Essays: Scientific, Political, & Speculative; Vol. 1 of 3: Library Edition (1891), Containing Seven Essays not before Republished, and Various other Additions.Spencer, Herbert
Philosophy
Essays: Scientific, Political, & Speculative; Vol. 1 of 3: Library Edition (1891), Containing Seven Essays not before Republished, and Various other Additions.
Spencer, Herbert
Philosophy; Political science; Science
[Footnote 14: A reference may fitly be made here to a reason given by
Mons. Babinet for rejection of the Nebular Hypothesis. He has calculated
that taking the existing Sun, with its observed angular velocity, its
substance, if expanded so as to fill the orbit of Neptune, would have
nothing approaching the angular velocity which the time of revolution of
that planet implies. The assumption he makes is inadmissible. He
supposes that all parts of the nebulous spheroid when it filled
Neptune's orbit, had the same angular velocities. But the process of
nebular condensation as indicated above, implies that the remoter
flocculi of nebulous matter, later in reaching the central mass, and
forming its peripheral portions, will acquire, during their longer
journeys towards it, greater velocities. An inspection of one of the
spiral nebulæ, as 51st or 99th Messier, at once shows that the outlying
portions when they reach the nucleus, will form an equatorial belt
moving round the common centre more rapidly than the rest. Thus the
central parts will have small angular velocities, while there will be
increasing angular velocities of parts increasingly remote from the
centre. And while the density of the spheroid continues small, fluid
friction will scarcely at all change these differences.
A like criticism may, I think, be passed on an opinion expressed by
Prof. Newcomb. He says:--"When the contraction [of the nebulous
spheroid] had gone so far that the centrifugal and attracting forces
nearly balanced each other at the outer equatorial limit of the mass,
the result would have been that contraction in the direction of the
equator would cease entirely, and be confined to the polar regions, each
particle dropping, not towards the sun, but towards the plane of the
solar equator. Thus, we should have a constant flattening of the
spheroidal atmosphere until it was reduced to a thin flat disk. This
disk might then separate itself into rings, which would form planets in
much the same way that Laplace supposed. But there would probably be no
marked difference in the age of the planets." (_Popular Astronomy_,
p. 512.) Now this conclusion assumes, like that of M. Babinet, that all
parts of the nebulous spheroid had equal angular velocities. If, as
above contended, it is inferable from the process by which a nebulous
spheroid was formed, that its outer portions revolved with greater
angular velocities than its inner; then the inference which Prof.
Newcomb draws is not necessitated.]
[Footnote 15: It is true that since this essay was written reasons have
been given for concluding that comets consist of swarms of meteors
enveloped in aeriform matter. Very possibly this is the constitution of
the periodic comets which, approximating their orbits to the plane of
the Solar System, form established parts of the System, and which, as
will be hereafter indicated, have probably a quite different origin.]
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