Stellar Evolution and Its Relations to Geological Time — John Shaqi
Stellar Evolution and Its Relations to Geological TimeCroll, James
Science
Stellar Evolution and Its Relations to Geological Time
Croll, James
Cosmogony; Geological time; Stars -- Evolution
9. _Condensation the third and last condition of a nebula._—According to
the gravitation theory, condensation is the first stage of a nebula as
well as the last; for, according to it, gravity is the force which both
collects together the scattered materials and gives them their heat.[18]
Before condensation begins there can, according to the gravitation
theory, be no such thing as a nebula properly so called. The materials
exist, of course, but they do not exist in the form of a nebula.
According to the impact theory which I here advocate, condensation
cannot begin till after the nebula has begun to lose the heat with which
it was originally endowed.
[Footnote 18: Laplace held a more accurate view of the primitive
condition of the solar nebula. He considered that, owing to intense
heat, the solar mass became expanded to the limits of the remotest
planetary orbit of our system; that, in cooling, it began slowly to
condense; and that, as condensation went on, planet after planet became
detached from the mass. Laplace, however, offered no explanation of the
manner in which the primitive nebula obtained its heat.]
10. _How nebulæ emit such feeble light._—The light of nebulæ is mainly
derived from glowing hydrogen and nitrogen in a condition of extreme
gaseous tenuity; and it is well known that these gases are exceedingly
bad radiators. The oxyhydrogen flame, although its temperature is
surpassed only by that of the voltaic arc, gives a light so feeble as to
be scarcely visible in daylight. The small luminosity of nebulæ is,
however, mainly due to a different cause. The enormous space occupied by
those bodies is not so much due to the heat which they possess as to the
fact that their materials were dispersed into space before they had time
to pass into the gaseous condition; so that, by the time that this
latter state was assumed, the space occupied was far greater than was
demanded either by the temperature or by the amount of heat which they
originally received. If we adopt the nebular hypothesis of the origin of
our solar system, we must assume that our sun’s mass, when in the
condition of a nebula, extended beyond the orbit of the planet Neptune,
and consequently filled the entire space included within that orbit.
Even supposing Neptune’s orbit to have been its outer limit, which,
obviously, was not the case, it would nevertheless have occupied
274,000,000,000 times the space it does at present. We shall assume, as
before, that 50,000,000 years’ heat was generated by the concussion. Of
course, there might have been twice or even ten times that quantity; but
it is of no importance what amount is in the meantime adopted. Enormous
as 50,000,000 years’ heat is, it yet gives, as we shall presently see,
only 32 foot-pounds of energy for each cubic foot. The amount of heat
due to concussion being equal, as before stated, to 100,000,000,000
foot-pounds for each pound of the mass, and a cubic foot of the sun at
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