Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent AstronomersOlmsted, Denison
Science
Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent Astronomers
Olmsted, Denison
Astronomy
Soon afterwards, he began to publish his
writings, in rapid succession, and became at once among the most
conspicuous of his age,--a rank which he afterwards well sustained and
greatly exalted, by the invention of the telescope, and by his numerous
astronomical discoveries. I will reserve an account of these great
achievements until we come to that part of astronomy to which they were
more immediately related, and proceed, now, to explain to you the
leading principles of _terrestrial gravity_, as exemplified in falling
bodies.
First, _all bodies near the earth's surface fall in straight lines
towards the centre of the earth_. We are not to infer from this fact,
that there resides at the centre any peculiar force, as a great
loadstone, for example, which attracts bodies towards itself; but bodies
fall towards the centre of the sphere, because the combined attractions
of all the particles of matter in the earth, each exerting its proper
force upon the body, would carry it towards the centre. This may be
easily illustrated by a diagram. Let B, Fig. 29, page 140, be the
centre of the earth, and A a body without it. Every portion of matter in
the earth exerts some force on A, to draw it down to the earth. But
since there is just as much matter on one side of the line A B, as on
the other side, each half exerts an equal force to draw the body towards
itself; therefore it falls in the direction of the diagonal between the
two forces. Thus, if we compare the effects of any two particles of
matter at equal distances from the line A B, but on opposite sides of
it, as _a_, _b_, while the force of the particle at _a_ would tend to
draw A in the direction of A _a_, that of _b_ would draw it in the
direction of A _b_, and it would fall in the line A B, half way between
the two. The same would hold true of any other two corresponding
particles of matter on different sides of the earth, in respect to a
body situated in any place without it.
[Illustration Fig. 29.]
Secondly, _all bodies fall towards the earth, from the same height, with
equal velocities_. A musket-ball, and the finest particle of down, if
let fall from a certain height towards the earth, tend to descend
towards it at the same rate, and would proceed with equal speed, were it
not for the resistance of the air, which retards the down more than it
does the ball, and finally stops it. If, however, the air be removed out
of the way, as it may be by means of the air-pump, the two bodies keep
side by side in falling from the greatest height at which we can try the
experiment.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account