Chapter VIII.

Of The Four Methods Of Experimental Inquiry.

§ 1. The simplest and most obvious modes of singling out from among the

circumstances which precede or follow a phenomenon, those with which it is

really connected by an invariable law, are two in number. One is, by

comparing together different instances in which the phenomenon occurs. The

other is, by comparing instances in which the phenomenon does occur, with

instances in other respects similar in which it does not. These two

methods may be respectively denominated, the Method of Agreement, and the

Method of Difference.

In illustrating these methods, it will be necessary to bear in mind the

twofold character of inquiries into the laws of phenomena; which may be

either inquiries into the cause of a given effect, or into the effects or

properties of a given cause. We shall consider the methods in their

application to either order of investigation, and shall draw our examples

equally from both.

We shall denote antecedents by the large letters of the alphabet, and the

consequents corresponding to them by the small. Let A, then, be an agent

or cause, and let the object of our inquiry be to ascertain what are the

effects of this cause. If we can either find, or produce, the agent A in

such varieties of circumstances that the different cases have no

circumstance in common except A; then whatever effect we find to be

produced in all our trials, is indicated as the effect of A. Suppose, for

example, that A is tried along with B and C, and that the effect is _a b

c_; and suppose that A is next tried with D and E, but without B and C,

and that the effect is _a d e_. Then we may reason thus: _b_ and _c_ are

not effects of A, for they were not produced by it in the second

experiment; nor are _d_ and _e_, for they were not produced in the first.

Whatever is really the effect of A must have been produced in both

instances; now this condition is fulfilled by no circumstance except _a_.

The phenomenon _a_ can not have been the effect of B or C, since it was

produced where they were not; nor of D or E, since it was produced where

they were not. Therefore it is the effect of A.

For example, let the antecedent A be the contact of an alkaline substance

and an oil. This combination being tried under several varieties of

circumstances, resembling each other in nothing else, the results agree in

the production of a greasy and detersive or saponaceous substance: it is

therefore concluded that the combination of an oil and an alkali causes

the production of a soap. It is thus we inquire, by the Method of

Agreement, into the effect of a given cause.

In a similar manner we may inquire into the cause of a given effect. Let

_a_ be the effect. Here, as shown in the last chapter, we have only the

resource of observation without experiment: we can not take a phenomenon

of which we know not the origin, and try to find its mode of production by

producing it: if we succeeded in such a random trial it could only be by

accident. But if we can observe a in two different combinations, _a b c_

and _a d e_; and if we know, or can discover, that the antecedent

circumstances in these cases respectively were A B C and A D E, we may

conclude by a reasoning similar to that in the preceding example, that A

is the antecedent connected with the consequent _a_ by a law of causation.

B and C, we may say, can not be causes of _a_, since on its second

occurrence they were not present; nor are D and E, for they were not

present on its first occurrence. A, alone of the five circumstances, was

found among the antecedents of _a_ in both instances.

For example, let the effect _a_ be crystallization. We compare instances

in which bodies are known to assume crystalline structure, but which have

no other point of agreement; and we find them to have one, and as far as

we can observe, only one, antecedent in common: the deposition of a solid

matter from a liquid state, either a state of fusion or of solution. We

conclude, therefore, that the solidification of a substance from a liquid

state is an invariable antecedent of its crystallization.

In this example we may go further, and say, it is not only the invariable

antecedent but the cause; or at least the proximate event which completes

the cause. For in this case we are able, after detecting the antecedent A,

to produce it artificially, and by finding that _a_ follows it, verify the

result of our induction. The importance of thus reversing the proof was

strikingly manifested when, by keeping a phial of water charged with

siliceous particles undisturbed for years, a chemist (I believe Dr.

Wollaston) succeeded in obtaining crystals of quartz; and in the equally

interesting experiment in which Sir James Hall produced artificial marble

by the cooling of its materials from fusion under immense pressure: two

admirable examples of the light which may be thrown upon the most secret

processes of Nature by well-contrived interrogation of her.

But if we can not artificially produce the phenomenon A, the conclusion

that it is the cause of _a_ remains subject to very considerable doubt.

Though an invariable, it may not be the unconditional antecedent of _a_,

but may precede it as day precedes night or night day. This uncertainty

arises from the impossibility of assuring ourselves that A is the _only_

immediate antecedent common to both the instances. If we could be certain

of having ascertained all the invariable antecedents, we might be sure

that the unconditional invariable antecedent, or cause, must be found

somewhere among them. Unfortunately it is hardly ever possible to

ascertain all the antecedents, unless the phenomenon is one which we can

produce artificially. Even then, the difficulty is merely lightened, not

removed: men knew how to raise water in pumps long before they adverted to

what was really the operating circumstance in the means they employed,

namely, the pressure of the atmosphere on the open surface of the water.

It is, however, much easier to analyze completely a set of arrangements

made by ourselves, than the whole complex mass of the agencies which

nature happens to be exerting at the moment of the production of a given

phenomenon. We may overlook some of the material circumstances in an

experiment with an electrical machine; but we shall, at the worst, be

better acquainted with them than with those of a thunder-storm.

The mode of discovering and proving laws of nature, which we have now

examined, proceeds on the following axiom: Whatever circumstances can be

excluded, without prejudice to the phenomenon, or can be absent

notwithstanding its presence, is not connected with it in the way of

causation. The casual circumstances being thus eliminated, if only one

remains, that one is the cause which we are in search of: if more than

one, they either are, or contain among them, the cause; and so, _mutatis

mutandis_, of the effect. As this method proceeds by comparing different

instances to ascertain in what they agree, I have termed it the Method of

Agreement; and we may adopt as its regulating principal the following

canon:

FIRST CANON.

_If two or more instances of the phenomenon under investigation have only

one circumstance in common, the circumstance in which alone all the

instances agree, is the cause (or effect) of the given phenomenon._

Quitting for the present the Method of Agreement, to which we shall almost

immediately return, we proceed to a still more potent instrument of the

investigation of nature, the Method of Difference.

§ 2. In the Method of Agreement, we endeavored to obtain instances which

agreed in the given circumstance but differed in every other: in the

present method we require, on the contrary, two instances resembling one

another in every other respect, but differing in the presence or absence

of the phenomenon we wish to study. If our object be to discover the

effects of an agent A, we must procure A in some set of ascertained

circumstances, as A B C, and having noted the effects produced, compare

them with the effect of the remaining circumstances B C, when A is absent.

If the effect of A B C is _a b c_, and the effect of B C _b c_, it is

evident that the effect of A is _a_. So again, if we begin at the other

end, and desire to investigate the cause of an effect _a_, we must select

an instance, as _a b c_, in which the effect occurs, and in which the

antecedents were A B C, and we must look out for another instance in which

the remaining circumstances, _b c_, occur without _a_. If the antecedents,

in that instance, are B C, we know that the cause of _a_ must be A: either

A alone, or A in conjunction with some of the other circumstances present.

It is scarcely necessary to give examples of a logical process to which we

owe almost all the inductive conclusions we draw in daily life. When a man

is shot through the heart, it is by this method we know that it was the

gunshot which killed him: for he was in the fullness of life immediately

before, all circumstances being the same, except the wound.

The axioms implied in this method are evidently the following. Whatever

antecedent can not be excluded without preventing the phenomenon, is the

cause, or a condition, of that phenomenon: whatever consequent can be

excluded, with no other difference in the antecedents than the absence of

a particular one, is the effect of that one. Instead of comparing

different instances of a phenomenon, to discover in what they agree, this

method compares an instance of its occurrence with an instance of its

non-occurrence, to discover in what they differ. The canon which is the

regulating principle of the Method of Difference may be expressed as

follows:

SECOND CANON.

_If an instance in which the phenomenon under investigation occurs, and an

instance in which it does not occur, have every circumstance in common

save one, that one occurring only in the former; the circumstance in which

alone the two instances differ, is the effect, or the cause, or an

indispensable part of the cause, of the phenomenon._

§ 3. The two methods which we have now stated have many features of

resemblance, but there are also many distinctions between them. Both are

methods of _elimination_. This term (employed in the theory of equations

to denote the process by which one after another of the elements of a

question is excluded, and the solution made to depend on the relation

between the remaining elements only) is well suited to express the

operation, analogous to this, which has been understood since the time of

Bacon to be the foundation of experimental inquiry: namely, the successive

exclusion of the various circumstances which are found to accompany a

phenomenon in a given instance, in order to ascertain what are those among

them which can be absent consistently with the existence of the

phenomenon. The Method of Agreement stands on the ground that whatever can

be eliminated, is not connected with the phenomenon by any law. The Method

of Difference has for its foundation, that whatever can not be eliminated,

is connected with the phenomenon by a law.

Of these methods, that of Difference is more particularly a method of

artificial experiment; while that of Agreement is more especially the

resource employed where experimentation is impossible. A few reflections

will prove the fact, and point out the reason of it.

It is inherent in the peculiar character of the Method of Difference, that

the nature of the combinations which it requires is much more strictly

defined than in the Method of Agreement. The two instances which are to be

compared with one another must be exactly similar, in all circumstances

except the one which we are attempting to investigate: they must be in the

relation of A B C and B C, or of _a b c_ and _b c_. It is true that this

similarity of circumstances needs not extend to such as are already known

to be immaterial to the result. And in the case of most phenomena we learn

at once, from the commonest experience, that most of the co-existent

phenomena of the universe may be either present or absent without

affecting the given phenomenon; or, if present, are present indifferently

when the phenomenon does not happen and when it does. Still, even limiting

the identity which is required between the two instances, A B C and B C,

to such circumstances as are not already known to be indifferent, it is

very seldom that nature affords two instances, of which we can be assured

that they stand in this precise relation to one another. In the

spontaneous operations of nature there is generally such complication and

such obscurity, they are mostly either on so overwhelmingly large or on so

inaccessibly minute a scale, we are so ignorant of a great part of the

facts which really take place, and even those of which we are not ignorant

are so multitudinous, and therefore so seldom exactly alike in any two

cases, that a spontaneous experiment, of the kind required by the Method

of Difference, is commonly not to be found. When, on the contrary, we

obtain a phenomenon by an artificial experiment, a pair of instances such

as the method requires is obtained almost as a matter of course, provided

the process does not last a long time. A certain state of surrounding

circumstances existed before we commenced the experiment; this is B C. We

then introduce A; say, for instance, by merely bringing an object from

another part of the room, before there has been time for any change in the

other elements. It is, in short (as M. Comté observes), the very nature of

an experiment, to introduce into the pre-existing state of circumstances a

change perfectly definite. We choose a previous state of things with which

we are well acquainted, so that no unforeseen alteration in that state is

likely to pass unobserved; and into this we introduce, as rapidly as

possible, the phenomenon which we wish to study; so that in general we are

entitled to feel complete assurance that the pre-existing state, and the

state which we have produced, differ in nothing except the presence or

absence of that phenomenon. If a bird is taken from a cage, and instantly

plunged into carbonic acid gas, the experimentalist may be fully assured

(at all events after one or two repetitions) that no circumstance capable

of causing suffocation had supervened in the interim, except the change

from immersion in the atmosphere to immersion in carbonic acid gas. There

is one doubt, indeed, which may remain in some cases of this description;

the effect may have been produced not by the change, but by the means

employed to produce the change. The possibility, however, of this last

supposition generally admits of being conclusively tested by other

experiments. It thus appears that in the study of the various kinds of

phenomena which we can, by our voluntary agency, modify or control, we can

in general satisfy the requisitions of the Method of Difference; but that

by the spontaneous operations of nature those requisitions are seldom

fulfilled.

The reverse of this is the case with the Method of Agreement. We do not

here require instances of so special and determinate a kind. Any instances

whatever, in which nature presents us with a phenomenon, may be examined

for the purposes of this method; and if all such instances agree in any

thing, a conclusion of considerable value is already attained. We can

seldom, indeed, be sure that the one point of agreement is the only one;

but this ignorance does not, as in the Method of Difference, vitiate the

conclusion; the certainty of the result, as far as it goes, is not

affected. We have ascertained one invariable antecedent or consequent,

however many other invariable antecedents or consequents may still remain

unascertained. If A B C, A D E, A F G, are all equally followed by a, then

a is an invariable consequent of A. If _a b c_, _a d e_, _a f g_, all

number A among their antecedents, then A is connected as an antecedent, by

some invariable law, with _a_. But to determine whether this invariable

antecedent is a cause, or this invariable consequent an effect, we must be

able, in addition, to produce the one by means of the other; or, at least,

to obtain that which alone constitutes our assurance of having produced

any thing, namely, an instance in which the effect, _a_, has come into

existence, with no other change in the pre-existing circumstances than the

addition of A. And this, if we can do it, is an application of the Method

of Difference, not of the Method of Agreement.

It thus appears to be by the Method of Difference alone that we can ever,

in the way of direct experience, arrive with certainty at causes. The

Method of Agreement leads only to laws of phenomena (as some writers call

them, but improperly, since laws of causation are also laws of phenomena):

that is, to uniformities, which either are not laws of causation, or in

which the question of causation must for the present remain undecided. The

Method of Agreement is chiefly to be resorted to, as a means of suggesting

applications of the Method of Difference (as in the last example the

comparison of A B C, A D E, A F G, suggested that A was the antecedent on

which to try the experiment whether it could produce _a_); or as an

inferior resource, in case the Method of Difference is impracticable;

which, as we before showed, generally arises from the impossibility of

artificially producing the phenomena. And hence it is that the Method of

Agreement, though applicable in principle to either case, is more

emphatically the method of investigation on those subjects where

artificial experimentation is impossible; because on those it is,

generally, our only resource of a directly inductive nature; while, in the

phenomena which we can produce at pleasure, the Method of Difference

generally affords a more efficacious process, which will ascertain causes

as well as mere laws.

§ 4. There are, however, many cases in which, though our power of

producing the phenomenon is complete, the Method of Difference either can

not be made available at all, or not without a previous employment of the

Method of Agreement. This occurs when the agency by which we can produce

the phenomenon is not that of one single antecedent, but a combination of

antecedents, which we have no power of separating from each other, and

exhibiting apart. For instance, suppose the subject of inquiry to be the

cause of the double refraction of light. We can produce this phenomenon at

pleasure, by employing any one of the many substances which are known to

refract light in that peculiar manner. But if, taking one of those

substances, as Iceland spar, for example, we wish to determine on which of

the properties of Iceland spar this remarkable phenomenon depends, we can

make no use, for that purpose, of the Method of Difference; for we can not

find another substance precisely resembling Iceland spar except in some

one property. The only mode, therefore, of prosecuting this inquiry is

that afforded by the Method of Agreement; by which, in fact, through a

comparison of all the known substances which have the property of doubly

refracting light, it was ascertained that they agree in the circumstance

of being crystalline substances; and though the converse does not hold,

though all crystalline substances have not the property of double

refraction, it was concluded, with reason, that there is a real connection

between these two properties; that either crystalline structure, or the

cause which gives rise to that structure, is one of the conditions of

double refraction.

Out of this employment of the Method of Agreement arises a peculiar

modification of that method, which is sometimes of great avail in the

investigation of nature. In cases similar to the above, in which it is not

possible to obtain the precise pair of instances which our second canon

requires—instances agreeing in every antecedent except A, or in every

consequent except _a_, we may yet be able, by a double employment of the

Method of Agreement, to discover in what the instances which contain A or

_a_ differ from those which do not.

If we compare various instances in which _a_ occurs, and find that they

all have in common the circumstance A, and (as far as can be observed) no

other circumstance, the Method of Agreement, so far, bears testimony to a

connection between A and _a_. In order to convert this evidence of

connection into proof of causation by the direct Method of Difference, we

ought to be able, in some one of these instances, as for example, A B C,

to leave out A, and observe whether by doing so, _a_ is prevented. Now

supposing (what is often the case) that we are not able to try this

decisive experiment; yet, provided we can by any means discover what would

be its result if we could try it, the advantage will be the same. Suppose,

then, that as we previously examined a variety of instances in which _a_

occurred, and found them to agree in containing A, so we now observe a

variety of instances in which _a_ does not occur, and find them agree in

not containing A; which establishes, by the Method of Agreement, the same

connection between the absence of A and the absence of _a_, which was

before established between their presence. As, then, it had been shown

that whenever A is present _a_ is present, so, it being now shown that

when A is taken away a is removed along with it, we have by the one

proposition A B C, _a b c_, by the other B C, _b c_, the positive and

negative instances which the Method of Difference requires.

This method may be called the Indirect Method of Difference, or the Joint

Method of Agreement and Difference; and consists in a double employment of

the Method of Agreement, each proof being independent of the other, and

corroborating it. But it is not equivalent to a proof by the direct Method

of Difference. For the requisitions of the Method of Difference are not

satisfied, unless we can be quite sure either that the instances

affirmative of _a_ agree in no antecedent whatever but A, or that the

instances negative of _a_ agree in nothing but the negation of A. Now, if

it were possible, which it never is, to have this assurance, we should not

need the joint method; for either of the two sets of instances separately

would then be sufficient to prove causation. This indirect method,

therefore, can only be regarded as a great extension and improvement of

the Method of Agreement, but not as participating in the more cogent

nature of the Method of Difference. The following may be stated as its

canon:

THIRD CANON.

_If two or more instances in which the phenomenon occurs have only one

circumstance in common, while two or more instances in which it does not

occur have nothing in common save the absence of that circumstance, the

circumstance in which alone the two sets of instances differ, is the

effect, or the cause, or an indispensable part of the cause, of the

phenomenon._

We shall presently see that the Joint Method of Agreement and Difference

constitutes, in another respect not yet adverted to, an improvement upon

the common Method of Agreement, namely, in being unaffected by a

characteristic imperfection of that method, the nature of which still

remains to be pointed out. But as we can not enter into this exposition

without introducing a new element of complexity into this long and

intricate discussion, I shall postpone it to a subsequent chapter, and

shall at once proceed to a statement of two other methods, which will

complete the enumeration of the means which mankind possess for exploring

the laws of nature by specific observation and experience.

§ 5. The first of these has been aptly denominated the Method of Residues.

Its principle is very simple. Subducting from any given phenomenon all the

portions which, by virtue of preceding inductions, can be assigned to

known causes, the remainder will be the effect of the antecedents which

had been overlooked, or of which the effect was as yet an unknown

quantity.

Suppose, as before, that we have the antecedents A B C, followed by the

consequents _a b c_, and that by previous inductions (founded, we will

suppose, on the Method of Difference) we have ascertained the causes of

some of these effects, or the effects of some of these causes; and are

thence apprised that the effect of A is _a_, and that the effect of B is

_b_. Subtracting the sum of these effects from the total phenomenon, there

remains _c_, which now, without any fresh experiments, we may know to be

the effect of C. This Method of Residues is in truth a peculiar

modification of the Method of Difference. If the instance A B C, _a b c_,

could have been compared with a single instance A B, _a b_, we should have

proved C to be the cause of _c_, by the common process of the Method of

Difference. In the present case, however, instead of a single instance A

B, we have had to study separately the causes A and B, and to infer from

the effects which they produce separately what effect they must produce in

the case A B C, where they act together. Of the two instances, therefore,

which the Method of Difference requires—the one positive, the other

negative—the negative one, or that in which the given phenomenon is

absent, is not the direct result of observation and experiment, but has

been arrived at by deduction. As one of the forms of the Method of

Difference, the Method of Residues partakes of its rigorous certainty,

provided the previous inductions, those which gave the effects of A and B,

were obtained by the same infallible method, and provided we are certain

that C is the _only_ antecedent to which the residual phenomenon _c_ can

be referred; the only agent of which we had not already calculated and

subducted the effect. But as we can never be quite certain of this, the

evidence derived from the Method of Residues is not complete unless we can

obtain C artificially, and try it separately, or unless its agency, when

once suggested, can be accounted for, and proved deductively from known

laws.

Even with these reservations, the Method of Residues is one of the most

important among our instruments of discovery. Of all the methods of

investigating laws of nature, this is the most fertile in unexpected

results: often informing us of sequences in which neither the cause nor

the effect were sufficiently conspicuous to attract of themselves the

attention of observers. The agent C may be an obscure circumstance, not

likely to have been perceived unless sought for, nor likely to have been

sought for until attention had been awakened by the insufficiency of the

obvious causes to account for the whole of the effect. And _c_ may be so

disguised by its intermixture with _a_ and _b_, that it would scarcely

have presented itself spontaneously as a subject of separate study. Of

these uses of the method, we shall presently cite some remarkable

examples. The canon of the Method of Residues is as follows:

FOURTH CANON.

_Subduct from any phenomenon such part as is known by previous inductions

to be the effect of certain antecedents, and the residue of the phenomenon

is the effect of the remaining antecedents._

§ 6. There remains a class of laws which it is impracticable to ascertain

by any of the three methods which I have attempted to characterize:

namely, the laws of those Permanent Causes, or indestructible natural

agents, which it is impossible either to exclude or to isolate; which we

can neither hinder from being present, nor contrive that they shall be

present alone. It would appear at first sight that we could by no means

separate the effects of these agents from the effects of those other

phenomena with which they can not be prevented from co-existing. In

respect, indeed, to most of the permanent causes, no such difficulty

exists; since, though we can not eliminate them as co-existing facts, we

can eliminate them as influencing agents, by simply trying our experiment

in a local situation beyond the limits of their influence. The pendulum,

for example, has its oscillations disturbed by the vicinity of a mountain:

we remove the pendulum to a sufficient distance from the mountain, and the

disturbance ceases: from these data we can determine by the Method of

Difference, the amount of effect due to the mountain; and beyond a certain

distance every thing goes on precisely as it would do if the mountain

exercised no influence whatever, which, accordingly, we, with sufficient

reason, conclude to be the fact.

The difficulty, therefore, in applying the methods already treated of to

determine the effects of Permanent Causes, is confined to the cases in

which it is impossible for us to get out of the local limits of their

influence. The pendulum can be removed from the influence of the mountain,

but it can not be removed from the influence of the earth: we can not take

away the earth from the pendulum, nor the pendulum from the earth, to

ascertain whether it would continue to vibrate if the action which the

earth exerts upon it were withdrawn. On what evidence, then, do we ascribe

its vibrations to the earth’s influence? Not on any sanctioned by the

Method of Difference; for one of the two instances, the negative instance,

is wanting. Nor by the Method of Agreement; for though all pendulums agree

in this, that during their oscillations the earth is always present, why

may we not as well ascribe the phenomenon to the sun, which is equally a

co-existent fact in all the experiments? It is evident that to establish

even so simple a fact of causation as this, there was required some method

over and above those which we have yet examined.

As another example, let us take the phenomenon Heat. Independently of all

hypothesis as to the real nature of the agency so called, this fact is

certain, that we are unable to exhaust any body of the whole of its heat.

It is equally certain that no one ever perceived heat not emanating from a

body. Being unable, then, to separate Body and Heat, we can not effect

such a variation of circumstances as the foregoing three methods require;

we can not ascertain, by those methods, what portion of the phenomena

exhibited by any body is due to the heat contained in it. If we could

observe a body with its heat, and the same body entirely divested of heat,

the Method of Difference would show the effect due to the heat, apart from

that due to the body. If we could observe heat under circumstances

agreeing in nothing but heat, and therefore not characterized also by the

presence of a body, we could ascertain the effects of heat, from an

instance of heat with a body and an instance of heat without a body, by

the Method of Agreement; or we could determine by the Method of Difference

what effect was due to the body, when the remainder which was due to the

heat would be given by the Method of Residues. But we can do none of these

things; and without them the application of any of the three methods to

the solution of this problem would be illusory. It would be idle, for

instance, to attempt to ascertain the effect of heat by subtracting from

the phenomena exhibited by a body all that is due to its other properties;

for as we have never been able to observe any bodies without a portion of

heat in them, effects due to that heat might form a part of the very

results which we were affecting to subtract, in order that the effect of

heat might be shown by the residue.

If, therefore, there were no other methods of experimental investigation

than these three, we should be unable to determine the effects due to heat

as a cause. But we have still a resource. Though we can not exclude an

antecedent altogether, we may be able to produce, or nature may produce

for us some modification in it. By a modification is here meant, a change

in it not amounting to its total removal. If some modification in the

antecedent A is always followed by a change in the consequent _a_, the

other consequents _b_ and _c_ remaining the same; or _vicè versa_, if

every change in _a_ is found to have been preceded by some modification in

A, none being observable in any of the other antecedents, we may safely

conclude that _a_ is, wholly or in part, an effect traceable to A, or at

least in some way connected with it through causation. For example, in the

case of heat, though we can not expel it altogether from any body, we can

modify it in quantity, we can increase or diminish it; and doing so, we

find by the various methods of experimentation or observation already

treated of, that such increase or diminution of heat is followed by

expansion or contraction of the body. In this manner we arrive at the

conclusion, otherwise unattainable by us, that one of the effects of heat

is to enlarge the dimensions of bodies; or, what is the same thing in

other words, to widen the distances between their particles.

A change in a thing, not amounting to its total removal, that is, a change

which leaves it still the same thing it was, must be a change either in

its quantity, or in some of its variable relations to other things, of

which variable relations the principal is its position in space. In the

previous example, the modification which was produced in the antecedent

was an alteration in its quantity. Let us now suppose the question to be,

what influence the moon exerts on the surface of the earth. We can not try

an experiment in the absence of the moon, so as to observe what

terrestrial phenomena her annihilation would put an end to; but when we

find that all the variations in the _position_ of the moon are followed by

corresponding variations in the time and place of high water, the place

being always either the part of the earth which is nearest to, or that

which is most remote from, the moon, we have ample evidence that the moon

is, wholly or partially, the cause which determines the tides. It very

commonly happens, as it does in this instance, that the variations of an

effect are correspondent, or analogous, to those of its cause; as the moon

moves farther toward the east, the high-water point does the same: but

this is not an indispensable condition, as may be seen in the same

example, for along with that high-water point there is at the same instant

another high-water point diametrically opposite to it, and which,

therefore, of necessity, moves toward the west, as the moon, followed by

the nearer of the tide waves, advances toward the east: and yet both these

motions are equally effects of the moon’s motion.

That the oscillations of the pendulum are caused by the earth, is proved

by similar evidence. Those oscillations take place between equidistant

points on the two sides of a line, which, being perpendicular to the

earth, varies with every variation in the earth’s position, either in

space or relatively to the object. Speaking accurately, we only know by

the method now characterized, that all terrestrial bodies tend to the

earth, and not to some unknown fixed point lying in the same direction. In

every twenty-four hours, by the earth’s rotation, the line drawn from the

body at right angles to the earth coincides successively with all the

radii of a circle, and in the course of six months the place of that

circle varies by nearly two hundred millions of miles; yet in all these

changes of the earth’s position, the line in which bodies tend to fall

continues to be directed toward it: which proves that terrestrial gravity

is directed to the earth, and not, as was once fancied by some, to a fixed

point of space.

The method by which these results were obtained may be termed the Method

of Concomitant Variations; it is regulated by the following canon:

FIFTH CANON.

_Whatever phenomenon varies in any manner whenever another phenomenon

varies in some particular manner, is either a cause or an effect of that

phenomenon, or is connected with it through some fact of causation._

The last clause is subjoined, because it by no means follows when two

phenomena accompany each other in their variations, that the one is cause

and the other effect. The same thing may, and indeed must happen,

supposing them to be two different effects of a common cause: and by this

method alone it would never be possible to ascertain which of the

suppositions is the true one. The only way to solve the doubt would be

that which we have so often adverted to, viz., by endeavoring to ascertain

whether we can produce the one set of variations by means of the other. In

the case of heat, for example, by increasing the temperature of a body we

increase its bulk, but by increasing its bulk we do not increase its

temperature; on the contrary (as in the rarefaction of air under the

receiver of an air-pump), we generally diminish it: therefore heat is not

an effect, but a cause, of increase of bulk. If we can not ourselves

produce the variations, we must endeavor, though it is an attempt which is

seldom successful, to find them produced by nature in some case in which

the preexisting circumstances are perfectly known to us.

It is scarcely necessary to say, that in order to ascertain the uniform

concomitance of variations in the effect with variations in the cause, the

same precautions must be used as in any other case of the determination of

an invariable sequence. We must endeavor to retain all the other

antecedents unchanged, while that particular one is subjected to the

requisite series of variations; or, in other words, that we may be

warranted in inferring causation from concomitance of variations, the

concomitance itself must be proved by the Method of Difference.

It might at first appear that the Method of Concomitant Variations assumes

a new axiom, or law of causation in general, namely, that every

modification of the cause is followed by a change in the effect. And it

does usually happen that when a phenomenon A causes a phenomenon _a_, any

variation in the quantity or in the various relations of A, is uniformly

followed by a variation in the quantity or relations of _a_. To take a

familiar instance, that of gravitation. The sun causes a certain tendency

to motion in the earth; here we have cause and effect; but that tendency

is _toward_ the sun, and therefore varies in direction as the sun varies

in the relation of position; and, moreover, the tendency varies in

intensity, in a certain numerical correspondence to the sun’s distance

from the earth, that is, according to another relation of the sun. Thus we

see that there is not only an invariable connection between the sun and

the earth’s gravitation, but that two of the relations of the sun, its

position with respect to the earth and its distance from the earth, are

invariably connected as antecedents with the quantity and direction of the

earth’s gravitation. The cause of the earth’s gravitating at all, is

simply the sun; but the cause of its gravitating with a given intensity

and in a given direction, is the existence of the sun in a given direction

and at a given distance. It is not strange that a modified cause, which is

in truth a different cause, should produce a different effect.

Although it is for the most part true that a modification of the cause is

followed by a modification of the effect, the Method of Concomitant

Variations does not, however, presuppose this as an axiom. It only

requires the converse proposition: that any thing on whose modifications,

modifications of an effect are invariably consequent, must be the cause

(or connected with the cause) of that effect; a proposition, the truth of

which is evident; for if the thing itself had no influence on the effect,

neither could the modifications of the thing have any influence. If the

stars have no power over the fortunes of mankind, it is implied in the

very terms that the conjunctions or oppositions of different stars can

have no such power.

Although the most striking applications of the Method of Concomitant

Variations take place in the cases in which the Method of Difference,

strictly so called, is impossible, its use is not confined to those cases;

it may often usefully follow after the Method of Difference, to give

additional precision to a solution which that has found. When by the

Method of Difference it has first been ascertained that a certain object

produces a certain effect, the Method of Concomitant Variations may be

usefully called in, to determine according to what law the quantity or the

different relations of the effect follow those of the cause.

§ 7. The case in which this method admits of the most extensive

employment, is that in which the variations of the cause are variations of

quantity. Of such variations we may in general affirm with safety, that

they will be attended not only with variations, but with similar

variations, of the effect: the proposition that more of the cause is

followed by more of the effect, being a corollary from the principle of

the Composition of Causes, which, as we have seen, is the general rule of

causation; cases of the opposite description, in which causes change their

properties on being conjoined with one another, being, on the contrary,

special and exceptional. Suppose, then, that when A changes in quantity,

_a_ also changes in quantity, and in such a manner that we can trace the

numerical relation which the changes of the one bear to such changes of

the other as take place within our limits of observation. We may then,

with certain precautions, safely conclude that the same numerical relation

will hold beyond those limits. If, for instance, we find that when A is

double, _a_ is double; that when A is treble or quadruple, _a_ is treble

or quadruple; we may conclude that if A were a half or a third, _a_ would

be a half or a third, and finally, that if A were annihilated, _a_ would

be annihilated; and that _a_ is wholly the effect of A, or wholly the

effect of the same cause with A. And so with any other numerical relation

according to which A and _a_ would vanish simultaneously; as, for

instance, if _a_ were proportional to the square of A. If, on the other

hand, _a_ is not wholly the effect of A, but yet varies when A varies, it

is probably a mathematical function not of A alone, but of A and something

else: its changes, for example, may be such as would occur if part of it

remained constant, or varied on some other principle, and the remainder

varied in some numerical relations to the variations of A. In that case,

when A diminishes, _a_ will be seen to approach not toward zero, but

toward some other limit; and when the series of variations is such as to

indicate what that limit is, if constant, or the law of its variation, if

variable, the limit will exactly measure how much of _a_ is the effect of

some other and independent cause, and the remainder will be the effect of

A (or of the cause of A).

These conclusions, however, must not be drawn without certain precautions.

In the first place, the possibility of drawing them at all, manifestly

supposes that we are acquainted not only with the variations, but with the

absolute quantities both of A and _a_. If we do not know the total

quantities, we can not, of course, determine the real numerical relation

according to which those quantities vary. It is, therefore, an error to

conclude, as some have concluded, that because increase of heat expands

bodies, that is, increases the distance between their particles, therefore

the distance is wholly the effect of heat, and that if we could entirely

exhaust the body of its heat, the particles would be in complete contact.

This is no more than a guess, and of the most hazardous sort, not a

legitimate induction: for since we neither know how much heat there is in

any body, nor what is the real distance between any two of its particles,

we can not judge whether the contraction of the distance does or does not

follow the diminution of the quantity of heat according to such a

numerical relation that the two quantities would vanish simultaneously.

In contrast with this, let us consider a case in which the absolute

quantities are known; the case contemplated in the first law of motion:

viz., that all bodies in motion continue to move in a straight line with

uniform velocity until acted upon by some new force. This assertion is in

open opposition to first appearances; all terrestrial objects, when in

motion, gradually abate their velocity, and at last stop; which

accordingly the ancients, with their _inductio per enumerationem

simplicem_, imagined to be the law. Every moving body, however, encounters

various obstacles, as friction, the resistance of the atmosphere, etc.,

which we know by daily experience to be causes capable of destroying

motion. It was suggested that the whole of the retardation might be owing

to these causes. How was this inquired into? If the obstacles could have

been entirely removed, the case would have been amenable to the Method of

Difference. They could not be removed, they could only be diminished, and

the case, therefore, admitted only of the Method of Concomitant

Variations. This accordingly being employed, it was found that every

diminution of the obstacles diminished the retardation of the motion: and

inasmuch as in this case (unlike the case of heat) the total quantities

both of the antecedent and of the consequent were known, it was

practicable to estimate, with an approach to accuracy, both the amount of

the retardation and the amount of the retarding causes, or resistances,

and to judge how near they both were to being exhausted; and it appeared

that the effect dwindled as rapidly, and at each step was as far on the

road toward annihilation, as the cause was. The simple oscillation of a

weight suspended from a fixed point, and moved a little out of the

perpendicular, which in ordinary circumstances lasts but a few minutes,

was prolonged in Borda’s experiments to more than thirty hours, by

diminishing as much as possible the friction at the point of suspension,

and by making the body oscillate in a space exhausted as nearly as

possible of its air. There could therefore be no hesitation in assigning

the whole of the retardation of motion to the influence of the obstacles;

and since, after subducting this retardation from the total phenomenon,

the remainder was a uniform velocity, the result was the proposition known

as the first law of motion.

There is also another characteristic uncertainty affecting the inference

that the law of variation which the quantities observe within our limits

of observation, will hold beyond those limits. There is, of course, in the

first instance, the possibility that beyond the limits, and in

circumstances therefore of which we have no direct experience, some

counteracting cause might develop itself; either a new agent or a new

property of the agents concerned, which lies dormant in the circumstances

we are able to observe. This is an element of uncertainty which enters

largely into all our predictions of effects; but it is not peculiarly

applicable to the Method of Concomitant Variations. The uncertainty,

however, of which I am about to speak, is characteristic of that method;

especially in the cases in which the extreme limits of our observation are

very narrow, in comparison with the possible variations in the quantities

of the phenomena. Any one who has the slightest acquaintance with

mathematics, is aware that very different laws of variation may produce

numerical results which differ but slightly from one another within narrow

limits; and it is often only when the absolute amounts of variation are

considerable, that the difference between the results given by one law and

by another becomes appreciable. When, therefore, such variations in the

quantity of the antecedents as we have the means of observing are small in

comparison with the total quantities, there is much danger lest we should

mistake the numerical law, and be led to miscalculate the variations which

would take place beyond the limits; a miscalculation which would vitiate

any conclusion respecting the dependence of the effect upon the cause,

that could be founded on those variations. Examples are not wanting of

such mistakes. “The formulæ,” says Sir John Herschel,(136) “which have

been empirically deduced for the elasticity of steam (till very recently),

and those for the resistance of fluids, and other similar subjects,” when

relied on beyond the limits of the observations from which they were

deduced, “have almost invariably failed to support the theoretical

structures which have been erected on them.”

In this uncertainty, the conclusion we may draw from the concomitant

variations of _a_ and A, to the existence of an invariable and exclusive

connection between them, or to the permanency of the same numerical

relation between their variations when the quantities are much greater or

smaller than those which we have had the means of observing, can not be

considered to rest on a complete induction. All that in such a case can be

regarded as proved on the subject of causation is, that there is some

connection between the two phenomena; that A, or something which can

influence A, must be _one_ of the causes which collectively determine _a_.

We may, however, feel assured that the relation which we have observed to

exist between the variations of A and _a_, will hold true in all cases

which fall between the same extreme limits; that is, wherever the utmost

increase or diminution in which the result has been found by observation

to coincide with the law, is not exceeded.

The four methods which it has now been attempted to describe, are the only

possible modes of experimental inquiry—of direct induction _a posteriori_,

as distinguished from deduction: at least, I know not, nor am able to

imagine any others. And even of these, the Method of Residues, as we have

seen, is not independent of deduction; though, as it also requires

specific experience, it may, without impropriety, be included among

methods of direct observation and experiment.

These, then, with such assistance as can be obtained from Deduction,

compose the available resources of the human mind for ascertaining the

laws of the succession of phenomena. Before proceeding to point out

certain circumstances by which the employment of these methods is

subjected to an immense increase of complication and of difficulty, it is

expedient to illustrate the use of the methods, by suitable examples drawn

from actual physical investigations. These, accordingly, will form the

subject of the succeeding chapter.

A System of Logic, Ratiocinative and Inductive · 第 8 / 33 章