introduction-weak-interaction-volume-one
introduction-weak-interaction-volume-one
introduction-weak-interaction-volume-one
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CHAPTER THREE : vCLEAR BETA DECAY .<br />
3 .1 Phenoscnolcg of Beta Bees .<br />
In 1896 Becquerel (1) found an ionizing radiation issuing from uraniu m<br />
salts . In 1899 Giesel (2) demonstrated that it was deflected by a magneti c<br />
field, and it 1900 the Curies (3) showed that it consisted of a stream of<br />
negatively-charged particles . In the same year Becquerel (4) obtained a value<br />
for the charge-to-mass ratio, e/a, for the new radiation, and by 1903 mien had<br />
made a first estimate for the magnitude of their charge (5) . Rutherford name d<br />
tt .s radiation 'beta radiation' (6) in 1902, and by 1904 the experiments of<br />
Kaufmann (7), Bestelmeyer (8) and Bucherer (9) had confirmed that it consiste d<br />
of a stream of high-energy electrons whose mass varied in the manner prescribe d<br />
by relativity.<br />
At first, absorption experiments seemed to indicate that the electron s<br />
emitted in the beta decay of nuclei were monoenergetic, but in 1909 Wilson (10 )<br />
showed that they did, in fact, have a wide range of velocities . Von Baeyer ,<br />
Hann and iH .eitner (11) found that there existed seversl distinct velocity group s<br />
in the beta rays emitted from mesothorium two . The much more accurate method<br />
of the Dempster mass spectrograph was used by Rutherford and Robinson (12) i n<br />
1913, she found a number of well-defined lines in the beta ray spectrum o f<br />
radium B and C . The principle of the mass spectrograph was to place th e<br />
radioactive source to be analysed, in the forum of a thin wire, at the edge o f<br />
a uniform magnetic field, so that the emitted beta rays would be bent roun d<br />
in semicircles whose radii were inversely proportional to their velocity . The<br />
distribution of the deflected beta rays was recorded by means of a photographi c<br />
plate . In 1914, Chadwick (13) showed that two types of beta ray spectra<br />
existed, continuous spectra and line spectra. The line spectra were explained<br />
as being due to the removal of extranuclear atomic electrons from their shell s<br />
by high-energy gamma rays from the disintegrating nucleus .<br />
However, the existence of continuous beta ray spectra posed a problem .<br />
If the nuclei in the initial and final states in the decay had unique characteristic