However, as matters chanced, the scientific world was not called upon to

decide between the merits of a discovery made by direct observation and

one effected by means of abstract reasoning. It was not until Saturn had

been examined with much higher telescopic power than Galileo could

employ, that the appendage which had so perplexed the Florentine

astronomer was seen to be a thin flat ring, nowhere touching the planet,

and considerably inclined to the plane in which Saturn travels. We

cannot wonder that the discovery was regarded as a most interesting one.

Astronomers had heretofore had to deal with solid masses, either known

to be spheroidal, like the earth, the sun, the moon, Jupiter, and Venus,

or presumed to be so, like the stars. The comets might be judged to be

vaporous masses of various forms; but even these were supposed to

surround or to attend upon globe-shaped nuclear masses. Here, however,

in the case of Saturn's ring, was a quoit-shaped body travelling around

the sun in continual attendance upon Saturn, whose motions, no matter

how they varied in velocity or direction, were so closely followed by

this strange attendant that the planet remained always centrally poised

within the span of its ring-girdle. To appreciate the interest with

which this strange phenomenon was regarded, we must remember that as yet

the law of gravity had not been recognised. Huyghens discovered the

ring (or rather perceived its nature) in 1659, but it was not till 1666

that Newton first entertained the idea that the moon is retained in its

orbit about the earth by the attractive energy which causes unsupported

bodies to fall earthwards; and he was unable to demonstrate the law of

gravity before 1684. Now, in a general sense, we can readily understand

in these days how a ring around a planet continues to travel along with

the planet despite all changes of velocity or direction of motion. For

the law of gravity teaches that the same causes which tend to change the

direction and velocity of the planet's motion tend in precisely the same

degree to change the direction and velocity of the ring's motion. But

when Huyghens made his discovery it must have appeared a most mysterious

circumstance that a ring and planet should be thus constantly

associated--that during thousands of years no collision should have

occurred whereby the relatively delicate structure of the ring had been

destroyed.

Only six years later a discovery was made by two English observers,

William and Thomas Ball, which enhanced the mystery. Observing the

northern face of the ring, which was at that time turned earthwards,

they perceived a black stripe of considerable breadth dividing the ring

into two concentric portions. The discovery did not attract so much

attention as it deserved, insomuch that when Cassini, ten years later,

announced the discovery of a corresponding dark division on the southern

surface, none recalled the observation made by the brothers Ball.

Cassini expressed the opinion that the ring is really divided into two,

not merely marked by a dark stripe on its southern face. This conclusion

would, of course, have been an assured one, had the previous observation

of a dark division on the northern face been remembered. With the

knowledge which we now possess, indeed, the darkness of the seeming

stripe would be sufficient evidence that there must be a real division

there between the rings; for we know that no mere darkness of the ring's

substance could account for the apparent darkness of the stripe. It has

been well remarked by Professor Tyndall, that if the moon's whole

surface could be covered with black velvet, she would yet appear white

when seen on the dark background of the sky. And it may be doubted

whether a circular strip of black velvet 2000 miles wide, placed where

we see the dark division between the rings, would appear nearly as dark

as that division. Since we could only admit the possibility of some

substance resembling our darker rocks occupying this position (for we

know of nothing to justify the supposition that a substance as dark as

lampblack or black velvet could be there), we are manifestly precluded

from supposing that the dark space is other than a division between two

distinct rings.

Yet Sir W. Herschel, in examining the rings of Saturn with his powerful

telescopes, for a long time favoured the theory that there is no real

division. He called it the 'broad black mark,' and argued that it can

neither indicate the existence of a zone of hills upon the ring, nor of

a vast cavernous groove, for in either case it would present changes of

appearance (according to the ring's changes of position) such as he was

unable to detect. It was not until the year 1790, eleven years after his

observations had commenced, that, perceiving a corresponding broad black

mark upon the ring's southern face, Herschel expressed a 'suspicion'

that the ring is divided into two concentric portions by a circular gap

nearly 2000 miles in width. He expressed at the same time, very

strongly, his belief that this division was the only one in Saturn's

ring-system.

A special interest attached at that time to the question whether the

ring is divided or not, for Laplace had then recently published the

results of his mathematical inquiry into the movements of such a ring as

Saturn's, and, having _proved_ that a single solid ring of such enormous

width could not continue to move around the planet, had expressed the

_opinion_ that Saturn's ring consists in reality of many concentric

rings, each turning, with its own proper rotation rate, around the

central planet. It is singular that Herschel, who, though not versed in

the methods of the higher mathematics, had considerable native power as

a mathematician, was unable to perceive the force of Laplace's

reasoning. Indeed, this is one of those cases where clearness of

perception rather than profundity of mathematical insight was required.

Laplace's equations of motion did not express all the relations

involved, nor was it possible to judge, from the results he deduced, how

far the stability of the Saturnian rings depended on the real structure

of these appendages. One who was well acquainted with mechanical

matters, and sufficiently versed in mathematics to understand how to

estimate generally the forces acting upon the ring-system, could have

perceived as readily the general conditions of the problem as the most

profound mathematician. One may compare the case to the problem of

determining whether the action of the moon in causing the tidal wave

modifies in any manner the earth's motion of rotation. We know that as a

mathematical question this is a very difficult one. The Astronomer

Royal, for example, not long ago dealt with it analytically, and deduced

the conclusion that there is no effect on the earth's rotation,

presently however, discovering by a lucky chance a term in the result

which indicates an effect of that kind. But if we look at the matter in

its mechanical aspect, we perceive at once, without any profound

mathematical research, that the retardation so hard to detect

mathematically must necessarily take place. As Sir E. Beckett says in

his masterly work, _Astronomy without Mathematics_, 'the conclusion is

as evident without mathematics as with them, when once it has been

suggested.' So when we consider the case of a wide flat ring surrounding

a mighty planet like Saturn, we perceive that nothing could possibly

save such a ring from destruction if it were really one solid structure.

To recognise this the more clearly, let us first notice the dimensions

of the planet and rings.

We have in Saturn a globe about 70,000 miles in mean diameter, an

equatorial diameter being about 73,000 miles, the polar diameter 66,000

miles. The attractive force of this mighty mass upon bodies placed on

its surface is equal to about one-fifth more than terrestrial gravity if

the body is near the pole of Saturn, and is almost exactly the same as

terrestrial gravity if the body is at the planet's equator. Its action

on the matter of the ring is, of course, very much less, because of the

increased distance, but still a force is exerted on every part of the

ring which is comparable with the familiar force of terrestrial gravity.

The outer edge of the outer ring lies about 83,500 miles from the

planet's centre, the inner edge of the inner ring (I speak throughout of

the ring-system as known to Sir W. Herschel and Laplace) about 54,500

miles from the centre, the breadth of the system of bright rings being

about 29,000 miles. Between the planet's equator and the inner edge of

the innermost bright ring there intervenes a space of about 20,000

miles. Roughly speaking, it may be said that the attraction of the

planet on the substance of the ring's inner edge is less than gravity at

Saturn's equator (or, which is almost exactly the same thing, is less

than terrestrial gravity) in about the proportion of 9 to 20; or, still

more roughly, the inner edge of Saturn's inner bright ring is drawn

inwards by about half the force of gravity at the earth's surface. The

outer edge is drawn towards Saturn by a force less than terrestrial

gravity in the proportion of about 3 to 16--say roughly that the force

thus exerted by Saturn on the matter of the outer edge of the

ring-system is equivalent to about one-fifth of the force of gravity at

the earth's surface.

It is clear, first, that if the ring-system did not rotate, the forces

thus acting on the material of the rings would immediately break them

into fragments, and, dragging these down to the planet's equator, would

leave them scattered in heaps upon that portion of Saturn's surface. The

ring would in fact be in that case like a mighty arch, each portion of

which would be drawn towards Saturn's centre by its own weight. This

weight would be enormous if Bessel's estimate of the mass of the

ring-system is correct. He made the mass of the ring rather greater than

the mass of the earth--an estimate which I believe to be greatly in

excess of the truth. Probably the rings do not amount in mass to more

than a fourth part of the earth's mass. But even that is enormous, and

subjected as is the material of the rings to forces varying from

one-half to a fifth of terrestrial gravity, the strains and pressures

upon the various parts of the system would exceed thousands of times

those which even the strongest material built up into their shape could

resist. The system would no more be able to resist such strains and

pressures than an arch of iron spanning the Atlantic would be able to

sustain its own weight against the earth's attraction.

It would be necessary then that the ring-system should rotate around the

planet. But it is clear that the proper rate of rotation for the outer

portion would be very different from the rate suited for the inner

portion. In order that the inner portion should travel around Saturn

entirely relieved of its weight, it should complete a revolution in

about seven hours twenty-three minutes. The outer portion, however,

should revolve in about thirteen hours fifty-eight minutes, or nearly

fourteen hours. Thus the inner part should rotate in little more than

half the time required by the outer part. The result would necessarily

be that the ring-system would be affected by tremendous strains, which

it would be quite unable to resist. The existence of the great division

would manifestly go far to diminish the strains. It is easily shown that

the rate of turning where the division is, would be once in about eleven

hours and twenty-five minutes, not differing greatly from the mean

between the rotation-periods for the outside and for the inside edges of

the system. Even then, however, the strains would be hundreds of times

greater than the material of the ring could resist. A mass comparable in

weight to our earth, compelled to rotate in (say) nine hours when it

ought to rotate in eleven or in seven, would be subjected to strains

exceeding many times the resistances which the cohesive power of its

substance could afford. That would be the condition of the inner ring.

And in like manner the outer ring, if it rotated in about twelve hours

and three-quarters, would have its outer portions rotating too fast and

its inner portions too slowly, because their proper periods would be

fourteen hours and eleven hours and a half respectively. Nothing but the

division of the ring into a number of narrow hoops could possibly save

it from destruction through the internal strains and pressures to which

its material would be subjected.

Even this complicated arrangement, however, would not save the

ring-system. If we suppose a fine hoop to turn around a central

attracting body as the rings of Saturn rotate around the planet, it may

be shown that unless the hoop is so weighted that its centre of gravity

is far from the planet, there will be no stability in the resulting

motions; the hoop will before long be made to rotate eccentrically, and

eventually be brought into destructive collision with the central

planet.

It was here that Laplace left the problem. Nothing could have been more

unsatisfactory than his result, though it was accepted for nearly half a

century unquestioned. He had shown that a weighted fine hoop may

possibly turn around a central attracting mass without destructive

changes of position, but he had not proved more than the bare

possibility of this, while nothing in the appearance of Saturn's rings

suggests that any such arrangement exists. Again, manifestly a multitude

of narrow hoops, so combined as to form a broad flat system of rings,

would be constantly in collision _inter se_. Besides, each one of them

would be subjected to destructive strains. For though a fine uniform

hoop set rotating at a proper rate around an attracting mass at its

centre would be freed from all strains, the case is very different with

a hoop so weighted as to have its centre of gravity greatly displaced.

Laplace had saved the theoretical stability of the motions of a fine

ring at the expense of the ring's power of resisting the strains to

which it would be exposed. It seems incredible that such a result

(expressed, too, very doubtingly by the distinguished mathematician who

had obtained it) should have been accepted so long almost without

question. There is nothing in nature in the remotest degree resembling

the arrangement imagined by Laplace, which indeed appears on _a priori_

grounds impossible. It was not claimed for it that it removed the

original difficulties of the problem; and it introduced others fully as

serious. So strong, however, is authority in the scientific world that

none ventured to express any doubts except Sir W. Herschel, who simply

denied that the two rings were divided into many, as Laplace's theory

required. As time went on and the signs of many divisions were at times

recognised, it was supposed that Laplace's reasoning had been justified;

and despite the utter impossibility of the arrangement he had suggested,

that arrangement was ordinarily described as probably existing.

At length, however, a discovery was made which caused the whole question

to be reopened.

On November 10, 1850, W. Bond, observing the planet with the telescope

of the Harvard Observatory, perceived within the inner bright ring a

feeble illumination which he was at a loss to understand. On the next

night the faint light was better seen. On the 15th, Tuttle, who was

observing with Bond, suggested the idea that the light within the inner

bright ring was due to a dusky ring inside the system of bright rings.

On November 25, Mr. Dawes in England perceived this dusky ring, and

announced the discovery before the news had reached England that Bond

had already seen the dark ring. The credit of the discovery is usually

shared between Bond and Dawes, though the usual rule in such matters

would assign the discovery to Bond alone. It was found that the dark

ring had already been seen at Rome so far back as 1828, and again by

Galle at Berlin in May 1838. The Roman observations were not

satisfactory. Those by Galle, however, were sufficient to have

established the fact of the ring's existence; indeed, in 1839 Galle

measured the dark ring. But very little attention was attracted to this

interesting discovery, insomuch that when Bond and Dawes announced their

observation of the dark ring in 1850, the news was received by

astronomers with all the interest attaching to the detection of before

unnoted phenomena.

It may be well to notice under what conditions the dark ring was

detected in 1850. In September 1848 the ring had been turned edgewise

towards the sun, and as rather more than seven years are occupied in

the apparent gradual opening out of the ring from that edge view to its

most open appearance (when the outline of the ring-system is an eclipse

whose lesser axis is nearly equal to half the greater), it will be seen

that in November 1850 the rings were but slightly opened. Thus the

recognition of the dark ring within the bright system was made under

unfavourable conditions. For four preceding years--that is, from the

year 1846--the rings had been as little or less opened; and again for

several years preceding 1846, though the rings had been more open, the

planet had been unfavourably placed for observation in northern

latitudes, crossing the meridian at low altitudes. Still, in 1838 and

1839, when the rings were most open, although the planet was never seen

under favourable conditions, the opening of the rings, then nearly at

its greatest, made the recognition of the dark ring possible; and we

have seen that Galle then made the discovery. When Bond rediscovered the

dark ring, everything promised that before long the appendage would be

visible with telescopes far inferior in power to the great Harvard

refractor. Year after year the planet was becoming more favourably

placed for observation, while all the time the rings were opening out.

Accordingly it need not surprise us to learn that in 1853 the dark ring

was seen with a telescope less than three inches and a half in aperture.

Even so early as 1851, Mr. Hartnup, observing the planet with a

telescope eight inches and a half in aperture, found that 'the dark ring

could not be overlooked for an instant.'

But while this increase in the distinctness of the dark ring was to be

expected, from the mere fact that the ring was discovered under

relatively unfavourable conditions, yet the fact that Saturn was thus

found to have an appendage of a remarkable character, perfectly obvious

even with moderate telescopic power, was manifestly most surprising.

The planet had been studied for nearly two centuries with telescopes

exceeding in power those with which the dark ring was now perceived.

Some among these telescopes were not only of great power, but employed

by observers of the utmost skill. The elder Herschel had for a quarter

of a century studied Saturn with his great reflectors eighteen inches in

aperture, and had at times turned on the planet his monstrous (though

not mighty) four-feet mirror. Schroeter had examined the dark space

within the inner bright ring for the special purpose of determining

whether the ring-system is really disconnected from the globe. He had

used a mirror nineteen inches in aperture, and he had observed that the

dark space seen on either side of Saturn inside the ring-system not only

appeared dark, but actually darker than the surrounding sky. This was

presumably (though not quite certainly) an effect of contrast only, the

dark space being bounded all round by bright surfaces. If real, the

phenomenon signified that whereas the space outside the ring, where the

satellites of the planet travel, was occupied by some sort of cosmical

dust, the space within the ring-system was, as it were, swept and

garnished, as though all the scattered matter which might otherwise have

occupied that region had been either attracted to the body of the planet

or to the rings.[36] But manifestly the observation was entirely

inconsistent with the supposition that there existed in Schroeter's time

a dark or dusky ring within the bright system. Again, the elder Struve

made the most careful measurement of the whole of the ring-system in

1826, when the system was as well placed for observation as in 1856

(or, in other words, as well placed as it can possibly be); but though

he used a telescope nine inches and a half in aperture, and though his

attention was specially attracted to the inner edge of the inner bright

ring (_which seemed to him indistinct_), he did not detect the dark

ring. Yet we have seen that in 1851, under much less favourable

conditions, a less practised observer, using a telescope of less

aperture, found that the dark ring could not be overlooked for an

instant. It is manifest that all these considerations point to the

conclusion that the dark ring is a new formation, or, at the least, that

it has changed notably in condition during the present century.

I have hitherto only considered the appearance of the dusky ring as seen

on either side of the planet's globe within the bright rings. The most

remarkable feature of the appendage remains still to be mentioned--the

fact, namely, that the bright body of the planet can be seen through

this dusky ring. Where the dark ring crosses the planet, it appears as a

rather dark belt, which might readily be mistaken for a belt upon the

planet's surface; for the outline of the planet can be seen through the

ring as through a film of smoke or a crape veil.

Now it is worthy of notice that whereas the dark ring was not detected

outside the planet's body until 1838, nor generally recognised by

astronomers until 1850, the dark belt across the planet, really caused

by the dusky ring, was observed more than a century earlier. In 1715 the

younger Cassini saw it, and perceived that it was not curved enough for

a belt really belonging to the planet. Hadley again observed that the

belt attended the ring as this opened out and closed, or, in other

words, that the dark belt belonged to the ring, not to the body of the

planet. And in many pictures of Saturn's system a dark band is shown

along the inner edge of the inner bright ring where it crosses the body

of the planet. It seems to me that we have here a most important piece

of evidence respecting the rings. It is clear that the inner part of the

inner bright ring has for more than a century and a half (how much more

we do not know) been partially transparent, and it is probable that

within its inner edge there has been all the time a ring of matter; but

this ring has only within the last half-century gathered consistency

enough to be discernible. It is manifest that the existence of the dark

belt shown in the older pictures would have led directly to the

detection of the dark ring, had not this appendage been exceedingly

faint. Thus, while the observation of the dark belt across the planet's

face proves the dusky ring to have existed in some form long before it

was perceived, the same fact only helps to render us certain that the

dark ring has changed notably in condition during the present century.

The discovery of this singular appendage, an object unique in the solar

system, naturally attracted fresh attention to the question of the

stability of the rings. The idea was thrown out by the elder Bond that

the new ring may be fluid, or even that the whole ring-system may be

fluid, and the dark ring simply thinner than the rest. It was thought

possible that the ring-system is of the nature of a vast ocean, whose

waves are steadily advancing upon the planet's globe. The mathematical

investigation of the subject was also resumed by Professor Benjamin

Pierce, of Harvard, and it was satisfactorily demonstrated that the

stability of a system of actual rings of solid matter required so nice

an adjustment of so many narrow rings as to render the system far more

complex than even Laplace had supposed. 'A stable formation can,' he

said, 'be nothing other than a very great number of separate narrow

rigid rings, each revolving with its proper relative velocity.' As was

well remarked by the late Professor Nichol, 'If this arrangement or

anything like it were real, how many new conditions of instability do we

introduce. Observation tells us that the division between such rings

must be extremely narrow, so that the slightest disturbance by external

or internal causes would cause one ring to impinge upon another; and we

should thus have the seed of perpetual catastrophes.' Nor would such a

constitution protect the system against dissolution. 'There is no escape

from the difficulties, therefore, but through the final rejection of the

idea that Saturn's rings are rigid or in any sense a solid formation.'

Myths and Marvels of Astronomy · 第 14 / 28 段