Abstract
RUTHERFORD AND SODDY (Phil. Mag., 1902, p. 582; 1903, p. 453 and 579) pointed out that the almost invariable presence of helium in minerals containing uranium indicated that that gas might be one of the ultimate products of the disintegration of the radio-elements. Rutherford, moreover, determined the mass of the projected particle which constitutes the “α-ray” of radium (Phil. Mag., 1903, p. 177) to be approximately twice as great as that of the hydrogen atom, an observation which points in the same direction. These α-particles are readily absorbed by solids and should accumulate in the solid salts of radium and in the radio-active minerals.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Rights and permissions
About this article
Cite this article
RAMSAY, W., SODDY, F. Gases Occluded by Radium Bromide. Nature 68, 246 (1903). https://doi.org/10.1038/068246d0
Issue date:
DOI: https://doi.org/10.1038/068246d0
This article is cited by
-
Key step in atomic physics 100 years ago today
Nature (2003)
-
The role of gold in alchemy. Part III
Gold Bulletin (1985)
-
Role of Chemistry in the Study of Atomic Transmutation
Nature (1936)