The liquefaction of gases : papers / by Michael Faraday, (1823-1845) ; with an appendix consisting of papers by Thomas Northmore on the compression of gases. (1805-1806).

  • Faraday, Michael, 1791-1867.
Date:
1904
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Licence: In copyright

Credit: The liquefaction of gases : papers / by Michael Faraday, (1823-1845) ; with an appendix consisting of papers by Thomas Northmore on the compression of gases. (1805-1806). Source: Wellcome Collection.

Provider: This material has been provided by UCL Library Services. The original may be consulted at UCL (University College London)

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    Noithmore says, having collected about a pint and a half of sulphurous acid gas, I proceeded to con- dense it in the three cubic inch receiver, but after a very few pumps the forcing piston became im- moveable, being completely choked by the operation of the gas. A sufficient quantity had, however, been compressed to form vapour, and a thick slimy fluid, of a dark yellow colour, began to trickle down the sides of the receiver, which immediately evaporated with the most suffocating odour upon the removal of the pressure. xiii. 236. This experiment, Mr. Northmore remarks, corroborates the assertion of Monge and Clouet, that by cold and pressure they had condensed this gas. The fluid above described was evidently contaminated wth oil, but from its evaporation on removing the pressure, and from the now ascertained low pressure of the vapour of sulphurous acid, there can be no hesitation in ad- mitting that it was sulphurous acid liquefied. The results obtained by Mr. Northmore, with chlorine gas and sulphurous acid gas, are referred to by Nicholson, in his Chemical Dictionary, 8vo. Articles, Gas (muriatic acid oxygenized) and Gas (sulphurous acid); and that of chlorine is referred to by Murray, in his System, ii. 550; although at page 405 of the same volume, he says that, only sulphurous acid and ammonia of these gases that are at natural temperatures permanently elastic, have been found capable of this reduction. Carbonic Acid.—Another experiment in which it is very probable that liquid carbonic acid has been produced, is one made by Mr. Babbage, about the year 1813. The object Mr. Babbage had in view, was to ascertain whether pressure would prevent decomposition, and it was expected that either that would be the case, or that decomposition would go on, and the rock be split by the expansive force of carbonic acid gas. The place was Chudley