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The author finds that the peculiar substance he has denominatedozone , and which, reverting to the opinion he originally entertained, he now believes to be a compound of oxygen and hydrogen, is obtained readily and in great abundance by placing phosphorus in immediate contact with water and atmospheric air at a temperature of about 30° Cent., but that none is produced when water is absent. Heat was found to effect, the decomposition of ozone. He infers, both from his own experiments and those of M. Marignac, that the presence of nitrogen, instead of being essential to the formation of ozone, as he formerly believed, does not in reality contribute in any way to the production of that substance.

abstracts of the papers communicated to the royal society of london

On Ozone. By C. F. Schœnbein, Professor of Chemistry at Basle, in a letter to Michael Faraday, Esq., D. C. L., F. R. S. Communicated by Michael Faraday, Esq