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16O/18O oxygen isotope exchange kinetics in MnO 4 as probed by 55Mn NMR

  • Kinetics and Mechanism of Chemical Reactions. Catalysis
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Abstract

The effect of the 16O ↔ 18O substitution in the coordination sphere of permanganate anion MnO 4 on the chemical shift of 55Mn nuclei have been studied by 17O and 55Mn NMR. Time constants τ n,k of oxygen exchange in the water–permanganate anion system have been estimated. In nearly neutral solutions (pH ≈ 6.8–7.2), the oxygen exchange time is on the order of tens of hours. Bubbling gaseous HCl through this solution for a few seconds leads to the equilibrium distribution of oxygen isotopes in the manganese coordination sphere. The observed temperature dependences of isotope-induced 55Mn NMR shifts in Mn16 O 1844-n O n (n = 0–4) have been treated as a result of rovibrational averaging of Mn–O bond lengths. The change in the Mn—O bond length in caused by the 16O → 18O isotope substitution is on the order of 10–4 Å.

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Correspondence to V. P. Tarasov.

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Original Russian Text © V.P. Tarasov, G.A. Kirakosyan, 2016, published in Khimicheskaya Fizika, 2016, Vol. 35, No. 8, pp. 15–20.

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Tarasov, V.P., Kirakosyan, G.A. 16O/18O oxygen isotope exchange kinetics in MnO 4 as probed by 55Mn NMR. Russ. J. Phys. Chem. B 10, 582–586 (2016). https://doi.org/10.1134/S1990793116040278

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  • DOI: https://doi.org/10.1134/S1990793116040278

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