In drawing towards the close of these lectures I must say a few words

about some dim and mysterious objects to which we have not yet

alluded. They are what are called nebulæ, or little clouds; and in

one sense they are justly called little, for each of them occupies but

a very small spot in the sky as compared with that which would be

filled by an ordinary cloud in our air. The nebulæ are, however,

objects of the most stupendous proportions. Were our earth and

thousands of millions of bodies quite as big all put together, they

would not be nearly so great as one of these nebulæ. Astronomers

reckon up the various nebulæ by thousands, but I must add that most of

them are apparently faint and uninteresting. A nebula is sometimes

liable to be mistaken for a comet. The comet is, as I have already

explained, at once distinguished by the fact that it is moving and

changing its appearance from hour to hour, while scores of years

elapse without changes in the aspect or position of a nebula. The most

powerful telescopes are employed in observing these faint objects. I

take this opportunity of showing a picture of an instrument suitable

for such observations. It is the great reflector of the Paris

Observatory (Fig. 5).

[Illustration: FIG. 5. A GREAT REFLECTING TELESCOPE.]

[Illustration: FIG. 6. THE RING NEBULA IN LYRA, UNDER DIFFERENT

TELESCOPIC POWERS.]

There are such multitudes of nebulæ that I can only show a few of the

more remarkable kinds. In Fig. 6 will be seen pictures of a curious

object in the constellation of Lyra seen under different telescopic

powers. This is a gigantic ring of luminous gas. To judge of the size

of this ring let us suppose that a railway were laid across it, and

the train you entered at one side was not to stop until it reached the

other side, how long do you think this journey would require? I

recollect some time ago a picture in _Punch_ which showed a train

about to start from London to Brighton, and the guard walking up and

down announcing to the passengers the alarming fact that "this train

stops nowhere." An old gentleman was seen vainly gesticulating out of

the window and imploring to be let out ere the frightful journey was

commenced. In the nebular railway the passengers would almost require

such a warning.

Let the train start at a speed of a mile a minute, you would think,

surely, that it must soon cross the ring. But the minutes pass, an

hour has elapsed; so the distance must be sixty miles at all events.

The hours creep on into days, the days advance into years, and still

the train goes on. The years would lengthen out into centuries, and

even when the train had been rushing on for a thousand years with an

unabated speed of a mile a minute, the journey would certainly not

have been completed. Nor do I venture to say what ages must elapse ere

the terminus at the other side of the ring nebula would be reached.

A cluster of stars viewed in a small telescope will often seem like a

nebula, for the rays of the stars become blended. A powerful telescope

will, however, dispel the illusion and reveal the separate stars. It

was, therefore, thought that all the nebulæ might be merely clusters

so exceedingly remote that our mightiest instruments failed to resolve

them into stars. But this is now known not to be the case. Many of

these objects are really masses of glowing gas; such are, for

instance, the ring nebulæ, of which I have just spoken, and the form

of which I can simulate by a pretty experiment.

We take a large box with a round hole cut in one face, and a canvas

back at the opposite side. I first fill this box with smoke, and there

are different ways of doing so. Burning brown paper does not answer

well, because the supply of smoke is too irregular and the paper

itself is apt to blaze. A little bit of phosphorus set on fire yields

copious smoke, but it would be apt to make people cough, and, besides,

phosphorus is a dangerous thing to handle incautiously, and I do not

want to suggest anything which might be productive of disaster if the

experiment was repeated at home. A little wisp of hay, slightly damped

and lighted, will safely yield a sufficient supply, and you need not

have an elaborate box like this; any kind of old packing-case, or even

a bandbox with a duster stretched across its open top and a round hole

cut in the bottom, will answer capitally. While I have been speaking,

my assistant has kindly filled this box with smoke, and in order to

have a sufficient supply, and one which shall be as little

disagreeable as possible, he has mixed together the fumes of

hydrochloric acid and ammonia from two retorts shown in Fig. 7. A

still simpler way of doing the same thing is to put a little common

salt in a saucer and pour over it a little oil of vitriol; this is put

into the box, and over the floor of the box common smelling-salts is

to be scattered. You see there are dense volumes of white smoke

escaping from every corner of the box. I uncover the opening and give

a push to the canvas, and you see a beautiful ring flying across the

room; another ring and another follows. If you were near enough to

feel the ring, you would experience a little puff of wind; I can show

this by blowing out a candle which is at the other end of the table.

These rings are made by the air which goes into a sort of eddy as it

passes through the hole. All the smoke does is to render the air

visible. The smoke-ring is indeed quite elastic. If we send a second

ring hurriedly after the first, we can produce a collision, and you

see each of the two rings remains unbroken, though both are quivering

from the effects of the blow. They are beautifully shown along the

beam of the electric lamp, or, better still, along a sunbeam.

[Illustration: FIG. 7. HOW TO MAKE THE SMOKE RINGS.]

We can make many experiments with smoke-rings. Here, for instance, I

take an empty box, so far as smoke is concerned, but air-rings can be

driven forth from it, though you cannot see them, but you can feel

them even at the other side of the room, and they will, as you see,

blow out a candle. I can also shoot invisible air-rings at a column of

smoke, and when the missile strikes the smoke it produces a little

commotion and emerges on the other side, carrying with it enough of

the smoke to render itself visible, while the solid black looking ring

of air is seen in the interior. Still more striking is another way of

producing these rings, for I charge this box with ammonia, and the

rings from it you cannot see. There is a column of the vapor of

hydrochloric acid, that also you cannot see; but when the visible ring

enters the invisible column, then a sudden union takes place between

the vapor of the ammonia and the vapor of the hydrochloric acid; the

result is a solid white substance in extremely fine dust which renders

the ring instantly visible.

What the Nebulæ are made of.

There is a fundamental difference between the illumination of these

little rings that I have shown you and the great rings in the heavens.

I had to illuminate our smoke with the help of the electric light,

for, unless I had done so, you would not have been able to see them.

This white substance formed by the union of ammonia and hydrochloric

acid has, of course, no more light of its own than a piece of chalk;

it requires other light falling upon it to make it visible. Were the

ring nebula in Lyra composed of this material, we could not see it.

The sunlight which illuminates the planets might, of course, light up

such an object as the ring, if it wrere comparatively near us; but

Lyra is at such a stupendous distance that any light which the sun

could send out there would be just as feeble as the light we receive

from a fixed star. Should we be able to show our smoke-rings, for

instance, if, instead of having the electric light, I merely cut a

hole in the ceiling and allowed the feeble twinkle of a star in the

Great Bear to shine through? In a similar way the sunbeams would be

utterly powerless to effect any illumination of objects in these

stellar distances. If the sun were to be extinguished altogether, the

calamity would no doubt be a very dire one so far as we are concerned,

but the effect on the other celestial bodies (moon and planets

excepted) would be of the slightest possible description. All the

stars of heaven would continue to shine as before. Not a point in one

of the constellations wrould be altered, not a variation in the

brightness, not a change in the hue of any star could be noticed. The

thousands of nebulæ and clusters would be absolutely unaltered; in

fact, the total extinction of the sun would be hardly remarked in the

newspapers published in the Pleiades or in Orion. There might possibly

be a little line somewhere in an odd corner to the effect "Mr.

So-and-So, our well-known astronomer, has noticed that a tiny star,

inconspicuous to the eye, and absolutely of no importance whatever,

has now become invisible."

If, therefore, it be not the sun which lights up this nebula, where

else can be the source of its illumination? There can be no other star

in the neighborhood adequate to the purpose, for, of course, such an

object would be brilliant to us if it were large enough and bright

enough to impart sufficient illumination to the nebula. It would be

absurd to say that you could see a man's face by the light of a candle

while the candle itself was too faint or too distant to be visible.

The actual facts are, of course, the other way; the candle might be

visible, when it was impossible to discern the face which it lighted.

Hence we learn that the ring nebula must shine by some light of its

own, and now we have to consider how it can be possible for such

material to be self-luminous. The light of a nebula does not seem to

be like flame; it can, perhaps, be better represented by the pretty

electrical experiment with Geissler's tubes. These are glass vessels

of various shapes, and they are all very nearly empty, as you will

understand when I tell you the way in which they have been prepared. A

little gas was allowed into each tube, and then almost all the gas was

taken out again, so that only a mere trace was left. I pass a current

of electricity through these tubes, and now you see they are glowing

with beautiful colors. The different gases give out lights of

different hues, and the optician has exerted his skill so as to make

the effect as beautiful as possible. The electricity, in passing

through these tubes, heats the gas which they contain, and makes it

glow; and just as this gas can, when heated sufficiently, give out

light, so does the great nebula, which is a mass of gas poised in

space, become visible in virtue of the heat which it contains.

We are not left quite in doubt as to the constitution of these gaseous

nebulæ, for we can submit their light to the prism in the way I

explained when we were speaking of the stars. Distant though that ring

in Lyra may be, it is interesting to learn that the ingredients from

which it is made are not entirely different from substances we know on

our earth. The water in this glass, and every drop of water, is formed

by the union of two gases, of which one is hydrogen. This is an

extremely light material, as you see by a little balloon which ascends

so prettily when filled with it. Hydrogen also burns very readily,

though the flame is almost invisible. When I blow a jet of oxygen

through the hydrogen, I produce a little flame with a very intense

heat. For instance, I hold a steel pen in the flame, and it glows and

sputters, and falls down in white-hot drops. It is needless to say

that, as a constituent of water, hydrogen is one of the most important

elements on this earth. It is, therefore, of interest to learn that

hydrogen in some form or other is a constituent of the most distant

objects in space that the telescope has revealed.

Photographing the Nebulæ.

[Illustration: FIG. 8. THE PLEIADES.]

Of late years we have learned a great deal about nebulæ, by the help

which photography has given to us. Look at this group of stars which

constitutes that beautiful little configuration known as the Pleiades

(Fig. 8). It looks like a miniature representation of the Great Bear;

in fact, it would be far more appropriate to call the Pleiades the

Little Bear than to apply that title to another quite different

constellation, as has unfortunately been done. The Pleiades form a

group containing six or seven stars visible to the ordinary eye,

though persons endowed with exceptionally good vision can usually see

a few more. In an opera-glass the Pleiades becomes a beautiful

spectacle, though in a large telescope the stars appear too far apart

to make a really effective cluster. When Mr. Roberts took a photograph

of the Pleiades he placed a highly sensitive plate in his telescope,

and on that plate the Pleiades engraved their picture with their own

light. He left the plate exposed for hours, and on developing it not

only were the stars seen, but there were also patches of faint light

due to the presence of nebulæ. It could not be said that the objects

on the plate were fallacious, for another photograph was taken, when

the same appearances were reproduced.

When we look at that pretty group of stars which has attracted

admiration during all time, we are to think that some of those stars

are merely the bright points in a vast nebula, invisible to our

unaided eyes or even to our mighty telescopes, though capable of

recording its trace on the photographic plate. Does not this give us a

greatly increased notion of the extent of the universe, when we

reflect that by photography we are enabled to see much which the

mightiest of telescopes had previously failed to disclose?

Of all the nebulæ, numbering some thousands, there is but a single one

which can be seen without a telescope. It is in the constellation of

Andromeda, and on a clear dark night can just be seen with the unaided

eye as a faint stain of light on the sky. It has happened before now

that persons noticing this nebula for the first time have thought they

had discovered a comet. I would like you to try and find out this

object for yourselves.

If you look at it with an opera-glass it appears to be distinctly

elongated. You can see more of its structure when you view it in

larger instruments, but its nature was never made clear until some

beautiful photographs were taken by Mr. Roberts (Fig. 9).

Unfortunately, the nebula in Andromeda has not been placed in the best

position for its portrait from our point of view. It seems as if it

were a rather flat-shaped object, turned nearly edgewise towards us.

To look at the pattern on a plate, you would naturally hold the plate

so as to be able to look at it squarely. The pattern would not be seen

well if the plate were so tilted that its edge was turned towards you.

That seems to be nearly the way in which we are forced to view the

nebula in Andromeda. We can trace in the photograph some divisions

extending entirely round the nebula, showing that it seems to be

formed of a series of rings; and there are some outlying portions

which form part of the same system. Truly this is a marvellous object.

It is impossible for us to form any conception of the true dimensions

of this gigantic nebula; it is so far off that we have never yet been

able to determine its distance. Indeed, I may take this opportunity of

remarking that no astronomer has yet succeeded in ascertaining the

distance of any nebula. Everything, however, points to the conclusion

that they are at least as far as the stars.

[Illustration: FIG. 9. THE GREAT NEBULA IN ANDROMEDA.]

It is almost impossible to apply the methods which we use in finding

the distance of a star to the discovery of the distance of the

nebulæ. These flimsy bodies are usually too ill-defined to admit of

being measured with the precision and delicacy required for the

determination of distance. The measurements necessary for this purpose

can only be made from one star-like point to another similar point. If

we could choose a star in the nebula and determine its distance, then

of course, we have the distance of the nebula itself; but the

difficulty is that we have, in general, no means of knowing whether

the star does actually lie in the object. It may, for anything we can

tell, lie billions of miles nearer to us, or billions of miles further

off, and by merely happening to lie in the line of sight, appear to

glimmer in the nebula itself.

If we have any assurance that the star is surrounded by a mass of this

glowing vapor, then it may be possible to measure that nebula's

distance. It will occasionally happen that grounds can be found for

believing that a star which appears to be in the glowing gas does

veritably lie therein, and is not merely seen in the same direction.

There are hundreds of stars visible in a good drawing or a good

photograph of the famous object in Andromeda, and doubtless large

numbers of these are merely stars which happen to lie in the same line

of sight. The peculiar circumstances attending the history of one star

seem, however, to warrant us in making the assumption that it was

certainly in the nebula. The history of this star is a remarkable one.

It suddenly kindled from invisibility into brilliancy. How is a change

so rapid in the lustre of a star to be accounted for? In a few days

its brightness had undergone an extraordinary increase. Of course,

this does not tell us for certain that the star lay in the glowing

gas; but the most rational explanation that I have heard offered of

this occurrence is that due, I believe, to my friend Mr. Monck. He has

suggested that the sudden outbreak in brilliancy might be accounted

for on the same principles as those by which we explain the ignition

of meteors in our atmosphere. If a dark star, moving along with

terrific speed through space, were suddenly to plunge into a dense

region of the nebula, heat and light must be evolved in sufficient

abundance to transform the star into a brilliant object. If,

therefore, we knew the distance of this star at the time it was in

Andromeda, we should, of course, learn the distance of that

interesting object. This has been attempted, and it has thus been

proved that the Great Nebula must be very much further from us than is

that star of whose distance I attempted some time ago to give you a

notion.

We thus realize the enormous size of the Great Nebula. It appears that

if, on a map of this object, we were to lay down, accurately to scale,

a map of the solar system, putting the sun in the centre and all the

planets around their true proportions out to the boundary traced by

Neptune, this area, vast though it is, would be a mere speck on the

drawing of the object. Our system would have to be enormously bigger

before it sufficed to cover anything like the area of the sky included

in one of these great objects. Here is a sketch of a nebula, Fig. 10,

and near I have marked a dot, which is to indicate our solar system.

We may feel confident that the Great Nebula is at the very least as

mighty as this proportion would indicate.

[Illustration: FIG. 10. THE SOLAR SYSTEM AS COMPARED WITH A GREAT

NEBULA.]

RAIN AND SNOW

(FROM THE FORMS OF WATER.)

BY JOHN TYNDALL.

Oceanic Distillation.

[Illustration: SNOW CRYSTALS.]

At the equator, and within certain limits north and south of it, the

sun at certain periods of the year is directly overhead at noon. These

limits are called the Tropics of Cancer and of Capricorn. Upon the

belt comprised between these two circles the sun's rays fall with

their mightiest power; for here they shoot directly downwards, and

heat both earth and sea more than when they strike slantingly.

When the vertical sunbeams strike the land they heat it, and the air

in contact with the hot soil becomes heated in turn. But when heated

the air expands, and when it expands it becomes lighter. This lighter

air rises, like wood plunged into water, through the heavier air

overhead.

When the sunbeams fall upon the sea the water is warmed, though not so

much as the land. The warmed water expands, becomes thereby lighter,

and therefore continues to float upon the top. This upper layer of

water warms to some extent the air in contact with it, but it also

sends up a quantity of aqueous vapor, which being far lighter than

air, helps the latter to rise. Thus both from the land and from the

sea we have ascending currents established by the action of the sun.

When they reach a certain elevation in the atmosphere, these currents

divide and flow, part towards the north and part towards the south;

while from the north and the south a flow of heavier and colder air

sets in to supply the place of the ascending warm air.

Incessant circulation is thus established in the atmosphere. The

equatorial air and vapor flow above towards the north and south poles,

while the polar air flows below towards the equator. The two currents

of air thus established are called the upper and the lower trade

winds.

But before the air returns from the poles great changes have occurred.

For the air as it quitted the equatorial regions was laden with

aqueous vapor, which could not subsist in the cold polar regions. It

is there precipitated, falling sometimes as rain, or more commonly as

snow. The land near the pole is covered with this snow, which gives

birth to vast glaciers.

It is necessary that you should have a perfectly clear view of this

process, for great mistakes have been made regarding the manner in

which glaciers are related to the heat of the sun.

It was supposed that if the sun's heat were diminished, greater

glaciers than those now existing would be produced. But the lessening

of the sun's heat would infallibly diminish the quantity of aqueous

vapor, and thus cut off the glaciers at their source. A brief

illustration will complete your knowledge here.

In the process of ordinary distillation, the liquid to be distilled is

heated and converted into vapor in one vessel, and chilled and

reconverted into liquid in another. What has just been stated renders

it plain that the earth and its atmosphere constitute a vast

distilling apparatus in which the equatorial ocean plays the part of

the boiler, and the chill regions of the poles the part of the

condenser. In this process of distillation _heat_ plays quite as

necessary a part as _cold_, and before Bishop Heber could speak of

"Greenland's icy mountains," the equatorial ocean had to be warmed by

the sun. We shall have more to say upon this question afterwards.

The heating of the tropical air by the sun is _indirect_. The solar

beams have scarcely any power to heat the air through which they pass;

but they heat the land and ocean, and these communicate their heat to

the air in contact with them. The air and vapor start upwards charged

with the heat thus communicated.

Tropical Rains.

But long before the air and vapor from the equator reach the poles,

precipitation occurs. Wherever a humid warm wind mixes with a cold dry

one, rain falls. Indeed the heaviest rains occur at those places where

the sun is vertically overhead. We must enquire a little more closely

into their origin.

Fill a bladder about two-thirds full of air at the sea level, and take

it to the summit of Mount Blanc. As you ascend, the bladder becomes

more and more distended; at the top of the mountain it is fully

distended, and has evidently to bear a pressure from within. Returning

to the sea level you find that the tightness disappears, the bladder

finally appearing as flaccid as at first.

The reason is plain. At the sea level the air within the bladder has

to bear the pressure of the whole atmosphere, being thereby squeezed

into a comparatively small volume. In ascending the mountain, you

leave more and more of the atmosphere behind; the pressure becomes

less and less, and by its expansive force the air within the bladder

swells as the outside pressure is diminished. At the top of the

mountain the expansion is quite sufficient to render the bladder

tight, the pressure within being then actually greater than the

pressure without. By means of an air-pump we can show the expansion of

a balloon partly filled with air, when the external pressure has been

in part removed.

But why do I dwell upon this? Simply to make plain to you that the

_unconfined air_, heated at the earth's surface, and ascending by its

lightness, must expand more and more the higher it rises in the

atmosphere.

Young Folks' Library, Volume XI (of 20) Wonders of Earth, Sea and Sky · 第 20 / 23 段