The atom and the Bohr theory of its structure : $b an elementary presentationHolst, Helge
Science
The atom and the Bohr theory of its structure : $b an elementary presentation
Holst, Helge
Atomic theory
The properties of the nucleus determine—(_a_) the radioactive
processes, or explosions of the nucleus, and related processes;
(_b_) collisions, where two nuclei approach extremely near to
each other; and (_c_) weight which, as mentioned above, stands
in direct connection with atomic weight. The properties of the
electron system are, on the other hand, the determining factors in
all other physical and chemical activities, and, as has been stated,
are functions, we may say, of the atomic number of the given element.
The Bohr theory may be said to concern itself with the chemical and
physical properties of the atom with the exception of those which have
to do with the nucleus. We shall consequently devote our attention in
the next chapters to the electron system. But before turning to this we
shall dwell a little further upon the atomic nucleus.
The Structure of the Nucleus.
That the nucleus is not an elementary indivisible particle but a system
of particles, is clearly shown by the radioactive processes in which
α-particles and β-particles (electrons) are shot out of the nuclei of
radioactive elements. Bohr was the first to see clearly that not only
the α-particles emitted in such cases come from the nucleus, but that
the β-particles also have their source there. There is now no doubt
that, in addition to the outer electrons of the atom, which are the
determining factor in the atomic number, there must also be, in the
radioactive substances at any rate, special nuclear electrons which
lead a more hidden existence in the interior of the nucleus. One can
easily understand that isotopes may result as products of radioactive
disintegration. For example, let us suppose that a nucleus emits first
an α-particle (_i.e._ a helium nucleus with two positive charges),
and thereafter sends out two electrons, each with its negative charge,
in two new disintegrations. The nuclear charge in the resultant atom
will then obviously be the same as before, because the loss of the two
electrons exactly neutralizes that of the α-particle. But the atomic
weight will be diminished by four units (i.e. the weight of the helium
nucleus, remembering also that the electrons have but very negligible
masses). Among the radioactive substances are recognized many examples
of isotope elements, with atomic weights differing precisely by four.
The radioactive element uranium is the element with the greatest
atomic weight (238), and atomic number (92), and consequently with the
greatest nuclear charge. Almost all the other radioactive substances
are those with high atomic numbers in the periodic system. The cause
of radioactivity must be sought in the hypothesis that the nuclei
of the radioactive elements are very complicated systems with small
stability, and therefore break down rather easily into less complicated
and more stable systems with the emission of some of their constituent
particles; the corpuscular rays thus produced possess a considerable
amount of kinetic energy.
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