Conclusions
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1.
Isotopic exchange between beryllium, magnesium, calcium, strontium, and barium silicates (MO·SiO2) and molecular oxygen was studied, and it was shown that the exchangeable oxygen is a small proportion (0.1–3%) of the surface oxygen.
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2.
The equivalence of the exchangeable oxygen with respect to exchange with18O was established.
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3.
The oxygen in the free alkali-earth metal oxides which form a separate phase on the surface of the MO·SiO2 primarily participates in the exchange.
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4.
Modification of MO·SiO2 with phosphorus results in a decrease in the mobility of the oxygen.
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Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 11, pp. 2423–2426, November, 1984.
We would like to thank Kh. T. Kakhramanova for recording the IR spectra of the samples and G. V. Antoshin for discussing the results obtained.
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Tkachenko, O.P., Tagiev, D.B., Zul'fugarova, S.M. et al. Isotopic exchange between molecular oxygen and MO·SiO2 . Russ Chem Bull 33, 2213–2216 (1984). https://doi.org/10.1007/BF00948823
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DOI: https://doi.org/10.1007/BF00948823