The natural and artificial disintegration of the elements: An address by Professor Sir Ernest RutherfordRutherford, Ernest
Science
The natural and artificial disintegration of the elements: An address by Professor Sir Ernest Rutherford
Rutherford, Ernest
Atoms; Chemical elements; Radioactivity
One of the most interesting and important methods of throwing light on
nuclear structure is the study of the very penetrating _γ_ rays expelled
by some radioactive bodies. The _γ_ rays are identical in nature with
X-rays, but the most penetrating type of rays consists of waves of much
higher frequency than can be produced in an ordinary X-ray tube. The
work of the last few years has indicated very clearly that the major
part of the _γ_ radiation from bodies like radium B and C originates in
the nucleus. A determination of the frequencies of the _γ_ rays thus
gives us direct information on the modes of vibration of parts of the
nuclear structure. The frequency of some of the softer _γ_ rays excited
by radium B and radium C was measured by the crystal method by
Rutherford and Andrade, but it is difficult, if not impossible, by this
method to determine the frequencies of the very penetrating rays.
Fortunately, due largely to the work of Ellis and Fräulein Meitner, a
new and powerful method has been devised for this purpose. It is well
known that the _β_ rays from radium B and radium C give a veritable
spectrum in a magnetic field, showing the presence of a number of groups
of _β_ rays each expelled with a definite speed. It is clear that each of
the groups of _β_ rays arises from conversion of the energy of a _γ_ ray
of definite frequency into a _β_ ray in one or other of the electronic
levels in the outer atom. The energy ω required to move an electron
from one of these levels to the outside of the atom is known from a
study of X-ray absorption spectra. The frequency ν of the _γ_ ray is
thus given by the quantum relation hν = E + ω, where E is the measured
energy of the _β_ particle.
Since each _γ_ ray may be converted in any one of the known electronic
levels in the outer atom, a single _γ_ ray is responsible for the
appearance of a number of groups of _β_ rays, corresponding to conversion
in the K, L, M, etc., levels. In this way, an analysis of the _β_ ray
spectrum allows us to fix the frequency of the more intense _γ_ rays
which are emitted from the nucleus. The energy of the shortest wave
measured in this way by Ellis corresponds to more than two million
volts, while other evidence shows that probably still shorter waves are
emitted in small quantity from radium C.
Ellis and Skinner have shown that the energies of these rays show
certain combination differences, such as are so characteristic of the
energies of the X-rays arising from the outer electrons. A series of
energy levels may thus be postulated in the nucleus similar in character
to the electron levels of the outer atom, and the _γ_ rays have their
origin in the fall either of an electron or of an _α_ particle between
these levels. This is a significant and important result, indicating
that the quantum dynamics can be applied to the nucleus as well as to
the outer electronic structure.
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