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
The theory seems to dispense with the necessity for assuming a
luminiferous ether, for the functions attributed to the ether may, it is
thought, be performed by the particles themselves; a view which has been
advocated by Euler, Grove, and others. The origin of nebulæ, according
to the theory, is accounted for as follows:
“The nebular hypothesis,” says Mr. Morris, “holds that the matter now
concentrated into suns and planets was once more widely disseminated, so
that the substance of each sphere occupied a very considerable extent of
space. It even declares that the matter of the solar system was a
nebulous cloud, extending far beyond the present limits of that system.
From this original condition the existing condition of the spheres has
arisen through a continued concentration of matter. But this
concentration was constantly opposed by the heat energy of the
particles, or, in other words, by their centrifugal momentum. This
momentum could only be got rid of by a redistribution of motor energy.
If, for illustration, the average momentum of the particles of the
nebulæ was just equivalent to their gravitative energy, then a portion
of this energy must radiate or be conducted outwards ere the internal
particles could be held prisoners by gravitation. The loss of momentum
inwardly must be correlated with an increase of momentum outwardly.
“This is a necessary consequence of the heat relations of matter. As
substance condenses, its capacity for heat decreases and its temperature
rises, hence a difference of temperature must constantly have arisen
between the denser and the rarer portions of the nebulous mass, and
equality of temperature could be restored only by heat radiation. This
radiation still continues, and must continue until condensation ceases
and the temperatures of the spheres and space become equalised; but this
is equivalent to declaring that as the particles of the spheres decrease
in heat momentum those of interspheral space increase, and if originally
the centrifugal and centripetal energies of matter approached equality
they must become unequal, centripetal energy becoming in excess in
spheral matter, centrifugal energy in the matter of space. Thus, as a
portion of the widely distributed nebulous matter lost its heat, and
became permanently fixed in place by gravitative attraction, another
portion gained heat, became still more independent of gravity, and
assumed a state of greater nebulous diffusion than originally. The
condensing spheres only denuded space of a portion of the matter which
it formerly held, and left the remainder more thinly distributed than
before. The spheres, in their concentration, have emitted, and are
emitting, a vast energy of motion. This motor energy yet exists in space
as a motion of the particles of matter, which, therefore, press upon
each other, or seek to extend their limits, with increasing vigour, so
that the elasticity of interspheral matter is constantly increasing.”
Public-domain text, read in full here on John Shaqi.
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