EINSTEIN'S DEPARTURE

Since Einstein has cut loose from the ether, he lacks this canvas, and

therewith, at the first glance, also loses the possibility of fixing

the positions of the heavenly bodies and mathematically describing

their movement--i.e., by giving comparisons that define the positions

at every moment. How Einstein has overcome this difficulty may be

somewhat elucidated through a simple illustration.

On the surface of the earth the attraction of gravitation causes

all bodies to fall along vertical lines, and, indeed, when one omits

the resistance of the air, with an equally accelerated movement; the

velocity increases in equal degrees in equal consecutive divisions of

time at a rate that in this country gives the velocity attained at

the end of a second as 981 centimeters (32.2 feet) per second. The

number 981 defines the "acceleration in the field of gravitation,"

and this field is fully characterized by that single number; with its

help we can also calculate the movement of an object hurled out in an

arbitrary direction. In order to measure the acceleration we let the

body drop alongside of a vertical measure set solidly on the ground;

on this scale we read at every moment the figure that indicates the

height, the only co-ordinate that is of importance in this rectilinear

movement. Now we ask what would we be able to see if the measure were

not bound solidly to the earth, if it, let us suppose, moved down or

up with the place where it is located and where we are ourselves. If

in this case the speed were constant, then, and this is in accord with

the special theory of relativity, there would be no motion observed at

all; we should again find an acceleration of 981 for a falling body. It

would be different if the measure moved with changeable velocity.

If it went down with a constant acceleration of 981 itself, then an

object could remain permanently at the same point on the measure,

or could move up or down itself alongside of it, with constant

speed. The relative movement of the body with regard to the measure

should be without acceleration, and if we had to judge only by what

we observed in the spot where we were and which was falling itself,

then we should get the impression that there was no gravitation at

all. If the measure goes down with an acceleration equal to a half

or a third of what it just was, then the relative motion of the body

will, of course, be accelerated, but we should find the increase

in velocity per second one-half or two-thirds of 981. If, finally,

we let the measure rise with a uniformly accelerated movement, then

we shall find a greater acceleration than 981 for the body itself.

Thus we see that we, also when the measure is not attached to the

earth, disregarding its displacement, may describe the motion of the

body in respect to the measure always in the same way--i.e., as one

uniformly accelerated, as we ascribe now and again a fixed value to

the acceleration of the sphere of gravitation, in a particular case

the value of zero.

Of course, in the case here under consideration the use of a measure

fixed immovably upon the earth should merit all recommendation. But

in the spaces of the solar system we have, now that we have abandoned

the ether, no such support. We can no longer establish a system of

co-ordinates, like the one just mentioned, in a universal intermediate

matter, and if we were to arrive in one way or another at a definite

system of lines crossing each other in three directions, then we should

be able to use just as well another similar system that in respect to

the first moves this or that way. We should also be able to remodel the

system of co-ordinates in all kinds of ways, for example by extension

or compression. That in all these cases for fixed bodies that do not

participate in the movement or the remodelling of the system other

co-ordinates will be read off again and again is clear.

The Einstein Theory of Relativity: A Concise Statement · 第 8 / 11 题