BY SIR ROBERT BALL,

LOWNDEAN PROFESSOR OF ASTRONOMY AND GEOMETRY AT CAMBRIDGE, ENGLAND;

FORMERLY ROYAL ASTRONOMER OF IRELAND.

The light of the great orb of day emanates solely from a closely

fitting robe of surpassing brightness. The great bulk of the sun which

lies within that brilliant mantle is comparatively obscure, and might

at first seem to play but an unimportant part so far as the dispensing

of light and heat is concerned. It may indeed be likened to the

coal-cellar from whence are drawn the supplies that produce the warmth

and brightness of the domestic hearth; while the brilliant robe where

the sun develops its heat corresponds to the grate in which the coal

is consumed. With regard to the thickness of the robe, we might liken

this brilliant exterior to the rind of an orange, while the gloomy

interior regions would correspond to the edible portion of the fruit.

Generally speaking, the rind of the orange is rather too coarse for

the purpose of this illustration. It might be nearer the truth to

affirm that the luminous part of the sun may be compared to the

delicate filmy skin of the peach. There can be no doubt that if this

glorious veil were unhappily stripped from the sun, the great luminary

would forthwith lose its powers of shedding forth light and heat. The

spots which we see so frequently to fleck the dazzling surface, are

merely rents in the brilliant mantle through which we are permitted to

obtain glimpses of the comparatively non-luminous interior.

As the ability of the sun to warm and light this earth arises from the

peculiar properties of the thin glowing shell which surrounds it, a

problem of the greatest interest is presented in an inquiry as to the

material composition of this particular layer of solar substance.

We want, in fact, to ascertain what that special stuff can be which

enables the sun to be so useful to us dwellers on the earth. This

great problem has been solved, and the result is extremely interesting

and instructive; it has been discovered that the material which

confers on the sun its beneficent power is also a material which

is found in the greatest abundance on the earth, where it fulfils

purposes of the very highest importance. Let us see, in the first

place, what is the most patent fact with regard to the structure

of this solar mantle possessed of a glory so indescribable. It is

perfectly plain that it is not composed of any continuous solid

material. It has a granular character which is sometimes perceptible

when viewed through a powerful telescope, but which can be seen more

frequently and studied more satisfactorily on a photographic plate.

These granules have an obvious resemblance to clouds; and clouds,

indeed, we may call them. There is, however, a very wide difference

between the solar clouds and those clouds which float in our own

atmosphere. The clouds which we know so well are, of course, merely

vast collections of globules of water suspended in the air. No doubt

the mighty solar clouds do also consist of incalculable myriads

of globules of some particular substance floating in the solar

atmosphere. The material of which these solar clouds are composed

is, however, I need hardly say, not water, nor is it anything in

the remotest degree resembling water. Some years ago any attempt to

ascertain the particular substance out of which the solar clouds were

formed would at once have been regarded as futile; inasmuch as such a

problem would then have been thought to lie outside the possibilities

of human knowledge. The advance of discovery has, however, shed a

flood of light on the subject, and has revealed the nature of that

material to whose presence we are indebted for the solar beneficence.

The detection of the particular element to which all living creatures

are so much indebted is due to that distinguished physicist, Dr. G.

Johnstone Stoney.

In the whole range of science, one of the most remarkable discoveries

ever made is that which has taught us that the elementary bodies of

which the sun and the stars are constructed are essentially the same

as those of which the earth has been built. This discovery was indeed

as unexpected as it is interesting. Could we ever have anticipated

that a body ninety-three millions of miles away, as the sun is, or a

hundred million of millions of miles distant, as a star may be, should

actually prove to have been formed from the same materials as those

which compose this earth of ours and all which it contains, whether

animate or inanimate? Yet such is indeed the fact. We are thus, in

a measure, prepared to find that the material which forms the great

solar clouds may turn out to be a substance not quite unknown to the

terrestrial chemist. Nay, further, its very abundance in the sun might

seem to suggest that this particular material might perhaps prove to

be one which was very abundant on the earth.

[Illustration: THE SUN'S CORONA.

From a photograph taken by Professor Schaeberle, at Mina Bronces,

Chili, in April, 1893, and kindly loaned by Professor E.S. Holden,

director of the Lick Observatory.]

I had occasion to make use of the word carbon in a lecture which

I gave a short time ago, and I thought when I did so that I was of

course merely using a term with whose meaning all my audience must be

well acquainted. But I found out afterwards that in this matter I had

been mistaken. I was told that my introduction of the word carbon had

quite puzzled some of those who were listening to me. I learned that a

few of those who were unfamiliar with this word went to a gentleman

of their acquaintance who they thought would be likely to know, and

begged from him an explanation of this mysterious term; whereupon he

told them that he was not quite sure himself, but believed that carbon

was something which was made out of nitro-glycerine! Even at the risk

of telling what every schoolboy ought to know, I will say that

carbon is one of the commonest as well as one of the most remarkable

substances in nature. A lump of coke only differs from a piece

of carbon by the ash which the coke leaves behind when burned. As

charcoal is almost entirely carbon, so wood is largely composed of

this same element. Carbon is indeed present everywhere. In various

forms carbon is in the earth beneath our feet, and in the air which we

breath. This substance courses with the blood through our veins; it is

by carbon that the heat of the body is sustained; and the same element

is intimately associated with life in every phase. Nor is the presence

of carbon merely confined to this earth. We know it abounds on other

bodies in space. It has been shown to be eminently characteristic of

the composition of comets. Carbon is not only intimately associated

with articles of daily utility, and of plenteous abundance, but with

the most exquisite gems of "purest ray serene." More precious than

gold, more precious than rubies, the diamond itself is no more than

the same element in crystalline form. But the greatest of all the

functions of carbon in the universe has yet to be mentioned. This same

wonderful element has been shown to be in all probability the material

which constitutes those glowing solar clouds to whose kindly radiation

our very life owes its origin.

[Illustration: At 10.34 A.M. The height of the eruption at this stage

was 135,200 miles.]

[Illustration: At 10.40 A.M. Height, 161,500 miles.]

[Illustration: At 10.58 A.M. Height, 280,800 miles.

McClure's Magazine, Vol. 6, No. 2, January, 1896 · 第 70 / 89 题