First, how should the impacts postulated by this theory take place; is

it according to the laws of perfectly elastic bodies, or according to

those of bodies devoid of elasticity, or according to an intermediate

law? The corpuscles of Lesage can not act as perfectly elastic bodies;

otherwise the effect would be null, since the corpuscles intercepted by

the body _B_ would be replaced by others which would have rebounded from

_B_, and calculation proves that the compensation would be perfect. It

is necessary then that the impact make the corpuscles lose energy, and

this energy should appear under the form of heat. But how much heat

would thus be produced? Note that attraction passes through bodies; it

is necessary therefore to represent to ourselves the earth, for example,

not as a solid screen, but as formed of a very great number of very

small spherical molecules, which play individually the rôle of little

screens, but between which the corpuscles of Lesage may freely

circulate. So, not only the earth is not a solid screen, but it is not

even a cullender, since the voids occupy much more space than the

plenums. To realize this, recall that Laplace has demonstrated that

attraction, in traversing the earth, is weakened at most by one

ten-millionth part, and his proof is perfectly satisfactory: in fact, if

attraction were absorbed by the body it traverses, it would no longer be

proportional to the masses; it would be _relatively_ weaker for great

bodies than for small, since it would have a greater thickness to

traverse. The attraction of the sun for the earth would therefore be

_relatively_ weaker than that of the sun for the moon, and thence would

result, in the motion of the moon, a very sensible inequality. We should

therefore conclude, if we adopt the theory of Lesage, that the total

surface of the spherical molecules which compose the earth is at most

the ten-millionth part of the total surface of the earth.

Darwin has proved that the theory of Lesage only leads exactly to

Newton's law when we postulate particles entirely devoid of elasticity.

The attraction exerted by the earth on a mass 1 at a distance 1 will

then be proportional, at the same time, to the total surface _S_ of the

spherical molecules composing it, to the velocity _v_ of the corpuscles,

to the square root of the density [rho] of the medium formed by the

corpuscles. The heat produced will be proportional to _S_, to the

density [rho], and to the cube of the velocity _v_.

But it is necessary to take account of the resistance experienced by a

body moving in such a medium; it can not move, in fact, without going

against certain impacts, in fleeing, on the contrary, before those

coming in the opposite direction, so that the compensation realized in

the state of rest can no longer subsist. The calculated resistance is

proportional to _S_, to [rho] and to _v_; now, we know that the heavenly

bodies move as if they experienced no resistance, and the precision of

observations permits us to fix a limit to the resistance of the medium.

This resistance varying as _S_[rho]_v_, while the attraction varies as

_S_{sqrt([rho]_v_)}, we see that the ratio of the resistance to the

square of the attraction is inversely as the product _Sv_.

We have therefore a lower limit of the product _Sv_. We have already an

upper limit of _S_ (by the absorption of attraction by the body it

traverses); we have therefore a lower limit of the velocity _v_, which

must be at least 24·10^{17} times that of light.

From this we are able to deduce [rho] and the quantity of heat produced;

this quantity would suffice to raise the temperature 10^{26} degrees a

second; the earth would receive in a given time 10^{20} times more heat

than the sun emits in the same time; I am not speaking of the heat the

sun sends to the earth, but of that it radiates in all directions.

It is evident the earth could not long stand such a régime.

We should not be led to results less fantastic if, contrary to Darwin's

views, we endowed the corpuscles of Lesage with an elasticity imperfect

without being null. In truth, the vis viva of these corpuscles would not

be entirely converted into heat, but the attraction produced would

likewise be less, so that it would be only the part of this vis viva

converted into heat, which would contribute to produce the attraction

and that would come to the same thing; a judicious employment of the

theorem of the viriel would enable us to account for this.

The theory of Lesage may be transformed; suppress the corpuscles and

imagine the ether overrun in all senses by luminous waves coming from

all points of space. When a material object receives a luminous wave,

this wave exercises upon it a mechanical action due to the

Maxwell-Bartholi pressure, just as if it had received the impact of a

material projectile. The waves in question could therefore play the rôle

of the corpuscles of Lesage. This is what is supposed, for example, by

M. Tommasina.

The difficulties are not removed for all that; the velocity of

propagation can be only that of light, and we are thus led, for the

resistance of the medium, to an inadmissible figure. Besides, if the

light is all reflected, the effect is null, just as in the hypothesis of

the perfectly elastic corpuscles.

That there should be attraction, it is necessary that the light be

partially absorbed; but then there is production of heat. The

calculations do not differ essentially from those made in the ordinary

theory of Lesage, and the result retains the same fantastic character.

On the other hand, attraction is not absorbed by the body it traverses,

or hardly at all; it is not so with the light we know. Light which would

produce the Newtonian attraction would have to be considerably different

from ordinary light and be, for example, of very short wave length. This

does not count that, if our eyes were sensible of this light, the whole

heavens should appear to us much more brilliant than the sun, so that

the sun would seem to us to stand out in black, otherwise the sun would

repel us instead of attracting us. For all these reasons, light which

would permit of the explanation of attraction would be much more like

Röntgen rays than like ordinary light.

And besides, the X-rays would not suffice; however penetrating they may

seem to us, they could not pass through the whole earth; it would be

necessary therefore to imagine X'-rays much more penetrating than the

ordinary X-rays. Moreover a part of the energy of these X'-rays would

have to be destroyed, otherwise there would be no attraction. If you do

not wish it transformed into heat, which would lead to an enormous heat

production, you must suppose it radiated in every direction under the

form of secondary rays, which might be called X'' and which would have

to be much more penetrating still than the X'-rays, otherwise they would

in their turn derange the phenomena of attraction.

Such are the complicated hypotheses to which we are led when we try to

give life to the theory of Lesage.

But all we have said presupposes the ordinary laws of mechanics.

Will things go better if we admit the new dynamics? And first, can we

conserve the principles of relativity? Let us give at first to the

theory of Lesage its primitive form, and suppose space ploughed by

material corpuscles; if these corpuscles were perfectly elastic, the

laws of their impact would conform to this principle of relativity, but

we know that then their effect would be null. We must therefore suppose

these corpuscles are not elastic, and then it is difficult to imagine a

law of impact compatible with the principle of relativity. Besides, we

should still find a production of considerable heat, and yet a very

sensible resistance of the medium.

If we suppress these corpuscles and revert to the hypothesis of the

Maxwell-Bartholi pressure, the difficulties will not be less. This is

what Lorentz himself has attempted in his Memoir to the Amsterdam

Academy of Sciences of April 25, 1900.

Consider a system of electrons immersed in an ether permeated in every

sense by luminous waves; one of these electrons, struck by one of these

waves, begins to vibrate; its vibration will be synchronous with that of

light; but it may have a difference of phase, if the electron absorbs a

part of the incident energy. In fact, if it absorbs energy, this is

because the vibration of the ether _impels_ the electron; the electron

must therefore be slower than the ether. An electron in motion is

analogous to a convection current; therefore every magnetic field, in

particular that due to the luminous perturbation itself, must exert a

mechanical action upon this electron. This action is very slight;

moreover, it changes sign in the current of the period; nevertheless,

the mean action is not null if there is a difference of phase between

the vibrations of the electron and those of the ether. The mean action

is proportional to this difference, consequently to the energy absorbed

by the electron. I can not here enter into the detail of the

calculations; suffice it to say only that the final result is an

attraction of any two electrons, varying inversely as the square of the

distance and proportional to the energy absorbed by the two electrons.

Therefore there can not be attraction without absorption of light and,

consequently, without production of heat, and this it is which

determined Lorentz to abandon this theory, which, at bottom, does not

differ from that of Lesage-Maxwell-Bartholi. He would have been much

more dismayed still if he had pushed the calculation to the end. He

would have found that the temperature of the earth would have to

increase 10^{12} degrees a second.

IV

_Conclusions_

I have striven to give in few words an idea as complete as possible of

these new doctrines; I have sought to explain how they took birth;

otherwise the reader would have had ground to be frightened by their

boldness. The new theories are not yet demonstrated; far from it; only

they rest upon an aggregate of probabilities sufficiently weighty for us

not to have the right to treat them with disregard.

New experiments will doubtless teach us what we should finally think of

them. The knotty point of the question lies in Kaufmann's experiment and

those that may be undertaken to verify it.

In conclusion, permit me a word of warning. Suppose that, after some

years, these theories undergo new tests and triumph; then our secondary

education will incur a great danger; certain professors will doubtless

wish to make a place for the new theories.

Novelties are so attractive, and it is so hard not to seem highly

advanced! At least there will be the wish to open vistas to the pupils

and, before teaching them the ordinary mechanics, to let them know it

has had its day and was at best good enough for that old dolt Laplace.

And then they will not form the habit of the ordinary mechanics.

Is it well to let them know this is only approximative? Yes; but later,

when it has penetrated to their very marrow, when they shall have taken

the bent of thinking only through it, when there shall no longer be risk

of their unlearning it, then one may, without inconvenience, show them

its limits.

It is with the ordinary mechanics that they must live; this alone will

they ever have to apply. Whatever be the progress of automobilism, our

vehicles will never attain speeds where it is not true. The other is

only a luxury, and we should think of the luxury only when there is no

longer any risk of harming the necessary.

BOOK IV

ASTRONOMIC SCIENCE

CHAPTER I

THE MILKY WAY AND THE THEORY OF GASES

The considerations to be here developed have scarcely as yet drawn the

attention of astronomers; there is hardly anything to cite except an

ingenious idea of Lord Kelvin's, which has opened a new field of

research, but still waits to be followed out. Nor have I original

results to impart, and all I can do is to give an idea of the problems

presented, but which no one hitherto has undertaken to solve. Every one

knows how a large number of modern physicists represent the constitution

of gases; gases are formed of an innumerable multitude of molecules

which, at high speeds, cross and crisscross in every direction. These

molecules probably act at a distance one upon another, but this action

decreases very rapidly with distance, so that their trajectories remain

sensibly straight; they cease to be so only when two molecules happen to

pass very near to each other; in this case, their mutual attraction or

repulsion makes them deviate to right or left. This is what is sometimes

called an impact; but the word _impact_ is not to be understood in its

usual sense; it is not necessary that the two molecules come into

contact, it suffices that they approach sufficiently near each other for

their mutual attractions to become sensible. The laws of the deviation

they undergo are the same as for a veritable impact.

It seems at first that the disorderly impacts of this innumerable dust

can engender only an inextricable chaos before which analysis must

recoil. But the law of great numbers, that supreme law of chance, comes

to our aid; in presence of a semi-disorder, we must despair, but in

extreme disorder, this statistical law reestablishes a sort of mean

order where the mind can recover. It is the study of this mean order

which constitutes the kinetic theory of gases; it shows us that the

velocities of the molecules are equally distributed among all the

directions, that the rapidity of these velocities varies from one

molecule to another, but that even this variation is subject to a law

called Maxwell's law. This law tells us how many of the molecules move

with such and such a velocity. As soon as the gas departs from this law,

the mutual impacts of the molecules, in modifying the rapidity and

direction of their velocities, tend to bring it promptly back.

Physicists have striven, not without success, to explain in this way the

experimental properties of gases; for example Mariotte's law.

Consider now the milky way; there also we see an innumerable dust; only

the grains of this dust are not atoms, they are stars; these grains move

also with high velocities; they act at a distance one upon another, but

this action is so slight at great distance that their trajectories are

straight; and yet, from time to time, two of them may approach near

enough to be deviated from their path, like a comet which has passed too

near Jupiter. In a word, to the eyes of a giant for whom our suns would

be as for us our atoms, the milky way would seem only a bubble of gas.

Such was Lord Kelvin's leading idea. What may be drawn from this

comparison? In how far is it exact? This is what we are to investigate

together; but before reaching a definite conclusion, and without wishing

to prejudge it, we foresee that the kinetic theory of gases will be for

the astronomer a model he should not follow blindly, but from which he

may advantageously draw inspiration. Up to the present, celestial

mechanics has attacked only the solar system or certain systems of

double stars. Before the assemblage presented by the milky way, or the

agglomeration of stars, or the resolvable nebulae it recoils, because it

sees therein only chaos. But the milky way is not more complicated than

a gas; the statistical methods founded upon the calculus of

probabilities applicable to a gas are also applicable to it. Before all,

it is important to grasp the resemblance of the two cases, and their

difference.

Lord Kelvin has striven to determine in this manner the dimensions of

the milky way; for that we are reduced to counting the stars visible in

our telescopes; but we are not sure that behind the stars we see, there

are not others we do not see; so that what we should measure in this way

would not be the size of the milky way, it would be the range of our

instruments.

The new theory comes to offer us other resources. In fact, we know the

motions of the stars nearest us, and we can form an idea of the rapidity

and direction of their velocities. If the ideas above set forth are

exact, these velocities should follow Maxwell's law, and their mean

value will tell us, so to speak, that which corresponds to the

temperature of our fictitious gas. But this temperature depends itself

upon the dimensions of our gas bubble. In fact, how will a gaseous mass

let loose in the void act, if its elements attract one another according

to Newton's law? It will take a spherical form; moreover, because of

gravitation, the density will be greater at the center, the pressure

also will increase from the surface to the center because of the weight

of the outer parts drawn toward the center; finally, the temperature

will increase toward the center: the temperature and the pressure being

connected by the law called adiabatic, as happens in the successive

layers of our atmosphere. At the surface itself, the pressure will be

null, and it will be the same with the absolute temperature, that is to

say with the velocity of the molecules.

A question comes here: I have spoken of the adiabatic law, but this law

is not the same for all gases, since it depends upon the ratio of their

two specific heats; for the air and like gases, this ratio is 1.42; but

is it to air that it is proper to liken the milky way? Evidently not, it

should be regarded as a mono-atomic gas, like mercury vapor, like argon,

like helium, that is to say that the ratio of the specific heats should

be taken equal to 1.66. And, in fact, one of our molecules would be for

example the solar system; but the planets are very small personages, the

sun alone counts, so that our molecule is indeed mono-atomic. And even

if we take a double star, it is probable that the action of a strange

star which might approach it would become sufficiently sensible to

deviate the motion of general translation of the system much before

being able to trouble the relative orbits of the two components; the

double star, in a word, would act like an indivisible atom.

However that may be, the pressure, and consequently the temperature, at

the center of the gaseous sphere would be by so much the greater as the

sphere was larger since the pressure increases by the weight of all the

superposed layers. We may suppose that we are nearly at the center of

the milky way, and by observing the mean proper velocity of the stars,

we shall know that which corresponds to the central temperature of our

gaseous sphere and we shall determine its radius.

We may get an idea of the result by the following considerations: make a

simpler hypothesis: the milky way is spherical, and in it the masses are

distributed in a homogeneous manner; thence results that the stars in it

describe ellipses having the same center. If we suppose the velocity

becomes nothing at the surface, we may calculate this velocity at the

center by the equation of vis viva. Thus we find that this velocity is

proportional to the radius of the sphere and to the square root of its

density. If the mass of this sphere was that of the sun and its radius

that of the terrestrial orbit, this velocity would be (it is easy to

see) that of the earth in its orbit. But in the case we have supposed,

the mass of the sun should be distributed in a sphere of radius

1,000,000 times greater, this radius being the distance of the nearest

stars; the density is therefore 10^{18} times less; now, the velocities

are of the same order, therefore it is necessary that the radius be

10^{9} times greater, be 1,000 times the distance of the nearest stars,

which would give about a thousand millions of stars in the milky way.

But you will say these hypothesis differ greatly from the reality;

first, the milky way is not spherical and we shall soon return to this

point, and again the kinetic theory of gases is not compatible with the

hypothesis of a homogeneous sphere. But in making the exact calculation

according to this theory, we should find a different result, doubtless,

but of the same order of magnitude; now in such a problem the data are

so uncertain that the order of magnitude is the sole end to be aimed at.

And here a first remark presents itself; Lord Kelvin's result, which I

have obtained again by an approximative calculation, agrees sensibly

with the evaluations the observers have made with their telescopes; so

that we must conclude we are very near to piercing through the milky

way. But that enables us to answer another question. There are the stars

we see because they shine; but may there not be dark stars circulating

in the interstellar spaces whose existence might long remain unknown?

But then, what Lord Kelvin's method would give us would be the total

number of stars, including the dark stars; as his figure is comparable

to that the telescope gives, this means there is no dark matter, or at

least not so much as of shining matter.

Before going further, we must look at the problem from another angle. Is

the milky way thus constituted truly the image of a gas properly so

called? You know Crookes has introduced the notion of a fourth state of

matter, where gases having become too rarefied are no longer true gases

and become what he calls radiant matter. Considering the slight density

of the milky way, is it the image of gaseous matter or of radiant

matter? The consideration of what is called the _free path_ will furnish

us the answer.

The trajectory of a gaseous molecule may be regarded as formed of

straight segments united by very small arcs corresponding to the

successive impacts. The length of each of these segments is what is

called the free path; of course this length is not the same for all the

segments and for all the molecules; but we may take a mean; this is what

is called the _mean path_. This is the greater the less the density of

the gas. The matter will be radiant if the mean path is greater than the

dimensions of the receptacle wherein the gas is enclosed, so that a

molecule has a chance to go across the whole receptacle without

undergoing an impact; if the contrary be the case, it is gaseous. From

this it follows that the same fluid may be radiant in a little

receptacle and gaseous in a big one; this perhaps is why, in a Crookes

tube, it is necessary to make the vacuum by so much the more complete as

the tube is larger.

How is it then for the milky way? This is a mass of gas of which the

density is very slight, but whose dimensions are very great; has a star

chances of traversing it without undergoing an impact, that is to say

without passing sufficiently near another star to be sensibly deviated

from its route! What do we mean by _sufficiently near_? That is perforce

a little arbitrary; take it as the distance from the sun to Neptune,

which would represent a deviation of a dozen degrees; suppose therefore

each of our stars surrounded by a protective sphere of this radius;

could a straight pass between these spheres? At the mean distance of the

stars of the milky way, the radius of these spheres will be seen under

an angle of about a tenth of a second; and we have a thousand millions

of stars. Put upon the celestial sphere a thousand million little

circles of a tenth of a second radius. Are the chances that these

circles will cover a great number of times the celestial sphere? Far

from it; they will cover only its sixteen thousandth part. So the milky

way is not the image of gaseous matter, but of Crookes' radiant matter.

Nevertheless, as our foregoing conclusions are happily not at all

precise, we need not sensibly modify them.

But there is another difficulty: the milky way is not spherical, and we

have reasoned hitherto as if it were, since this is the form of

equilibrium a gas isolated in space would take. To make amends,

agglomerations of stars exist whose form is globular and to which would

better apply what we have hitherto said. Herschel has already endeavored

to explain their remarkable appearances. He supposed the stars of the

aggregates uniformly distributed, so that an assemblage is a homogeneous

sphere; each star would then describe an ellipse and all these orbits

would be passed over in the same time, so that at the end of a period

the aggregate would take again its primitive configuration and this

configuration would be stable. Unluckily, the aggregates do not appear

to be homogeneous; we see a condensation at the center, we should

observe it even were the sphere homogeneous, since it is thicker at the

center; but it would not be so accentuated. We may therefore rather

compare an aggregate to a gas in adiabatic equilibrium, which takes the

spherical form because this is the figure of equilibrium of a gaseous

mass.

But, you will say, these aggregates are much smaller than the milky way,

of which they even in probability make part, and even though they be

more dense, they will rather present something analogous to radiant

matter; now, gases attain their adiabatic equilibrium only through

innumerable impacts of the molecules. That might perhaps be adjusted.

Suppose the stars of the aggregate have just enough energy for their

velocity to become null when they reach the surface; then they may

traverse the aggregate without impact, but arrived at the surface they

will go back and will traverse it anew; after a great number of

crossings, they will at last be deviated by an impact; under these

conditions, we should still have a matter which might be regarded as

gaseous; if perchance there had been in the aggregate stars whose

velocity was greater, they have long gone away out of it, they have left

it never to return. For all these reasons, it would be interesting to

examine the known aggregates, to seek to account for the law of the

densities, and to see if it is the adiabatic law of gases.

But to return to the milky way; it is not spherical and would rather be

represented as a flattened disc. It is clear then that a mass starting

without velocity from the surface will reach the center with different

velocities, according as it starts from the surface in the neighborhood

of the middle of the disc or just on the border of the disc; the

velocity would be notably greater in the latter case. Now, up to the

present, we have supposed that the proper velocities of the stars, those

we observe, must be comparable to those which like masses would attain;

this involves a certain difficulty. We have given above a value for the

dimensions of the milky way, and we have deduced it from the observed

proper velocities which are of the same order of magnitude as that of

the earth in its orbit; but which is the dimension we have thus

measured? Is it the thickness? Is it the radius of the disc? It is

doubtless something intermediate; but what can we say then of the

thickness itself, or of the radius of the disc? Data are lacking to make

the calculation; I shall confine myself to giving a glimpse of the

possibility of basing an evaluation at least approximate upon a deeper

discussion of the proper motions.

And then we find ourselves facing two hypotheses: either the stars of

the milky way are impelled by velocities for the most part parallel to

the galactic plane, but otherwise distributed uniformly in all

directions parallel to this plane. If this be so, observation of the

proper motions should show a preponderance of components parallel to the

milky way; this is to be determined, because I do not know whether a

systematic discussion has ever been made from this view-point. On the

other hand, such an equilibrium could only be provisory, since because

of impacts the molecules, I mean the stars, would in the long run

acquire notable velocities in the sense perpendicular to the milky way

and would end by swerving from its plane, so that the system would tend

toward the spherical form, the only figure of equilibrium of an isolated

gaseous mass.

Or else the whole system is impelled by a common rotation, and for that

reason is flattened like the earth, like Jupiter, like all bodies that

twirl. Only, as the flattening is considerable, the rotation must be

rapid; rapid doubtless, but it must be understood in what sense this

word is used. The density of the milky way is 10^{23} times less than

that of the sun; a velocity of rotation sqrt(10^{25}) times less than

that of the sun, for it would, therefore, be the equivalent so far as

concerns flattening; a velocity 10^{12} times slower than that of the

earth, say a thirtieth of a second of arc in a century, would be a very

rapid rotation, almost too rapid for stable equilibrium to be possible.

In this hypothesis, the observable proper motions would appear to us

uniformly distributed, and there would no longer be a preponderance of

components parallel to the galactic plane.

They will tell us nothing about the rotation itself, since we belong to

the turning system. If the spiral nebulæ are other milky ways, foreign

to ours, they are not borne along in this rotation, and we might study

their proper motions. It is true they are very far away; if a nebula has

the dimensions of the milky way and if its apparent radius is for

example 20", its distance is 10,000 times the radius of the milky way.

But that makes no difference, since it is not about the translation of

our system that we ask information from them, but about its rotation.

The fixed stars, by their apparent motion, reveal to us the diurnal

rotation of the earth, though their distance is immense. Unluckily, the

possible rotation of the milky way, however rapid it may be relatively,

is very slow viewed absolutely, and besides the pointings on nebulæ can

not be very precise; therefore thousands of years of observations would

be necessary to learn anything.

However that may be, in this second hypothesis, the figure of the milky

way would be a figure of final equilibrium.

I shall not further discuss the relative value of these two hypotheses

since there is a third which is perhaps more probable. We know that

among the irresolvable nebulæ, several kinds may be distinguished: the

irregular nebulæ like that of Orion, the planetary and annular nebulæ,

the spiral nebulæ. The spectra of the first two families have been

determined, they are discontinuous; these nebulæ are therefore not

formed of stars; besides, their distribution on the heavens seems to

depend upon the milky way; whether they have a tendency to go away from

it, or on the contrary to approach it, they make therefore a part of the

system. On the other hand, the spiral nebulæ are generally considered as

independent of the milky way; it is supposed that they, like it, are

formed of a multitude of stars, that they are, in a word, other milky

ways very far away from ours. The recent investigations of Stratonoff

tend to make us regard the milky way itself as a spiral nebula, and this

is the third hypothesis of which I wish to speak.

How can we explain the very singular appearances presented by the spiral

nebulæ, which are too regular and too constant to be due to chance?

First of all, to take a look at one of these representations is enough

to see that the mass is in rotation; we may even see what the sense of

the rotation is; all the spiral radii are curved in the same sense; it

is evident that the _moving wing_ lags behind the pivot and that fixes

the sense of the rotation. But this is not all; it is evident that these

nebulæ can not be likened to a gas at rest, nor even to a gas in

relative equilibrium under the sway of a uniform rotation; they are to

be compared to a gas in permanent motion in which internal currents

prevail.

Suppose, for example, that the rotation of the central nucleus is rapid

(you know what I mean by this word), too rapid for stable equilibrium;

then at the equator the centrifugal force will drive it away over the

attraction, and the stars will tend to break away at the equator and

will form divergent currents; but in going away, as their moment of

rotation remains constant, while the radius vector augments, their

angular velocity will diminish, and this is why the moving wing seems to

lag back.

From this point of view, there would not be a real permanent motion, the

central nucleus would constantly lose matter which would go out of it

never to return, and would drain away progressively. But we may modify

the hypothesis. In proportion as it goes away, the star loses its

velocity and ends by stopping; at this moment attraction regains

possession of it and leads it back toward the nucleus; so there will be

centripetal currents. We must suppose the centripetal currents are the

first rank and the centrifugal currents the second rank, if we adopt the

comparison with a troop in battle executing a change of front; and, in

fact, it is necessary that the composite centrifugal force be

compensated by the attraction exercised by the central layers of the

swarm upon the extreme layers.

Besides, at the end of a certain time a permanent régime establishes

itself; the swarm being curved, the attraction exercised upon the pivot

by the moving wing tends to slow up the pivot and that of the pivot upon

the moving wing tends to accelerate the advance of this wing which no

longer augments its lag, so that finally all the radii end by turning

with a uniform velocity. We may still suppose that the rotation of the

nucleus is quicker than that of the radii.

A question remains; why do these centripetal and centrifugal swarms tend

to concentrate themselves in radii instead of disseminating themselves a

little everywhere? Why do these rays distribute themselves regularly? If

the swarms concentrate themselves, it is because of the attraction

exercised by the already existing swarms upon the stars which go out

from the nucleus in their neighborhood. After an inequality is produced,

it tends to accentuate itself in this way.

Why do the rays distribute themselves regularly? That is less obvious.

Suppose there is no rotation, that all the stars are in two planes at

right angles, in such a way that their distribution is symmetric with

regard to these two planes.

By symmetry, there would be no reason for their going out of these

planes, nor for the symmetry changing. This configuration would give us

therefore equilibrium, but _this would be an unstable equilibrium_.

If on the contrary, there is rotation, we shall find an analogous

configuration of equilibrium with four curved rays, equal to each other

and intersecting at 90°, and if the rotation is sufficiently rapid, this

equilibrium is stable.

I am not in position to make this more precise: enough if you see that

these spiral forms may perhaps some day be explained by only the law of

gravitation and statistical consideration recalling those of the theory

of gases.

What has been said of internal currents shows it is of interest to

discuss systematically the aggregate of proper motions; this may be done

in a hundred years, when the second edition is issued of the chart of

the heavens and compared with the first, that we now are making.

But, in conclusion, I wish to call your attention to a question, that of

the age of the milky way or the nebulæ. If what we think we see is

confirmed, we can get an idea of it. That sort of statistical

equilibrium of which gases give us the model is established only in

consequence of a great number of impacts. If these impacts are rare, it

can come about only after a very long time; if really the milky way (or

at least the agglomerations which are contained in it), if the nebulæ

have attained this equilibrium, this means they are very old, and we

shall have an inferior limit of their age. Likewise we should have of it

a superior limit; this equilibrium is not final and can not last always.

Our spiral nebulæ would be comparable to gases impelled by permanent

motions; but gases in motion are viscous and their velocities end by

wearing out. What here corresponds to the viscosity (and which depends

upon the chances of impact of the molecules) is excessively slight, so

that the present régime may persist during an extremely long time, yet

not forever, so that our milky ways can not live eternally nor become

infinitely old.

And this is not all. Consider our atmosphere: at the surface must reign

a temperature infinitely small and the velocity of the molecules there

is near zero. But this is a question only of the mean velocity; as a

consequence of impacts, one of these molecules may acquire (rarely, it

is true) an enormous velocity, and then it will rush out of the

atmosphere, and once out, it will never return; therefore our atmosphere

drains off thus with extreme slowness. The milky way also from time to

time loses a star by the same mechanism, and that likewise limits its

duration.

Well, it is certain that if we compute in this manner the age of the

milky way, we shall get enormous figures. But here a difficulty presents

itself. Certain physicists, relying upon other considerations, reckon

that suns can have only an ephemeral existence, about fifty million

years; our minimum would be much greater than that. Must we believe that

the evolution of the milky way began when the matter was still dark? But

how have the stars composing it reached all at the same time adult age,

an age so briefly to endure? Or must they reach there all successively,

and are those we see only a feeble minority compared with those

extinguished or which shall one day light up? But how reconcile that

with what we have said above on the absence of a noteworthy proportion

of dark matter? Should we abandon one of the two hypotheses, and which?

I confine myself to pointing out the difficulty without pretending to

solve it; I shall end therefore with a big interrogation point.

However, it is interesting to set problems, even when their solution

seems very far away.

CHAPTER II

FRENCH GEODESY

Every one understands our interest in knowing the form and dimensions of

our earth; but some persons will perhaps be surprised at the exactitude

sought after. Is this a useless luxury? What good are the efforts so

expended by the geodesist?

Should this question be put to a congressman, I suppose he would say:

"I am led to believe that geodesy is one of the most useful of the

sciences; because it is one of those costing us most dear." I shall try

to give you an answer a little more precise.

The great works of art, those of peace as well as those of war, are not

to be undertaken without long studies which save much groping,

miscalculation and useless expense. These studies can only be based upon

a good map. But a map will be only a valueless phantasy if constructed

without basing it upon a solid framework. As well make stand a human

body minus the skeleton.

Now, this framework is given us by geodesic measurements; so, without

geodesy, no good map; without a good map, no great public works.

These reasons will doubtless suffice to justify much expense; but these

are arguments for practical men. It is not upon these that it is proper

to insist here; there are others higher and, everything considered, more

important.

So we shall put the question otherwise; can geodesy aid us the better to

know nature? Does it make us understand its unity and harmony? In

reality an isolated fact is of slight value, and the conquests of

science are precious only if they prepare for new conquests.

If therefore a little hump were discovered on the terrestrial ellipsoid,

this discovery would be by itself of no great interest. On the other

hand, it would become precious if, in seeking the cause of this hump, we

hoped to penetrate new secrets.

Well, when, in the eighteenth century, Maupertuis and La Condamine

braved such opposite climates, it was not solely to learn the shape of

our planet, it was a question of the whole world-system.

If the earth was flattened, Newton triumphed and with him the doctrine

of gravitation and the whole modern celestial mechanics.

And to-day, a century and a half after the victory of the Newtonians,

think you geodesy has nothing more to teach us?

We know not what is within our globe. The shafts of mines and borings

have let us know a layer of 1 or 2 kilometers thickness, that is to say,

the millionth part of the total mass; but what is beneath?

Of all the extraordinary journeys dreamed by Jules Verne, perhaps that

to the center of the earth took us to regions least explored.

But these deep-lying rocks we can not reach, exercise from afar their

attraction which operates upon the pendulum and deforms the terrestrial

spheroid. Geodesy can therefore weigh them from afar, so to speak, and

tell us of their distribution. Thus will it make us really see those

mysterious regions which Jules Verne only showed us in imagination.

This is not an empty illusion. M. Faye, comparing all the measurements,

has reached a result well calculated to surprise us. Under the oceans,

in the depths, are rocks of very great density; under the continents, on

the contrary, are empty spaces.

New observations will modify perhaps the details of these conclusions.

In any case, our venerated dean has shown us where to search and what

the geodesist may teach the geologist, desirous of knowing the interior

constitution of the earth, and even the thinker wishing to speculate

upon the past and the origin of this planet.

And now, why have I entitled this chapter _French Geodesy_? It is

because, in each country, this science has taken, more than all others,

perhaps, a national character. It is easy to see why.

There must be rivalry. The scientific rivalries are always courteous, or

at least almost always; in any case, they are necessary, because they

are always fruitful. Well, in those enterprises which require such long

efforts and so many collaborators, the individual is effaced, in spite

of himself, of course; no one has the right to say: this is my work.

Therefore it is not between men, but between nations that rivalries go

on.

So we are led to seek what has been the part of France. Her part I

believe we are right to be proud of.

At the beginning of the eighteenth century, long discussions arose

between the Newtonians who believed the earth flattened, as the theory

of gravitation requires, and Cassini, who, deceived by inexact

measurements, believed our globe elongated. Only direct observation

could settle the question. It was our Academy of Sciences that undertook

this task, gigantic for the epoch.

While Maupertuis and Clairaut measured a degree of meridian under the

polar circle, Bouguer and La Condamine went toward the Andes Mountains,

in regions then under Spain which to-day are the Republic of Ecuador.

Our envoys were exposed to great hardships. Traveling was not as easy as

at present.

Truly, the country where Maupertuis operated was not a desert and he

even enjoyed, it is said, among the Laplanders those sweet satisfactions

of the heart that real arctic voyagers never know. It was almost the

region where, in our days, comfortable steamers carry, each summer,

hosts of tourists and young English people. But in those days Cook's

agency did not exist and Maupertuis really believed he had made a polar

expedition.

Perhaps he was not altogether wrong. The Russians and the Swedes carry

out to-day analogous measurements at Spitzbergen, in a country where

there is real ice-cap. But they have quite other resources, and the

difference of time makes up for that of latitude.

The name of Maupertuis has reached us much scratched by the claws of

Doctor Akakia; the scientist had the misfortune to displease Voltaire,

who was then the king of mind. He was first praised beyond measure; but

the flatteries of kings are as much to be dreaded as their displeasure,

because the days after are terrible. Voltaire himself knew something of

this.

Voltaire called Maupertuis, my amiable master in thinking, marquis of

the polar circle, dear flattener out of the world and Cassini, and even,

flattery supreme, Sir Isaac Maupertuis; he wrote him: "Only the king of

Prussia do I put on a level with you; he only lacks being a geometer."

But soon the scene changes, he no longer speaks of deifying him, as in

days of yore the Argonauts, or of calling down from Olympus the council

of the gods to contemplate his works, but of chaining him up in a

madhouse. He speaks no longer of his sublime mind, but of his despotic

pride, plated with very little science and much absurdity.

I care not to relate these comico-heroic combats; but permit me some

reflections on two of Voltaire's verses. In his 'Discourse on

Moderation' (no question of moderation in praise and criticism), the

poet has written:

You have confirmed in regions drear

What Newton discerned without going abroad.

These two verses (which replace the hyperbolic praises of the first

period) are very unjust, and doubtless Voltaire was too enlightened not

to know it.

Then, only those discoveries were esteemed which could be made without

leaving one's house.

To-day, it would rather be theory that one would make light of.

This is to misunderstand the aim of science.

Is nature governed by caprice, or does harmony rule there? That is the

question. It is when it discloses to us this harmony that science is

beautiful and so worthy to be cultivated. But whence can come to us this

revelation, if not from the accord of a theory with experiment? To seek

whether this accord exists or if it fails, this therefore is our aim.

Consequently these two terms, which we must compare, are as

indispensable the one as the other. To neglect one for the other would

be nonsense. Isolated, theory would be empty, experiment would be blind;

each would be useless and without interest.

Maupertuis therefore deserves his share of glory. Truly, it will not

equal that of Newton, who had received the spark divine; nor even that

of his collaborator Clairaut. Yet it is not to be despised, because his

work was necessary, and if France, outstripped by England in the

seventeenth century, has so well taken her revenge in the century

following, it is not alone to the genius of Clairauts, d'Alemberts,

Laplaces that she owes it; it is also to the long patience of the

Maupertuis and the La Condamines.

We reach what may be called the second heroic period of geodesy. France

is torn within. All Europe is armed against her; it would seem that

these gigantic combats might absorb all her forces. Far from it; she

still has them for the service of science. The men of that time recoiled

before no enterprise, they were men of faith.

Delambre and Méchain were commissioned to measure an arc going from

Dunkerque to Barcelona. This time there was no going to Lapland or to

Peru; the hostile squadrons had closed to us the ways thither. But,

though the expeditions are less distant, the epoch is so troubled that

the obstacles, the perils even, are just as great.

In France, Delambre had to fight against the ill-will of suspicious

municipalities. One knows that the steeples, which are visible from so

far, and can be aimed at with precision, often serve as signal points to

geodesists. But in the region Delambre traversed there were no longer

any steeples. A certain proconsul had passed there, and boasted of

knocking down all the steeples rising proudly above the humble abode of

the sans-culottes. Pyramids then were built of planks and covered with

white cloth to make them more visible. That was quite another thing:

with white cloth! What was this rash person who, upon our heights so

recently set free, dared to raise the hateful standard of the

counter-revolution? It was necessary to border the white cloth with blue

and red bands.

Méchain operated in Spain; the difficulties were other; but they were

not less. The Spanish peasants were hostile. There steeples were not

lacking: but to install oneself in them with mysterious and perhaps

diabolic instruments, was it not sacrilege? The revolutionists were

allies of Spain, but allies smelling a little of the stake.

"Without cease," writes Méchain, "they threaten to butcher us."

Fortunately, thanks to the exhortations of the priests, to the pastoral

letters of the bishops, these ferocious Spaniards contented themselves

with threatening.

Some years after Méchain made a second expedition into Spain: he

proposed to prolong the meridian from Barcelona to the Balearics. This

was the first time it had been attempted to make the triangulations

overpass a large arm of the sea by observing signals installed upon some

high mountain of a far-away isle. The enterprise was well conceived and

well prepared; it failed however.

The French scientist encountered all sorts of difficulties of which he

complains bitterly in his correspondence. "Hell," he writes, perhaps

with some exaggeration--"hell and all the scourges it vomits upon the

earth, tempests, war, the plague and black intrigues are therefore

unchained against me!"

The fact is that he encountered among his collaborators more of proud

obstinacy than of good will and that a thousand accidents retarded his

work. The plague was nothing, the fear of the plague was much more

redoubtable; all these isles were on their guard against the neighboring

isles and feared lest they should receive the scourge from them. Méchain

obtained permission to disembark only after long weeks upon the

condition of covering all his papers with vinegar; this was the

antisepsis of that time.

Disgusted and sick, he had just asked to be recalled, when he died.

Arago and Biot it was who had the honor of taking up the unfinished work

and carrying it on to completion.

Thanks to the support of the Spanish government, to the protection of

several bishops and, above all, to that of a famous brigand chief, the

operations went rapidly forward. They were successfully completed, and

Biot had returned to France when the storm burst.

It was the moment when all Spain took up arms to defend her independence

against France. Why did this stranger climb the mountains to make

signals? It was evidently to call the French army. Arago was able to

escape the populace only by becoming a prisoner. In his prison, his only

distraction was reading in the Spanish papers the account of his own

execution. The papers of that time sometimes gave out news prematurely.

He had at least the consolation of learning that he died with courage

and like a Christian.

Even the prison was no longer safe; he had to escape and reach Algiers.

There, he embarked for Marseilles on an Algerian vessel. This ship was

captured by a Spanish corsair, and behold Arago carried back to Spain

and dragged from dungeon to dungeon, in the midst of vermin and in the

most shocking wretchedness.

If it had only been a question of his subjects and his guests, the dey

would have said nothing. But there were on board two lions, a present

from the African sovereign to Napoleon. The dey threatened war.

The vessel and the prisoners were released. The port should have been

properly reached, since they had on board an astronomer; but the

astronomer was seasick, and the Algerian seamen, who wished to make

Marseilles, came out at Bougie. Thence Arago went to Algiers, traversing

Kabylia on foot in the midst of a thousand perils. He was long detained

in Africa and threatened with the convict prison. Finally he was able to

get back to France; his observations, which he had preserved and

safeguarded under his shirt, and, what is still more remarkable, his

instruments had traversed unhurt these terrible adventures. Up to this

point, not only did France hold the foremost place, but she occupied the

stage almost alone.

In the years which follow, she has not been inactive and our

staff-office map is a model. However, the new methods of observation and

calculation have come to us above all from Germany and England. It is

only in the last forty years that France has regained her rank. She owes

it to a scientific officer, General Perrier, who has successfully

executed an enterprise truly audacious, the junction of Spain and

Africa. Stations were installed on four peaks upon the two sides of the

Mediterranean. For long months they awaited a calm and limpid

atmosphere. At last was seen the little thread of light which had

traversed 300 kilometers over the sea. The undertaking had succeeded.

To-day have been conceived projects still more bold. From a mountain

near Nice will be sent signals to Corsica, not now for geodesic

determinations, but to measure the velocity of light. The distance is

only 200 kilometers; but the ray of light is to make the journey there

and return, after reflection by a mirror installed in Corsica. And it

should not wander on the way, for it must return exactly to the point of

departure.

Ever since, the activity of French geodesy has never slackened. We have

no more such astonishing adventures to tell; but the scientific work

accomplished is immense. The territory of France beyond the sea, like

that of the mother country, is covered by triangles measured with

precision.

We have become more and more exacting and what our fathers admired does

not satisfy us to-day. But in proportion as we seek more exactitude, the

difficulties greatly increase; we are surrounded by snares and must be

on our guard against a thousand unsuspected causes of error. It is

needful, therefore, to create instruments more and more faultless.

Here again France has not let herself be distanced. Our appliances for

the measurement of bases and angles leave nothing to desire, and, I may

also mention the pendulum of Colonel Defforges, which enables us to

determine gravity with a precision hitherto unknown.

The future of French geodesy is at present in the hands of the

Geographic Service of the army, successively directed by General Bassot

and General Berthaut. We can not sufficiently congratulate ourselves

upon it. For success in geodesy, scientific aptitudes are not enough; it

is necessary to be capable of standing long fatigues in all sorts of

climates; the chief must be able to win obedience from his collaborators

and to make obedient his native auxiliaries. These are military

qualities. Besides, one knows that, in our army, science has always

marched shoulder to shoulder with courage.

I add that a military organization assures the indispensable unity of

action. It would be more difficult to reconcile the rival pretensions of

scientists jealous of their independence, solicitous of what they call

their fame, and who yet must work in concert, though separated by great

distances. Among the geodesists of former times there were often

discussions, of which some aroused long echoes. The Academy long

resounded with the quarrel of Bouguer and La Condamine. I do not mean to

say that soldiers are exempt from passion, but discipline imposes

silence upon a too sensitive self-esteem.

Several foreign governments have called upon our officers to organize

their geodesic service: this is proof that the scientific influence of

France abroad has not declined.

Our hydrographic engineers contribute also to the common achievement a

glorious contingent. The survey of our coasts, of our colonies, the

study of the tides, offer them a vast domain of research. Finally I may

mention the general leveling of France which is carried out by the

ingenious and precise methods of M. Lallemand.

With such men we are sure of the future. Moreover, work for them will

not be lacking; our colonial empire opens for them immense expanses illy

explored. That is not all: the International Geodetic Association has

recognized the necessity of a new measurement of the arc of Quito,

determined in days of yore by La Condamine. It is France that has been

charged with this operation; she had every right to it, since our

ancestors had made, so to speak, the scientific conquest of the

Cordilleras. Besides, these rights have not been contested and our

government has undertaken to exercise them.

Captains Maurain and Lacombe completed a first reconnaissance, and the

rapidity with which they accomplished their mission, crossing the

roughest regions and climbing the most precipitous summits, is worthy of

all praise. It won the admiration of General Alfaro, President of the

Republic of Ecuador, who called them 'los hombres de hierro,' the men of

iron.

The final commission then set out under the command of

Lieutenant-Colonel (then Major) Bourgeois. The results obtained have

justified the hopes entertained. But our officers have encountered

unforeseen difficulties due to the climate. More than once, one of them

has been forced to remain several months at an altitude of 4,000 meters,

in the clouds and the snow, without seeing anything of the signals he

had to aim at and which refused to unmask themselves. But thanks to

their perseverance and courage, there resulted from this only a delay

and an increase of expense, without the exactitude of the measurements

suffering therefrom.

GENERAL CONCLUSIONS

What I have sought to explain in the preceding pages is how the

scientist should guide himself in choosing among the innumerable facts

offered to his curiosity, since indeed the natural limitations of his

mind compel him to make a choice, even though a choice be always a

sacrifice. I have expounded it first by general considerations,

recalling on the one hand the nature of the problem to be solved and on

the other hand seeking to better comprehend that of the human mind,

which is the principal instrument of the solution. I then have explained

it by examples; I have not multiplied them indefinitely; I also have had

to make a choice, and I have chosen naturally the questions I had

studied most. Others would doubtless have made a different choice; but

what difference, because I believe they would have reached the same

conclusions.

There is a hierarchy of facts; some have no reach; they teach us nothing

but themselves. The scientist who has ascertained them has learned

nothing but a fact, and has not become more capable of foreseeing new

facts. Such facts, it seems, come once, but are not destined to

reappear.

There are, on the other hand, facts of great yield; each of them teaches

us a new law. And since a choice must be made, it is to these that the

scientist should devote himself.

Doubtless this classification is relative and depends upon the weakness

of our mind. The facts of slight outcome are the complex facts, upon

which various circumstances may exercise a sensible influence,

circumstances too numerous and too diverse for us to discern them all.

But I should rather say that these are the facts we think complex, since

the intricacy of these circumstances surpasses the range of our mind.

Doubtless a mind vaster and finer than ours would think differently of

them. But what matter; we can not use that superior mind, but only our

own.

The facts of great outcome are those we think simple; may be they really

are so, because they are influenced only by a small number of

well-defined circumstances, may be they take on an appearance of

simplicity because the various circumstances upon which they depend obey

the laws of chance and so come to mutually compensate. And this is what

happens most often. And so we have been obliged to examine somewhat more

closely what chance is.

Facts where the laws of chance apply become easy of access to the

scientist who would be discouraged before the extraordinary complication

of the problems where these laws are not applicable. We have seen that

these considerations apply not only to the physical sciences, but to the

mathematical sciences. The method of demonstration is not the same for

the physicist and the mathematician. But the methods of invention are

very much alike. In both cases they consist in passing up from the fact

to the law, and in finding the facts capable of leading to a law.

To bring out this point, I have shown the mind of the mathematician at

work, and under three forms: the mind of the mathematical inventor and

creator; that of the unconscious geometer who among our far distant

ancestors, or in the misty years of our infancy, has constructed for us

our instinctive notion of space; that of the adolescent to whom the

teachers of secondary education unveil the first principles of the

science, seeking to give understanding of the fundamental definitions.

Everywhere we have seen the rôle of intuition and of the spirit of

generalization without which these three stages of mathematicians, if I

may so express myself, would be reduced to an equal impotence.

And in the demonstration itself, the logic is not all; the true

mathematical reasoning is a veritable induction, different in many

regards from the induction of physics, but proceeding like it from the

particular to the general. All the efforts that have been made to

reverse this order and to carry back mathematical induction to the rules

of logic have eventuated only in failures, illy concealed by the

employment of a language inaccessible to the uninitiated. The examples I

have taken from the physical sciences have shown us very different cases

of facts of great outcome. An experiment of Kaufmann on radium rays

revolutionizes at the same time mechanics, optics and astronomy. Why?

Because in proportion as these sciences have developed, we have the

better recognized the bonds uniting them, and then we have perceived a

species of general design of the chart of universal science. There are

facts common to several sciences, which seem the common source of

streams diverging in all directions and which are comparable to that

knoll of Saint Gothard whence spring waters which fertilize four

different valleys.

And then we can make choice of facts with more discernment than our

predecessors who regarded these valleys as distinct and separated by

impassable barriers.

It is always simple facts which must be chosen, but among these simple

facts we must prefer those which are situated upon these sorts of knolls

of Saint Gothard of which I have just spoken.

And when sciences have no direct bond, they still mutually throw light

upon one another by analogy. When we studied the laws obeyed by gases we

knew we had attacked a fact of great outcome; and yet this outcome was

still estimated beneath its value, since gases are, from a certain point

of view, the image of the milky way, and those facts which seemed of

interest only for the physicist, ere long opened new vistas to astronomy

quite unexpected.

And finally when the geodesist sees it is necessary to move his

telescope some seconds to see a signal he has set up with great pains,

this is a very small fact; but this is a fact of great outcome, not only

because this reveals to him the existence of a small protuberance upon

the terrestrial globe, that little hump would be by itself of no great

interest, but because this protuberance gives him information about the

distribution of matter in the interior of the globe, and through that

about the past of our planet, about its future, about the laws of its

development.

* * * * *

INDEX

aberration of light, 315, 496

Abraham, 311, 490-1, 505-7, 509, 515-6

absolute motion, 107

orientation, 83

space, 85, 93, 246, 257, 353

acceleration, 94, 98, 486, 509

accidental constant, 112

errors, 171, 402

accommodation of the eyes, 67-8

action at a distance, 137

addition, 34

aim of mathematics, 280

alchemists, 11

Alfaro, 543

algebra, 379

analogy, 220

analysis, 218-9, 279

analysis situs, 53, 239, 381

analyst, 210, 221

ancestral experience, 91

Andrade, 93, 104, 228

Andrews, 153

angle sum of triangle, 58

Anglo-Saxons, 3

antinomies, 449, 457, 477

Arago, 540-1

Aristotle, 205, 292, 460

arithmetic, 34, 379, 441, 463

associativity, 35

assumptions, 451, 453

astronomy, 81, 289, 315, 512

Atwood, 446

axiom, 60, 63, 65, 215

Bacon, 128

Bartholi, 503

Bassot, 542

beauty, 349, 368

Becquerel, 312

Beltrami, 56, 58

Bergson, 321

Berkeley, 4

Berthaut, 542

Bertrand, 156, 190, 211, 395

Betti, 239

Biot, 540

bodies, solid, 72

Boltzmann, 304

Bolyai, 56, 201, 203

Borel, 482

Bouguer, 537, 542

Bourgeois, 543

Boutroux, 390, 464

Bradley, 496

Briot, 298

Brownian movement, 152, 410

Bucherer, 507

Burali-Forti, 457-9, 477, 481-2

Caen, 387-8

Calinon, 228

canal rays, 491-2

canals, semicircular, 276

Cantor, 11, 448-9, 457, 459, 477

Cantorism, 381, 382, 480, 484

capillarity, 298

Carlyle, 128

Carnot's principle, 143, 151, 300, 303-5, 399

Cassini, 537

cathode rays, 487-92

cells, 217

center of gravity, 103

central forces, 297

Chaldeans, 290

chance, 395, 408

change of position, 70

state, 70

chemistry of the stars, 295

circle-squarers, 11

Clairaut, 537-8

Clausius, 119, 123, 143

color sensation, 252

Columbus, 228

commutativity, 35-6

compensation, 72

complete induction, 40

Comte, 294

Condorcet, 411

contingence, 340

continuity, 173

continuum, 43

amorphous, 238

mathematical, 46

physical, 46, 240

tridimensional, 240

convention, 50, 93, 106, 125, 173, 208, 317, 440, 451

convergence, 67-8

coordinates, 244

Copernicus, 109, 291, 354

Coulomb, 143, 516

Couturat, 450, 453, 456, 460, 462-3, 467, 472-6

creation, mathematical, 383

creed, 1

Crémieu, 168-9, 490

crisis, 303

Crookes, 195, 488, 527-8

crude fact, 326, 330

Curie, 312-3, 318

current, 186

curvature, 58-9

curve, 213, 346

curves without tangents, 51

cut, 52, 256

cyclones, 353

d'Alembert, 538

Darwin, 518-9

De Cyon, 276, 427

Dedekind, 44-5

Defforges, 542

definitions, 430, 453

deformation, 73, 415

Delage, 277

Delambre, 539

Delbeuf, 414

Descartes, 127

determinism, 123, 340

dictionary, 59

didymium, 333

dilatation, 76

dimensions, 53, 68, 78, 241, 256, 426

direction, 69

Dirichlet, 213

dispersion, 141

displacement, 73, 77, 247, 256

distance, 59, 292

distributivity, 36

Du Bois-Reymond, 50

earth, rotation of, 326, 353

eclipse, 326

electricity, 174

electrified bodies, 117

electrodynamic attraction, 308

induction, 188

mass, 311

electrodynamics, 184, 282

electromagnetic theory of light, 301

electrons, 316, 492-4, 505-8, 510, 512-4

elephant, 217, 436

ellipse, 215

Emerson, 203

empiricism, 86, 271

Epimenides, 478-9

equation of Laplace, 283

Erdély, 203

errors, accidental, 171, 402

law of, 119

systematic, 171, 402

theory of, 402, 406

ether, 145, 351

ethics, 205

Euclid, 62, 86, 202-3, 213

Euclidean geometry, 65, 235-6, 337

Euclid's postulate, 83, 91, 124, 353, 443, 453, 468, 470-1

experience, 90-1

experiment, 127, 317, 336, 446

fact, crude, 326, 330

in the rough, 327

scientific, 326

facts, 362, 371

Fahrenheit, 238

Faraday, 150, 192

Faye, 536

Fechner, 46, 52

Fehr, 383

finite, 57

Fitzgerald, 415-6, 500-1, 505

Fizeau, 146, 149, 309, 498, 504

Flammarion, 400, 406-7

flattening of the earth, 353

force, 72, 98, 444

direction of, 445

-flow, 284

forces, central, 297

equivalence of, 445

magnitude of, 445

Foucault's pendulum, 85, 109, 353

four dimensions, 78

Fourier, 298-9

Fourier's problem, 317

series, 286

Franklin, 513-4

Fresnel, 132, 140, 153, 174, 176, 181, 351, 498

Fuchsian, 387-8

function, 213

continuous, 218, 288

Galileo, 97, 331, 353-4

gaseous pressure, 141

gases, theory of, 400, 405, 523

Gauss, 384-5, 406

Gay-Lussac, 157

generalize, 342

geodesy, 535

geometer, 83, 210, 438

geometric space, 66

geometry, 72, 81, 125, 207, 380, 428, 442, 467

Euclidean, 65, 93

fourth, 62

non-Euclidean, 55

projective, 201

qualitative, 238

rational, 5, 467

Riemann's, 57

spheric, 59

Gibbs, 304

Goldstein, 492

Gouy, 152, 305, 410

gravitation, 512

Greeks, 93, 368

Hadamard, 459

Halsted, 3, 203, 464, 467

Hamilton, 115

helium, 294

Helmholtz, 56, 115, 118, 141, 190, 196

Hercules, 449

Hermite, 211, 220, 222, 285

Herschel, 528

Hertz, 102, 145, 194-5, 427, 488, 498, 502, 504, 510

Hertzian oscillator, 309, 317

Hilbert, 5, 11, 203, 433, 450-1, 464-8, 471, 475-7, 484

Himstedt, 195

Hipparchus, 291

homogeneity, 74, 423

homogeneous, 67

hydrodynamics, 284

hyperbola, 215

hypotheses, 6, 15, 127, 133

hysteresis, 151

identity of spaces, 268

of two points, 259

illusions, optical, 202

incommensurable numbers, 44

induction, complete, 40, 452-3, 467-8

electromagnetic, 188

mathematical, 40, 220

principle of, 481

inertia, 93, 486, 489, 507

infinite, 448

infinitesimals, 50

inquisitor, 331

integration, 139

interpolation, 131

intuition, 210, 213, 215

invariant, 333

Ionians, 127

ions, 152

irrational number, 44

irreversible phenomena, 151

isotropic, 67

Japanese mice, 277, 427

Jevons, 451

John Lackland, 128

Jules Verne, 111, 536

Jupiter, 131, 157, 231, 289

Kant, 16, 64, 202-3, 450-1, 471

Kauffman, 311, 490-1, 495, 506-7, 522, 545

Kazan, 203

Kelvin, 145, 523-4, 526-7

Kepler, 120, 133, 153, 282, 291-2

Kepler's laws, 136, 516

kinematics, 337

kinetic energy, 116

theory of gases, 141

Kirchhoff, 98-9, 103-5

Klein, 60, 211, 287

knowledge, 201

König, 144, 477

Kovalevski, 212, 286

Kronecker, 44

Lacombe, 543

La Condamine, 535, 537-8, 542-3

Lagrange, 98, 151, 179

Laisant, 383

Lallamand, 543

Langevin, 509

Laplace, 298, 398, 514-5, 518, 522, 538

Laplace's equation, 283, 287

Larmor, 145, 150

Lavoisier's principle, 301, 310, 312

law, 207, 291, 395

Leibnitz, 32, 450, 471

Le Roy, 28, 321-6, 332, 335, 337, 347-8, 354, 468

Lesage, 517-21

Liard, 440

Lie, 62-3, 212

light sensations, 252

theory of, 351

velocity of, 232, 312

Lindemann, 508

line, 203, 243

linkages, 144

Lippmann, 196

Lobachevski, 29, 56, 60, 62, 83, 86, 203

Lobachevski's space, 239

local time, 306-7, 499

logic, 214, 435, 448, 460-2, 464

logistic, 457, 472-4

logisticians, 472

Lorentz, 147, 149, 196-7, 306, 308, 311, 315, 415-6, 492, 498-502,

504-9, 512, 514-6, 521

Lotze, 264

luck, 399

Lumen, 407-8

MacCullagh, 150

Mach, 375

Mach-Delage, 276

magnetism, 149

magnitude, 49

Mariotte's law, 120, 132, 157, 342, 524

Maros, 203

mass, 98, 312, 446, 486, 489, 494, 515

mathematical analysis, 218

continuum, 46

creation, 383

induction, 40, 220

physics, 136, 297, 319

mathematics, 369, 448

matter, 492

Maupertuis, 535, 537-8

Maurain, 543

Maxwell, 140, 152, 175, 177, 181, 193, 282-3, 298, 301, 304-5, 351,

503, 524-5

Maxwell-Bartholi, 309, 503-4, 519, 521

Mayer, 119, 123, 300, 312, 318

measurement, 49

Méchain, 539-40

mechanical explanation, 177

mass, 312

mechanics, 92, 444, 486, 496, 512

anthropomorphic, 103

celestial, 279

statistical, 304

Méray, 211

metaphysician, 221

meteorology, 398

mice, 277

Michelson, 306, 309, 311, 316, 498, 500-1

milky way, 523-30

Mill, Stuart, 60-1, 453-4

Monist, 4, 89, 464

moons of Jupiter, 233

Morley, 309

motion of liquids, 283

of moon, 28

of planets, 341

relative, 107, 487

without deformation, 236

multiplication, 36

muscular sensations, 69

Nagaoka, 317

nature, 127

navigation, 289

neodymium, 333

neomonics, 283

Neumann, 181

Newton, 85, 96, 98, 109, 153, 291, 370, 486, 516, 536, 538

Newton's argument, 108, 334, 343

law, 111, 118, 132, 136, 149, 157, 233, 282, 292, 512, 514-5,

518, 525

principle, 146, 300, 308-9, 312

no-class theory, 478

nominalism, 28, 125, 321, 333, 335

non-Euclidean geometry, 55, 59, 388

language, 127

space, 55, 235, 237

straight, 236, 470

world, 75

number, 31

big, 88

imaginary, 283

incommensurable, 44

transfinite, 448-9

whole, 44, 469

objectivity, 209, 347, 349, 408

optical illusions, 202

optics, 174, 496

orbit of Saturn, 341

order, 385

orientation, 83

osmotic, 141

Padoa, 463

Panthéon, 414

parallax, 470

parallels, 56, 443

Paris time, 233

parry, 419-22, 427

partition, 45

pasigraphy, 456-7

Pasteur, 128

Peano, 450, 456-9, 463, 472

Pender, 490

pendulum, 224

Perrier, 541

Perrin, 195

phosphorus, 333, 468, 470-1

physical continuum, 46

physics, 127, 140, 144, 279, 297

physics of central forces, 297

of the principles, 299

Pieri, 11, 203

Plato, 292

Poincaré, 473

point, 89, 244

Poncelet, 215

postulates, 382

potential energy, 116

praseodymium, 333

principle, 125, 299

Carnot's, 143, 151, 300, 303-5, 399

Clausius', 119, 123, 143

Hamilton's, 115

Lavoisier's, 300, 310

Mayer's, 119, 121, 123, 300, 312, 318

Newton's, 146, 300, 308-9, 312

of action and reaction, 300, 487, 502

of conservation of energy, 300

of degradation of energy, 300

of inertia, 93, 486, 507

of least action, 118, 300

of relativity, 300, 305, 498, 505

Prony, 445

psychologist, 383

Ptolemy, 110, 291, 353-4

Pythagoras, 292

quadrature of the circle, 161

qualitative geometry, 238

space, 207

time, 224

quaternions, 282

radiometer, 503

radium, 312, 318, 486-7

Rados, 201

Ramsay, 313

rational geometry, 5, 467

reaction, 502

reality, 217, 340, 349

Réaumur, 238

recurrence, 37

Regnault, 170

relativity, 83, 305, 417, 423, 498, 505

Richard, 477-8, 480-1

Riemann, 56, 62, 145, 212, 239, 243, 381, 432

surface, 211, 287

Roemer, 233

Röntgen, 511, 520

rotation of earth, 225, 331, 353

roulette, 403

Rowland, 194-7, 305, 489

Royce, 202

Russell, 201, 450, 460-2, 464-7, 471-4, 477-82, 484-5

St. Louis exposition, 208, 320

Sarcey, 442

Saturn, 231, 317

Schiller, 202

Schliemann, 19

science, 205, 321, 323, 340, 354

Science and Hypothesis, 205-7, 220, 240, 246-7, 319, 353, 452

semicircular canals, 276

series, development in, 287

Fourier's, 286

Sirius, 226, 229

solid bodies, 72

space, 55, 66, 89, 235, 256

absolute, 85, 93

amorphous, 417

Bolyai, 56

Euclidean, 65

geometric, 66

Lobachevski's, 239

motor, 69

non-Euclidean, 55, 235, 237

of four dimensions, 78

perceptual, 66, 69

tactile, 68, 264

visual, 67, 252

spectra, 316

spectroscope, 294

Spencer, 9

sponge, 219

Stallo, 10

stars, 292

statistical mechanics, 304

straight, 62, 82, 236, 433, 450, 470

Stratonoff, 531

surfaces, 58

systematic errors, 171

tactile space, 68, 264

Tait, 98

tangent, 51

Tannery, 43

teaching, 430, 437

thermodynamics, 115, 119

Thomson, 98, 488

thread, 104

time, 223

equality, 225

local, 306, 307

measure of, 223-4

Tisserand, 515-6

Tolstoi, 354, 362, 368

Tommasina, 519

Transylvania, 203

triangle, 58

angle sum of, 58

truth, 205

Tycho Brahe, 133, 153, 228

unity of nature, 130

universal invariant, 333

Uriel, 203

van der Waals, 153

Vauban, 210

Veblen, 203

velocity of light, 232, 312

Venus of Milo, 201

verification, 33

Virchow, 21

visual impressions, 252

space, 67, 252

Volga, 203

Voltaire, 537-8

Weber, 117, 515-6

Weierstrass, 11, 212, 432

Whitehead, 472, 481-2

whole numbers, 44

Wiechert, 145, 488

x-rays, 152, 511, 520

Zeeman effect, 152, 196, 317, 494

Zeno, 382

Zermelo, 477, 482-3

zigzag theory, 478

zodiac, 398, 404

* * * * *

Transcriber's Note: The Greek alphabets are represented within square

brackets. For example, [alpha] stands for first Greek alphabet alpha.

Square root of a number is represented using the symbol (sqrt). That

is to say, sqrt(25) stands for square root of 25. The superscript is

shown with carat (^) symbol, example, 10^{5} stands for 5th power of

10. Similarly, subscript is represented by underscore (_) symbol. For

instance, n_{3} stands for letter n with subscript 3.

The Foundations of Science: Science and Hypothesis, The Value of Science, Science and Method · 第 12 / 12 章