CHAPTER IV

CELESTIAL MECHANISM

As soon as we begin to inquire closely into the actual condition of the

various members of the solar system we are struck with a certain

distinction. We find that there are two quite different points of view

from which these bodies can be regarded. For instance, we may make our

estimates of them either as regards _volume_--that is to say, the mere

room which they take up; or as regards _mass_--that is to say, the

amount of matter which they contain.

Let us imagine two globes of equal volume; in other words, which take up

an equal amount of space. One of these globes, however, may be composed

of material much more tightly put together than in the other; or of

greater _density_, as the term goes. That globe is said to be the

greater of the two in mass. Were such a pair of globes to be weighed in

scales, one globe in each pan, we should see at once, by its weighing

down the other, which of the two was composed of the more tightly packed

materials; and we should, in astronomical parlance, say of this one that

it had the greater mass.

Volume being merely another word for size, the order of the members of

the solar system, with regard to their volumes, will be as follows,

beginning with the greatest:--the Sun, Jupiter, Saturn, Uranus,

Neptune, the Earth, Venus, Mars, and Mercury.

With regard to mass the same order strangely enough holds good. The

actual densities of the bodies in question are, however, very different.

The densest or closest packed body of all is the Earth, which is about

five and a half times as dense as if it were composed entirely of water.

Venus follows next, then Mars, and then Mercury. The remaining bodies,

on the other hand, are relatively loose in structure. Saturn is the

least dense of all, less so than water. The density of the Sun is a

little greater than that of water.

This method of estimating is, however, subject to a qualification. It

must be remembered that in speaking of the Sun, for instance, as being

only a little denser than water, we are merely treating the question

from the point of view of an average. Certain parts of it in fact will

be ever so much denser than water: those are the parts in the centre.

Other portions, for instance, the outside portions, will be very much

less dense. It will easily be understood that in all such bodies the

densest or most compressed portions are to be found towards the centre;

while the portions towards the exterior being less pressed upon, will be

less dense.

We now reach a very important point, the question of Gravitation.

_Gravitation_, or _gravity_, as it is often called, is the attractive

force which, for instance, causes objects to fall to the earth. Now it

seems rather strange that one should say that it is owing to a certain

force that things fall towards the earth. All things seem to us to fall

so of their own accord, as if it were quite natural, or rather most

unnatural if they did not. Why then require a "force" to make them fall?

The story goes that the great Sir Isaac Newton was set a-thinking on

this subject by seeing an apple fall from a tree to the earth. He then

carried the train of thought further; and, by studying the movements of

the moon, he reached the conclusion that a body even so far off as our

satellite would be drawn towards the earth in the same manner. This

being the case, one will naturally ask why the moon herself does not

fall in upon the earth. The answer is indeed found to be that the moon

is travelling round and round the earth at a certain rapid pace, and it

is this very same rapid pace which keeps her from falling in upon us.

Any one can test this simple fact for himself. If we tie a stone to the

end of a string, and keep whirling it round and round fast enough, there

will be a strong pull from the stone in an outward direction, and the

string will remain tight all the time that the stone is being whirled.

If, however, we gradually slacken the speed at which we are making the

stone whirl, a moment will come at length when the string will become

limp, and the stone will fall back towards our hand.

It seems, therefore, that there are two causes which maintain the stone

at a regular distance all the time it is being steadily whirled. One of

these is the continual pull inward towards our hand by means of the

string. The other is the continual pull away from us caused by the rate

at which the stone is travelling. When the rate of whirling is so

regulated that these pulls exactly balance each other, the stone travels

comfortably round and round, and shows no tendency either to fall back

upon our hand or to break the string and fly away into the air. It is

indeed precisely similar with regard to the moon. The continual pull of

the earth's gravitation takes the place of the string. If the moon were

to go round and round slower than it does, it would tend to fall in

towards the earth; if, on the other hand, it were to go faster, it would

tend to rush away into space.

The same kind of pull which the earth exerts upon the objects at its

surface, or upon its satellite, the moon, exists through space so far as

we know. Every particle of matter in the universe is found in fact to

attract every other particle. The moon, for instance, attracts the earth

also, but the controlling force is on the side of the much greater mass

of the earth. This force of gravity or attraction of gravitation, as it

is also called, is perfectly regular in its action. Its power depends

first of all exactly upon the mass of the body which exerts it. The

gravitational pull of the sun, for instance, reaches out to an enormous

distance, controlling perhaps, in their courses, unseen planets circling

far beyond the orbit of Neptune. Again, the strength with which the

force of gravity acts depends upon distance in a regularly diminishing

proportion. Thus, the nearer an object is to the earth, for instance,

the stronger is the gravitational pull which it gets from it; the

farther off it is, the weaker is this pull. If then the moon were to be

brought nearer to the earth, the gravitational pull of the latter would

become so much stronger that the moon's rate of motion would have also

to increase in due proportion to prevent her from being drawn into the

earth. Last of all, the point in a body from which the attraction of

gravitation acts, is not necessarily the centre of the body, but rather

what is known as its _centre of gravity_, that is to say, the balancing

point of all the matter which the body contains.

It should here be noted that the moon does not actually revolve around

the centre of gravity of the earth. What really happens is that both

orbs revolve around their _common_ centre of gravity, which is a point

within the body of the earth, and situated about three thousand miles

from its centre. In the same manner the planets and the sun revolve

around the centre of gravity of the solar system, which is a point

within the body of the sun.

The neatly poised movements of the planets around the sun, and of the

satellites around their respective planets, will therefore be readily

understood to result from a nice balance between gravitation and speed

of motion.

The mass of the earth is ascertained to be about eighty times that of

the moon. Our knowledge of the mass of a planet is learned from

comparing the revolutions of its satellite or satellites around it, with

those of the moon around the earth. We are thus enabled to deduce what

the mass of such a planet would be compared to the earth's mass; that is

to say, a study, for instance, of Jupiter's satellite system shows that

Jupiter must have a mass nearly three hundred and eighteen times that of

our earth. In the same manner we can argue out the mass of the sun from

the movements of the planets and other bodies of the system around it.

With regard, however, to Venus and Mercury, the problem is by no means

such an easy one, as these bodies have no satellites. For information in

this latter case we have to rely upon such uncertain evidence as, for

instance, the slight disturbances caused in the motion of the earth by

the attraction of these planets when they pass closest to us, or their

observed effect upon the motions of such comets as may happen to pass

near to them.

Mass and weight, though often spoken of as one and the same thing, are

by no means so. Mass, as we have seen, merely means the amount of matter

which a body contains. The weight of a body, on the other hand, depends

entirely upon the gravitational pull which it receives. The force of

gravity at the surface of the earth is, for instance, about six times as

great as that at the surface of the moon. All bodies, therefore, weigh

about six times as much on the earth as they would upon the moon; or,

rather, a body transferred to the moon's surface would weigh only about

one-sixth of what it did on the terrestrial surface. It will therefore

be seen that if a body of given _mass_ were to be placed upon planet

after planet in turn, its _weight_ would regularly alter according to

the force of gravity at each planet's surface.

Gravitation is indeed one of the greatest mysteries of nature. What it

is, the means by which it acts, or why such a force should exist at all,

are questions to which so far we have not had even the merest hint of an

answer. Its action across space appears to be instantaneous.

The intensity of gravitation is said in mathematical parlance "to vary

inversely with the square of the distance." This means that at _twice_

the distance the pull will become only _one-quarter_ as strong, and not

one-half as otherwise might be expected. At _four_ times the distance,

therefore, it will be _one-sixteenth_ as strong. At the earth's surface

a body is pulled by the earth's gravitation, or "falls," as we

ordinarily term it, through 16 feet in one _second_ of time; whereas at

the distance of the moon the attraction of the earth is so very much

weakened that a body would take as long as one _minute_ to fall through

the same space.

Newton's investigations showed that if a body were to be placed _at

rest_ in space entirely away from the attraction of any other body it

would remain always in a motionless condition, because there would

plainly be no reason why it should move in any one direction rather than

in another. And, similarly, if a body were to be projected in a certain

direction and at a certain speed, it would move always in the same

direction and at the same speed so long as it did not come within the

gravitational attraction of any other body.

The possibility of an interaction between the celestial orbs had

occurred to astronomers before the time of Newton; for instance, in the

ninth century to the Arabian Musa-ben-Shakir, to Camillus Agrippa in

1553, and to Kepler, who suspected its existence from observation of the

tides. Horrox also, writing in 1635, spoke of the moon as moved by an

_emanation_ from the earth. But no one prior to Newton attempted to

examine the question from a mathematical standpoint.

Notwithstanding the acknowledged truth and far-reaching scope of the law

of gravitation--for we find its effects exemplified in every portion of

the universe--there are yet some minor movements which it does not

account for. For instance, there are small irregularities in the

movement of Mercury which cannot be explained by the influence of

possible intra-Mercurial planets, and similarly there are slight

unaccountable deviations in the motions of our neighbour the Moon.

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