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. Author manuscript; available in PMC: 2017 Nov 15.
Published in final edited form as: Dalton Trans. 2016 Nov 15;45(45):18259–18266. doi: 10.1039/c6dt03860c

Fig. 9.

Fig. 9

N2O formation from the reactions of in situ generated (OEP)Fe(HNO)(5-MeIm) with external NO. (a) spectra of authentic samples of 14N2O (solid line trace, 2237/2212 cm−1), 15N2O (broken line trace, 2167/2142 cm−1), and 15N218O (dotted line trace, 2160/2138 cm−1), (b) spectra of the headspace from the reactions of (solid line trace) (OEP)Fe(HNO)(5-MeIm) with 15N18O, and (broken line trace) (OEP)Fe(H15N18O)(5-MeIm) with NO; the newly formed mixed-isotope N2O bands are highlighted. The solid line trace shows formation of 14N15N18O (2185/2162 cm−1), while the broken line trace shows formation of 15N14N16O (2195/2169 cm−1), (c) IR spectrum of the headspace from the reaction of (OEP)Fe(H15NO)(5-MeIm) with NO. The newly formed bands for the mixed-isotope 15N14N16O bands at 2195/2169 cm−1 are highlighted. The singly labeled N2O gases are also present in the headspace, and provide good internal reference spectra.