A Preliminary Dissertation on the Mechanisms of the HeavensSomerville, Mary
Science
A Preliminary Dissertation on the Mechanisms of the Heavens
Somerville, Mary
Celestial mechanics
The masses of such planets as have no satellites are known by comparing
the inequalities they produce in the motions of the earth and of each
other, determined theoretically, with the same inequalities given by
observation, for the disturbing cause must necessarily be proportional
to the effect it produces. But as the quantities of matter in any two
primary planets are directly as the cubes of the mean distances at which
their satellites revolve, and inversely as the squares of their periodic
times, the mass of the sun and of any planets which have satellites, may
be compared with the mass of the earth. In this manner it is computed
that the mass of the sun is 354936 times greater than that of the earth;
whence the great perturbations of the moon and the rapid motion of the
perigee and nodes of her orbit. Even Jupiter, the largest of the
planets, is 1070.5 times less than the sun. The mass of the moon is
determined from four different sources,--from her action on the
terrestrial equator, which occasions the rotation in the axis of
rotation; from her horizontal parallax, from an inequality she produces
in the sun's longitude, and from her action on the titles. The three
first quantities, computed from theory, and compared with their observed
values, give her mass respectively equal to the 1/71, 1/74·2, and 1/69·2
part of that of the earth, which do not differ very much from each
other; but, from her action in raising the tides, which furnishes
the fourth method, her mass appears to be about the seventy-fifth part
of that of the earth, a value that cannot differ much from the truth.
The apparent diameters of the sun, moon, and planets are determined by
measurement; therefore their real diameters may be compared with that of
the earth; for the real diameter of a planet is to the real diameter of
the earth, or 8000 miles, as the apparent diameter of the planet to the
apparent diameter of the earth as seen from the planet, that is, to
twice the parallax of the planet The mean apparent diameter of the sun
is 1920", and with the solar parallax 8"·65, it will be found that
the diameter of the sun is about 888000 miles; therefore, the centre of
the sun were to coincide with the centre of the earth, his volume would
not only include the orbit of the moon, but would extend nearly as far
again, for the moon's mean distance from the earth is about sixty times
the earth's mean radius or 240000 miles; so that twice the distance of
the moon is 480000 miles, which differs but little from the solar
radius; his equatorial radius is probably not much less than the major
axis of the lunar orbit.
The diameter of the moon is only 2160 miles; and Jupiter's diameter of
88000 miles is incomparably less than that of the sun The diameter of
Pallas does not much exceed 71 miles, so that an inhabitant of that
planet, in one of our steam-carriages, might go round his world in five
or six hours.
Public-domain text, read in full here on John Shaqi.
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