An attempt to account for the discrepancy between the actual velocity of sound in air or vapour, and that resulting from theory

Sir Isaac Newton determined from theory that the velocity of the undulations of an elastic medium generally is equal to that which a heavy body acquires in falling by the action of gravity through half the height of a homogeneous atmosphere of that medium; but the actual velocity of sound in atmosph...

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Bibliographic Details
Published in:Abstracts of the Papers Printed in the Philosophical Transactions of the Royal Society of London
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 1837
Subjects:
Online Access:http://dx.doi.org/10.1098/rspl.1830.0276
https://royalsocietypublishing.org/doi/pdf/10.1098/rspl.1830.0276