production and how discriminate placement of ¹⁵N into molecules of N₂O occurs. Through direct measurements and atmospheric modeling, we can now place a constraint on the isotopic composition of biological sources of N₂O and trace its fate in the atmosphere. This powerful interdisciplinary combination of biology and atmospheric chemistry is rapidly advancing the closure of the global N₂O budget.

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