O R I G I N S O F T H E C O N C E P T I O N S O F I S O T O P E S
377
thorium subsequently produced, after the separation, from the easily separa-
ted mesothorium." (1907, p. 326).
The first part of the thorium disintegration series is shown below with
the average life of each member and the rays expelled in its change.
Thorium Mesothorium
I
Mesothorium
2
2.10
10
years
9.67 years
8.9 hours
Radiothorium Thorium X Emanation, etc.
2.9I years
5.25 days
78 seconds
The separation of thorium and radiothorium and of mesothorium I
and
thorium X by chemical analysis, now as then, are completely impossible.
But each can be obtained alone by a suitable combination of chemical pro-
cesses at suitable intervals of time. The exact procedure is dictated by the
relative periods of the substances to be separated. In this connection it must
be remembered, since the methods of ascertaining the nature of the products
separated are purely radioactive, that it is the relative intensity of the radio-
activity, or the relative number of
α−
or
β−
particles emitted per second, and
not the relative weights, which is of importance. For different radioactive
elements, the radioactivity is proportional to the weight divided by the
period. A rapidly changing substance reforms and attains its equilibrium
value correspondingly quickly, a slowly changing one correspondingly
slowly.*
The ease with which the mesothorium is separated, and the very long
time required for it to reform in substantial amount, is the reason why it was
not discovered in 1902 when thorium X was discovered. It would normally
* Thorium may be obtained, free from radiothorium, by repeated precipitations with
ammonia over an interval sufficient to allow the original radiothorium present to
decay. Mesothorium
1
is obtained free from thorium X from the first filtrate in the
ammonia precipitation after leaving it for a month for the thorium X to decay. Radio-
thorium is obtained free from thorium, by separating the mesothorium, waiting for it
partly to change into radiothorium, and then separating the radiothorium from the
mesothorium, by adding a trace of aluminium or similar substance to serve as a vehicle
in the filtration, and precipitating it with the radiothorium by ammonia. Lastly
thorium X is obtained free from mesothorium either from radiothorium or from
thorium by the ammonia precipitation, in the latter case from the second and successive
precipitations at monthly intervals, the first filtrate containing the mesothorium.
378
1921 F.SODDY
be present only in thorium compounds that have remained undisturbed a
long time since preparation, or purification. This fact had later an important
sequel, as we shall see.
The question, whether these non-separable pairs of radio-elements are
really chemically identical or not, is not of importance in the argument.
What is important is that 15 years ago pairs of radio-elements, actually not
separable by chemical analysis, were in fact separated by successive chemical
analyses at suitable intervals. If these pairs had been consecutive in the series,
instead of being separated by intermediate products of different chemical
character, they must have remained unresolved. Such a case, it seemed, was
known.
The isotopes of uranium
In 1908 Boltwood showed that the relative
α−
ray activities of the various
α−
ray giving products of the uranium series, in equilibrium in natural minerals,
conformed to the expulsion of one
α
-particle per atom disintegrating, ex-
cept in the case of the actinium series (which so was correctly indicated to be
a quite minor branch of the main uranium-radium series), and uranium
itself which gives two
α
-particles per atom disintegrating. This satisfied the
atomic weight difference of 12 units between uranium and radium, which
corresponds with the expulsion in all of 3
α−
particles. Ionium, a long-lived
intermediate product giving
α
-rays and generating radium, accounts for
the third
α
-particle. Thus it appeared that the 2
α−
particles from uranium
were due to two successive
α−
ray changes
Uranium I Uranium II Uranium X Ionium Radium, etc.
and that uranium I and uranium II were consecutive products, completely
similar in chemical character, analogous to thorium and radiothorium,
except that there was no intermediate product of different chemical character
to serve for their separate recognition.
The correctness of the inference that the two
α
-particles are successively
and not simultaneously expelled was established by Marsden and Barret in
1911. They observed the scintillations produced by a uranium compound
on a zinc-suiphide screen, and found no pairs, or any preponderance of
short intervals between scintillations, beyond that required by the theory of
O R I G I N S O F T H E C O N C E P T I O N S O F I S O T O P E S
379
probability for a purely random distribution of intervals. Although the other
inference, that the two uraniums are consecutive successive products, was
theoretically incorrect, because it was later found necessary to place uranium
X between the two uraniums, the practical consequences are unaffected.
Owing to the relatively short period of uranium X in comparison with its
product uranium II, the latter cannot be put into evidence, as radiothorium
was, by separating its parent and allowing it to change. The quantity of
uranium II so formed (divided by its period) is too small to be detected, even
when the uranium X from 20 kilograms of the element uranium is studied.
Even if sufficient uranium could be experimented with, the experiment
would still be rendered difficult, if not impossible, because of the ionium in
the series, which is much shorter-lived than uranium II, and non-separable
from uranium X, just as thorium X is from mesothorium I. This then is a
case to which the experimental method of separation does not apply owing
to the hopelessly unfavourable relation between the periods of the successive
products.
The chemical identity of
different
radio-elements and its implications
Examples of chemically non-separable pairs, or groups, of radio-elements
now began to accumulate very rapidly. Ionium, discovered by Boltwood,
and by Marckwald and Keetman independently, in 1908, which proved to
be the direct parent of radium, was shown to be identical in its chemical
character with thorium. Boltwood separated it from uranium minerals by
adding a little thorium and by separating and purifying the latter. Marck-
wald and Keetman obtained it by precipitating the rare earths in the mineral
with hydrofluoric acid, and found that any of the regular methods for puri-
fying thorium from the rare earths would separate the ionium from the
latter and actinium, but not from thorium. Keetman
2
tried twelve good
methods, all well known to be effective in the purification of thorium,
without effecting the least separation of ionium. He found at the same time
that he could not separate uranium X, either, from the ionium-thorium
mixture, though here, of course, just as with thorium X and mesothorium,
the uranium X, being short-lived, speedily disappears of itself.
Auer von Welsbach also, in 1910, carried out a masterly technical separa-
tion of the ionium and actinium of the "hydrate" fraction obtained from
30,000 kilograms of Joachimsthal pitchblende in the manufacture of radium,
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