Now take another step. Oxygen, as I showed above, three years
ago in the _Philosophical Magazine_ for 1847, vol. xxxi.,
pp. 410, 415, 416, is magnetic in relation to nitrogen and
other gases. E. Becquerel, without knowing of my results, has
confirmed and extended them in his paper of last year, and
given certain excellent measures. In my paper of 1847 I showed
also that oxygen (like iron and nickel) lost its magnetic power
and its ability of being attracted by the magnet when heated
(p. 417). And I further showed that the temperatures at which
this took place were within the range of common temperature,
for the oxygen of the air--_i.e._ the air altogether--is
increased in magnetic power when cooled to 0° F. (p. 406).
Now I must refer you to the papers themselves for the (to
me) strange results of the incompressibility (magnetically
speaking) of oxygen and the inexpansibility of nitrogen and
other gases; for the description of a differential balance by
which I can compare gas with gas, or the same gas at different
degrees of rarefaction; for the determination of the true
zero, or point between magnetic and diamagnetic bodies; and
for certain views of magnetic conduction and polarity. You
will there find described certain very delicate experiments
upon diamagnetic and very weak magnetic bodies concerning
their action on each other in a magnetic field of equal force.
The magnetic bodies repel each other, and the diamagnetic
bodies repel each other; but a magnetic and a diamagnetic body
_attract_ each other. And these results, combined with the
qualities of oxygen as just described, convince me that it is
able to deflect the lines of magnetic force passing through it
just as iron or nickel is, but to an infinitely smaller amount,
and that its power of deflecting the lines varies with its
temperature and degree of rarefaction.
[Sidenote: ATMOSPHERIC MAGNETISM.]
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