Issue 2, 1974

Oxygen-l7 nuclear magnetic resonance. Part I. Oxygen–nitrogen groupings

Abstract

Oxygen-l7 shifts are reported for N2O3, N2O4, MeONO, Me2NNO, NO2+, and NOCl, with 17O in natural abundance. These are compared with literature values of 17O shifts in other oxygen–nitrogen groupings, and with the corresponding nitrogen shifts. The shifts of adjacent oxygen and nitrogen in the same chromophore are roughly in the proportion of their respective values of 〈r–3〉, which gives the dependence of the paramagnetic shielding term (σp) on the radius of the 2p orbitals. The oxygen resonances tend to move downfield as the lowest-energy electronic absorption moves to longer wavelengths, but the scatter is large. The oxygen shielding in XNO and XNO2 compounds (as in RCOX) reflects the conjugative effect of the substituent X. This contrasts with the nitrogen shielding, in which inductive effects are relatively more important. Inductive effects may however be among those responsible for oxygen shift relationships, in certain sets of compound, that differ from the overall trends. The relative importance of the orbital terms that contribute to σp is compared for oxygen and nitrogen in these groupings.

Article information

Article type
Paper

J. Chem. Soc., Dalton Trans., 1974, 202-205

Oxygen-l7 nuclear magnetic resonance. Part I. Oxygen–nitrogen groupings

L. Andersson and J. Mason, J. Chem. Soc., Dalton Trans., 1974, 202 DOI: 10.1039/DT9740000202

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