Nature Publishing Group, publisher of Nature, and other science journals and reference works
Nature
my account e-alerts subscribe register
   
Monday 23 November 2009
Journal Home
Current Issue
AOP
Archive
Download PDF
References
Export citation
Export references
Send to a friend
More articles like this

Letters to Nature
Nature 166, 601 - 602 (07 October 1950); doi:10.1038/166601a0

An Absolute Method for Measuring the Activity of Radioactive Isotopes

J. P. KEENE

Christie Hospital and Holt Radium Institute, Withington, Manchester 20. July 12.

RADIOACTIVE isotopes are, at the present time, being used in a wide variety of scientific investigations. Thus the development of accurate methods for the assay of these substances is of considerable importance. The three methods in common use involve the Geiger counter, the ionization chamber and the micro-calorimeter; and, although simple in principle, they are quite complicated in practice. It therefore seemed worth while to investigate the possibilities of a new method based on the fact that a flow of beta-particles is equivalent to a current. In the case of a pure beta-emitting isotope, 3.7 times 107 beta-particles are emitted per second per millicurie (by definition), and this is equivalent to a current of 5.93 times 10-12 amp. If the isotope is deposited on a thin foil, mounted in a vacuum to eliminate gas ionization, and an electric field is applied to prevent slow secondary electrons from escaping, then the current flowing from the foil should be a direct measure of the total activity. The accurate measurement of a current in the region of 10-12 amp. is quite feasible, so that in principle it should be possible to measure radioactivity in this way. A preliminary investigation of the method has been completed, and the present communication gives a brief account of the results so far obtained, with particular reference to the effects caused by secondary emission and by ionization of the residual gas.

  1. Gross, W. , and Failla, G. , Bull. Amer. Phys. Soc., 25, No. 3, 18 (1950).



© 1950 Nature Publishing Group
Privacy Policy