A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
History
A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
American journal of science; Science -- United States -- History
It was pointed out by Mendeléeff that, with the exception of series 1
and 2 at the top of the table, the alternate members of the groups show
particularly close relationships. These subordinate groups, marked A and
B, in most cases show remarkable analogies and gradations in their
properties, for example, in the alkali-metals from lithium to cæsium,
and in the halogens from fluorine to iodine. The two divisions of a
group do not usually show very close relations to each other, except in
their valency, and they even display, in several instances, opposite
gradations in chemical activity in the order of their atomic weights.
For instance, cæsium stands at the electro-positive end, while gold
stands at the electro-negative end of its subordinate group. The
difference between the two divisions is very great in Groups VI and VII,
but it is extreme in Group VIII, where heavy metals are on one side and
inactive gases on the other. Many authorities separate these gases into
a “Group O” by themselves at the left-hand side of the table, but this
does not change their relative positions, and the plan may be objected
to on the ground that many vacant places are thus left in the groups
VIII and O.
The periodic law has been useful in rectifying certain atomic weights.
At the outset Mendeléeff was obliged to change beryllium from 14·5
(assuming Be_{2}O_{3}) to 9 (assuming BeO), and later the atomic weights
of indium and uranium were changed to make them fit the system. All of
these changes have been confirmed by physical means.
Mendeléeff found a number of vacant places in his table, and was thus
able to render further service to chemical science by predicting the
properties of undiscovered elements, and his predictions were very
closely confirmed by the later discovery of scandium, gallium, and
germanium. The table indicates that there are still two undiscovered
elements below manganese and probably two more among the rare-earth
metals. The interesting observation has just recently been made by Soddy
that the products of radioactive disintegration appear to pass in a
symmetrical way through positions in the periodic system, giving off a
helium molecule at alternate transformations until the place of lead is
reached. It appears, therefore, that the five vacant places in the table
above bismuth are probably occupied by these evanescent elements, and it
is to be noticed that all of the elements that have been placed in this
region of high atomic weights are radioactive.
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