Conclusions
-
1.
The thermal decomposition of ozone was studied within the temperature interval 136–226‡.
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2.
The experimental data were explained by the following reaction mechanism O3+M⇌O2+O+M O+O3=O2+O2
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3.
The rate constant of the latter process k=(2.9±0.9) ·1012.e(−3700±300)/RT, cm3-mole−1· sec−1, was meastured.
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Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 11, pp. 2440–2446, November, 1967.
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Intezarova, E.I., Kondrat'ev, V.N. Thermal decomposition of ozone. Russ Chem Bull 16, 2326–2331 (1967). https://doi.org/10.1007/BF00911837
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DOI: https://doi.org/10.1007/BF00911837