On Einstein's Theory of gravitation
| On Einstein's Theory of gravitation I-IV (1916) by |
| Proceedings of the Royal Netherlands Academy of Arts and Sciences, 1917, 19 (2):1341-1361 Online, 20 (1):2-34 Online |
"On Einstein's Theory of gravitation." By Prof. H. A. Lorentz.
I.
(Communicated in the meeting of February 26, 1916).
§ 1. In pursuance of his important researches on gravitation Einstein has recently attained the aim which he had constantly kept in view; he has succeeded in establishing equations whose form is not changed by an arbitrarily chosen change of the system of coordinates[1]. Shortly afterwards, working out an idea that had been expressed already in one of Einstein's papers, Hilbert[2] has shown the use that may be made of a variation law that may be regarded as Hamilton's principle in a suitably generalized form. By these results the "general theory of relativity" may be said to have taken a definitive form, though much remains still to be done in further developing it and in applying it to special problems. It will also be desirable to present the fundamental ideas in a form as simple as possible.
In this communication it will be shown that a four-dimensional geometric representation may be of much use for this latter purpose; by means of it we shall be able to indicate for a system containing a number of material points and an electromagnetic field (or eventually only one of these) the quantity
, which occurs in the variation theorem, and which we may call the principal function. This quantity consists of three parts, of which the first relates to the material points, the second to the electromagnetic field and the third to the gravitation field itself.
As to the material points, it will be assumed that the only connexion between them is that which results from their mutual gravitational attraction.
§ 2. We shall be concerned with a four-dimensional extension
, in which "space" and "time" are combined, so that each point
in it indicates a definite place
and at the same time a definite moment of time
. If we say that
refers to a material point we mean that at the time
this point is found at the place
. In the course of time the material point is represented every moment by a new point
; all these points lie on the "world-line", which represents the state of motion (or eventually the state of rest) of the material point[3]. In the same sense we may speak of the world-line of a propagated light-vibration. An intersection of two world-lines means that the two objects to which they belong meet at a certain moment, that a "coincidence" takes place[4]. Now Einstein has made the striking remark[5] that the only thing we can learn from our observations and with which our theories are essentially concerned, is the existence of these coincidences. Let us suppose e.g. that we have observed an occultation of a star by the moon or rather the reappearance of a star at the moon's border. Then the world-line of a certain light-vibration starting from a point on the world-line of the star has in its further course intersected the world-line of a point of the border of the moon and finally that of the observer's eye. A similar remark may be made when the moment of reappearance is read on a clock. Let us suppose that the light-vibration itself lights the dial-plate, reaching it when the hand is at the point
; then we may say that three world-lines, viz. that of the light-vibration, that of the hand and that of the point
intersect.
§ 3. We may imagine that, in order to investigate a gravitation field as e.g. that of the sun, a great number of material points, moving in all directions and with different velocities, are thrown into it, that light-beams are also made to traverse the field and that all coincidences are noted[6]. It would be possible to represent the results of these observations by world-lines in a four-dimensional figure — let us say in a "field-figure" — the lines being drawn in such a way that each observed coincidence is represented by an intersection of two lines and that the points of intersection of one line with a number of the others succeed each other in the right order.
Now, as we have to attend only to the intersections, we have a great degree of liberty in the construction of the "field-figure". If, independently of each other, two persons were to describe the same observations, their figures would probably look quite different and if these figures were deformed in an arbitrary way, without break of continuity, they would not cease to serve the purpose.
After having constructed a field-figure
we may introduce "coordinates", by which we mean that to each point
we ascribe four numbers
, in such a way that along any line in the field-figure these numbers change continuously and that never two different points get the same four numbers. Having done this we may for each point
seek a point
in a four-dimensional extension
, in which the numbers
ascribed to
are the Cartesian coordinates of the point
. In this way we obtain in
a figure
, which just as well as
can serve as field-figure and which of course may be quite different according to the choice of the numbers
, that have been ascribed to the points of
.
If now it is true that the coincidences only are of importance it must be possible to express the fundamental laws of the phenomena by geometric considerations referring to the field-figure, in such a way that this mode of expression is the same for all possible field-figures; from our point of view all these figures can be considered as being the same. In such a geometric treatment the introduction of coordinates will be of secondary importance; with a single exception (§ 13) it only serves for short calculations which we have to intercalate (for the proof of certain geometric propositions) and for establishing the final equations, which have to be used for the solution of special problems. In the discussion of the general principles coordinates play no part; and it is thus seen that the formulation of these principles can take place in the same way whatever be our choice of coordinates. So we are sure beforehand of the general covariancy of the equations that was postulated by Einstein.
§ 4. Einstein ascribes to a line-element
in the field-figure a length
defined by the equation
![]() |
(1) |
Here
are the changes of the coordinates when we pass from
to
, while the coefficients
depend in one way or another on the coordinates. The gravitation field is known when these 10 quantities are given as functions of
. Here it must be remarked that in all real cases the coordinates can be chosen in such a way that for one point arbitrarily chosen (1) becomes

This requires that the determinant
of the coefficients of (1) be always negative. The minor of this determinant corresponding to the coefficient
will be denoted by
.
Around each point
of the field-figure as a centre we may now construct an infinitesimal surface[7], which, when
is chosen as origin of coordinates, is determined by the equation
![]() |
(2) |
where
is an infinitely small positive constant which we shall fix once for all. This surface, which we shall call the indicatrix, is a hyperboloid with one real axis and three imaginary ones. We shall also introduce the surface determined by the equation
![]() |
(3) |
which differs from (2) only by the sign of
. We shall call this the conjugate indicatrix. It is to be understood that the indicatrices and conjugate indicatrices take part in the changes to which the field-figure may be subjected. As these surfaces are infinitely small, they always remain hyperboloids of the said kind. The gravitation field will now be determined by these indicatrices, which we can imagine to have been constructed in the field-figure without the introduction of coordinates. When we have occasion to use these latter, we shall so choose them that the "axes"
intersect the conjugate indicatrix constructed around their starting point, while the indicatrix itself is intersected by the axis
. This involves that the coefficients
are negative and that
is positive.
§ 5. The indicatrices will give us the units in which we shall express the length of lines in the field-figure and the magnitude of two-, three or four-dimensional extensions. When we use these units we shall say that the quantities in question are expressed in natural measure.
In the case of a line-element
the unit might simply be the radius-vector in the direction
of the indicatrix or the conjugate indicatrix described about
. It is however desirable to distinguish the two cases that
intersects the indicatrix itself or the conjugate indicatrix. In the latter case we shall ascribe an imaginary length to the line-element[8]. Besides, by taking as unit not the radius-vector itself but a length proportional to it, the numerical value of a line-element may be made to be independent of the choice of the quantity
.
These considerations lead us to define the length that will be ascribed to line-elements by the assumption that each radius-vector of the indicatrix has in natural measure the length
, while each radius-vector of the conjugate indicatrix has the length
.[9]
It will now be clear that the length of an arbitrary line in the field-figure can be found by integration, each of its elements being measured by means of the indicatrix or the conjugate indicatrix belonging to the position of the element. In virtue of our definitions a deformation of the field-figure will not change the length of lines expressed in natural measure and a geodetic line will remain a geodetic line.
§ 6. We are now in a position to indicate the first part
of the principal function (§ 1). Let
be a closed surface in the field-figure and let us confine ourselves to the principal function so far as it belongs to the space
enclosed by that surface. Then the quantity
is the sum, taken with the negative sign, of the lengths of all world-lines of material points so far as they lie within
, each length multiplied by a constant
, characteristic of the point in question and to be called its mass.[10]
It must be remarked that the elements of the world-lines of material points intersect the corresponding indicatrices themselves. The lengths of these lines are therefore real positive quantities.
A deformation of the field-figure leaves
unchanged.
§ 7. We shall now pass on to the part of the principal function belonging to the gravitation field. The mathematical expression for this part was communicated to me by Einstein in our correspondence. It is also to be found in Hilbert's paper in which it is remarked that the quantity in question may be regarded as the measure of the curvature of the four-dimensional extension to which (1) relates. Here we have to speak only of the interpretation of this quantity. To find this the following geometrical considerations may be used.
Let
and
be two line-elements starting from a point
of the field-figure,
the line-element joining the extremities
and
. If then the lengths of these elements in natural measure are

we define the angle
between
and
by the well known trigonometric formula
![]() |
(4) |
from which one can derive
![]() |
(5) |
By means of this formula we are able to determine the angle between any two intersecting lines. Of course the two other angles of the triangle
can be calculated in the same way.
Now two cases must be distinguished.
a. The plane of the triangle
cuts the conjugate indicatrix, but not the indicatrix itself. Then the three sides have positive imaginary values. Moreover each of them proves to be smaller than the sum of the others, from which one finds that the angles have real values and that their sum is
.
b. The plane PQR cuts both the indicatrix and the conjugate indicatrix. In this case different positions of the triangle are still possible. We can however confine ourselves to triangles the three sides of which are real. These are really possible, for in the plane of a hyperbola we can draw triangles the sides of which are parallel to radius-vectors drawn from the centre to points of the curve (and not of the conjugate hyperbola).
By a closer consideration of the triangles now in question it is found however that by the choice of our "natural" units one side is necessarily longer than the sum of the other two. Formula (4) then shows that the cosines of the angles are real quantities, greater than 1 in absolute value, two of them being positive, and the third negative. We must therefore ascribe to the angles imaginary or complex values. If for
we put

and

we find for the three angles expressions of the form
and 
so that the sum is again
.
From the cosine calculated by (4) or (5) the sine can be derived by means of the formula

where for the case
we can confine ourselves to the value

with the positive sign.
It deserves special notice that two conjugate radius-vectors of the indicatrix and the conjugate indicatrix are perpendicular to each other and that a deformation of the field-figure does not change the angle between two intersecting lines determined according to our definitions.
§ 8. Before proceeding further we must now indicate the natural units (§ 5) for two-, three-, or four-dimensional extensions in the field-figure. Like the unit of length, these are defined for each point separately, so that the numerical value of a finite extension is found by dividing it into infinitely small parts.
A two-dimensional extension cuts the conjugate indicatrix in an ellipse, or the indicatrix itself and the conjugate indicatrix in two conjugate hyperbolae. In both cases we derive our unit from the area of a parallelogram described on conjugate radius-vectors.
A three-dimensional extension cuts the conjugate indicatrix in an ellipsoid, or the indicatrix and its conjugate in two conjugate hyperboloids. Now our unit will be derived from the volume of a parallelepiped described on three conjugate radius-vectors.
In a similar way the magnitude of four-dimensional extensions will be determined by comparison with a parallelepiped the edges of which are four conjugate radius-vectors of the indicatrix and the conjugate indicatrix.
It must here be kept in mind that, according to well known theorems, the area of the parallelogram and the volume of the parallelepipeds in question are independent of the special choice of the conjugate radius-vectors.
We shall further specify the units in such a way (comp. § 5) that the numerical magnitude of a parallelogram or a parallelepiped described on conjugate radius-vectors is found by multiplying the numbers by which the edges are expressed in natural measure.
From what has been said it follows that the area of the parallelogram described on two line-elements is given by the product of the lengths of these elements and the sine of the enclosed angle. Similarly the area of an infinitely small triangle is determined by half the product of two sides and the sine of the angle between them.
We need hardly add that the numerical value of any two-, three- or four-dimensional domain expressed in natural measure is not changed by a deformation of the field-figure.
§ 9. Let, at any point
of the field-figure, 1, 2, 3, 4 be four arbitrarily chosen conjugate radius-vectors of the indicatrix. Two of these determine an infinitely small part
of a two-dimensional extension. We may prolong this part to finite distances from
by drawing from this point geodetic lines whose initial directions lie in the plane
. In this way we obtain six two-dimensional extensions (1,2), (2,3), (3,1), (1,4), (2,4) and (3,4). Let us now consider in one of these e. g. (
) an infinitesimal triangle near the point
, the sides of which are geodetic lines (viz. geodetic lines in (
)). If in calculating the angles of this triangle we go to quantities of the second order with respect to the sides and to the distances from
, the sum
of the angles proves to have no longer the value
(comp. § 7). The "excess"
is proportional to the area
of the triangle, independently of the length of the sides, of their ratios and of the position of the triangle in the extension (
). For the three extensions (1,2) (2,3), (3,1), which do not intersect the indicatrix itself but the conjugate indicatrix, this proposition follows from a well-known theorem of Gauss in the theory of curvature of surfaces; for the other three (1,4), (2,4), (3,4), which cut the indicatrix itself, the proof can be given by direct calculation. The considerations necessary for this, and some other calculations with which we shall be concerned further on will be communicated in a later paper.
In considering the three last-mentioned extensions I have confined myself to triangles with real sides (§ 7, b).
The quotient

is now for each extension a definite number, which we may consider as a measure of the curvature of the two-dimensional extension (
); the sum
of the six numbers
may be called the curvature of the field-figure at the point
in question. This quantity is the same that has been introduced by Hilbert; this results from the calculation of its value, which at the same time shows
to be independent of the special choice of the directions 1, 2, 3, 4 introduced in the beginning of this §.
The numbers
all real and have a meaning that can be indicated without the introduction of coordinates; moreover their sum
is not changed by a deformation of the field-figure.
If now
is an element of the four-dimensional extension of the field-figure, expressed in natural measure, the part of the principal function belonging to the gravitation field is
![]() |
(6) |
where the integration is extended to the domain considered (§ 6) while
is the gravitation constant.
too is not changed by a deformation of the field-figure.
The factor
has been introduced in order to obtain a real value for
, the element
being represented in natural measure by a negative imaginary number (§ 8).
§ 10. What we have to say of the electromagnetic field must be preceded by some considerations belonging to what may be called the "vector theory" of the field-figure.
A line-element
, taken in a definite, direction (indicated by the order of the letters), may be called a vector. Such vectors can be compounded or decomposed by means of parallelograms or parallelepipeds. Especially, when coordinates
have been chosen, a vector may be resolved into four components which have the directions of the coordinates, viz. such directions that a shift along the first e.g. changes
, while
remain constant. The four components in question are determined by the differentials
corresponding to
. We shall say that by these they are expressed in "
-measure". Their values in natural measure are found by multiplying
by certain factors. If we keep in mind that the radius-vectors of the e conjugate indicatrix and the indicatrix in the directions of the axes are expressed in "
measure" by

and in natural units by

we find for the reducing factors
![]() |
(7) |
In the language of vector-analysis the vector obtained by the composition of two or more vectors is also called the sum of these vectors.
We shall also speak of finite vectors, i.e. of directed quantities which can be represented on an infinitely reduced scale by line-elements in the field-figure. If
is the constant "reduction factor" chosen for this purpose, a vector
will be represented by a line-element
, the direction of which is also ascribed to
. It will now be evident that two finite vectors, as well as two infinitely small ones, determine an infinitesimal two dimensional extension and that finite vectors can be compounded and resolved by means of parallelograms and parallelepipeds. Also that we may speak of the "magnitude" of such figures, that e.g. the rule given in § 8 applies to the parallelogram described on two vectors.
The components of a vector in the directions of the coordinates expressed in
-measure will be called
. This means that
are equal to the differentials
corresponding to the infinitely small vector
.
If we want to know the components of
in natural units we must multiply
by the factors (7).
§ 11. Two vectors
and
starting from a point
of the field-figure and lying in a plane
, determine what we shall call a rotation
in that plane. We ascribe to it the direction indicated by the order
and a value given by the parallelogram described on
and
and expressed in natural measure[11]. This involves that the same rotation may be represented in many different ways by two vectors in the plane
.
For the rotation
we shall also use the symbol
.
By the vector product
of three vectors
at a point of the field-figure and not lying in one plane we shall understand a vector
the direction of which is conjugate with each of the three vectors (and therefore with the three-dimensional extension
), the direction of
corresponding to those of
and
in a way presently to be indicated, while the magnitude of
, expressed in natural measure, is equal to that of the parallelepiped described on
,
and
and expressed in the same measure. This definition involves that the value is ascribed to the vector product of three vectors lying in one and the same plane.
A further statement about the direction of
is necessary because two opposite directions are conjugate with
. For one set of three directions
we shall choose arbitrarily which of its two conjugate directions will be said to correspond to it. If this is the direction
, then the direction
corresponding to
will be determined by the rule that
, passes into
by a gradual passage of the first three vectors from
into
, this latter passage being effected in such a way that during the change the vectors never come to lie in one plane.
The vector product
takes the opposite direction when one of the vectors is reversed as well as when two of them are interchanged. We must therefore always attend to the order of the symbols in
.
The vector product possesses the distributive property with respect to each of the three vectors, so that e.g. if
and
are vectors,
![\left[\left(\mathrm{A}_{1}+\mathrm{A}_{2}\right)\cdot\mathrm{B\cdot C}\right]=\mathrm{\left[A_{1}\cdot B\cdot C\right]+\left[A_{2}\cdot B\cdot C\right]}](http://upload.wikimedia.org/math/c/5/a/c5a6cb28510e69eddce34a29ded2cfac.png)
From this we can infer that
depends only on
and the rotation
determined by
and
. For this reason we write for the vector product also
; in calculating it we are free to replace the rotation
by any two vectors by means of which it can be represented.
If
,
and
are rotations in the same plane, such that the value and direction of
are found by adding
and
algebraically, we have, in virtue of the distributive property
![[\mathrm{R_{1}\cdot C]}+[\mathrm{R_{2}\cdot C]}=[\mathrm{R\cdot C]}](http://upload.wikimedia.org/math/d/b/d/dbdbf952d365958a7f1afcfcfbc0dbc9.png)
we may also express these volumes in the "
-units" corresponding to the coordinates chosen.
Let us consider e.g. the three-dimensional extension
, which cuts the conjugate indicatrix in the ellipsoid

If we agree that in
-measure spaces in this extension will be represented by positive numbers and that a parallelepiped with the positive edges
will have the volume
, we find for that of the parallelepiped on three conjugate radius-vectors

where it has been taken into consideration that
is negative.
The volume of the same parallelepiped being expressed in natural measure by —
(§ 8), we have to multiply by
![]() |
(8) |
if we want to pass from the expression in
-measure to that in natural measure.
For the extension
, i.e.
the corresponding factor is
![]() |
(9) |
§ 13. In the theory of electromagnetic phenomena we are concerned in the first place with the electric charge and the convection current. So far as these quantities belong to a definite element
of the field-figure they may be combined into

where
is a vector which we may call the current vector. When it is resolved into four components having the directions of the axes, the first three components determine the convection current, while the fourth component gives the density of the electric charge.
As to the electric and the magnetic force, these two taken together can be represented at each point of the field-figure by two rotations
and 
in definite, mutually conjugate two-dimensional extensions. These quantities are closely connected with the current vector, for after having introduced coordinates
we have for each closed surface
the vector equation
![]() |
(10) |
where the second integral has to be taken over the domain
enclosed by
. On the left hand side
represents a three-dimensional surface-element expressed in natural units and
a vector of the magnitude 1 in natural measure conjugate with or perpendicular to that element (§ 7) and directed towards the outside of the domain
. The index
shows that the vector
must be expressed in
-measure. At each point of the surface we must resolve the vector along the four directions of the coordinates, express each component in
-measure (§10) and finally, after multiplication by
, we must add algebraically all
-components; similarly all
-components and so on.
It must be expressly remarked that if an equation like (10) in which we are concerned with the composition of vectors at different points of the field-figure, shall have a definite meaning we must know which components are to be considered as having the same direction, so that they can be added. This has been determined by the introduction of coordinates.
On the right hand side of the equation the index
means that the vector
must be expressed in
-measure and the factor
had to be introduced because
is imaginary.
One can prove that equation (10) is equivalent to the differential equations which in Einstein's theory serve for the same purpose and further that when the equation holds for one choice of coordinates it will also be true for any other choice.
§ 14. The proof for these assertions must be deferred to the second part of this communication. For the present we shall only add that the part of the principal function referring to the electromagnetic field is given by

where
and
are, expressed in natural units, the two rotations that are characteristic of the field. Like the two other parts of the principal function,
is not changed by a deformation of the field-figure. In this statement it is to be understood that the parallelograms by which
and
are represented take part in the deformation.
Some remarks on the way in which, starting from the principal function, we may obtain the fundamental equations of the theory must also be deferred. I shall conclude now by remarking that, as an immediate consequence of Hamilton's principle, the world-line of a material point which is acted on only by a given gravitation field, will be a geodetic line, and that the equations which determine the gravitation field caused by material and electromagnetic systems will be found by the consideration of infinitely small variations of the indicatrices, by which the numerical values of all quantities that are measured by means of these surfaces will be changed.
II.
(Communicated in the meeting of March 25, 1916).
§ 15. In the first part of this communication the connexion between the electric and the magnetic force on one hand and the charge and the convection current on the other was expressed by the equation
![]() |
(10) |
which has been discussed in § 13. It will now be shown that this formula is equivalent to the differential equations by which the connexion in question is expressed in the theory of Einstein. For this purpose some further geometrical considerations must first be developed. They refer to the special case that the quantities
, have the same values at every point of the field-figure.
If this condition is fulfilled, considerations which generally may be applied to infinitesimal extensions only are valid for finite extensions too.
§ 16. The factor required, in the measurement of four-dimensional domains, for the passage from
-units to natural units has now the same value at every point of the field-figure. Similarly, when any one-, two- or three-dimensional extension in the field-figure that is determined by linear equations ("linear extensions") is considered, the factor by means of which the said passage may be effected for parts of that extension, will be the same for all those parts. Moreover the factor in question will be the same for two "parallel" extensions of this kind, i.e. for two extensions the determining equations of which can be written in such a way that the coefficients of
are the same in them.
It is obvious that linear one-dimensional extensions can be called "straight lines", also it will be clear what is to be understood by a "prism" (or "cylinder"). This latter is bounded by two mutually parallel linear three-dimensional extensions
and
and by a lateral surface which may be extended indefinitely to both sides and in which mutually parallel straight lines ("generating lines") can be drawn.
We need not dwell upon the elementary properties of the prism.
§ 17. A vector may now be represented by a straight line of finite length; the quantities
, which have been introduced in § 10, are the changes of the coordinates caused by a displacement along that line. The magnitude of the vector, expressed in natural units, will be denoted by
. It is given by a formula similar to (1), viz. by
![]() |
(11) |
A vector may be regarded as being the same everywhere in the field-figure, if
have constant values. In the same way a rotation
(§ 11) may be said to be the same everywhere, if it can be represented by two vectors of this kind.
If from a point
two vectors
and
issue, denoted by
,
and
,
resp., the angle between them (comp. (5)) is defined by
![]() |
(12) |
We remark here that
are real, positive or negative quantities and that
and
are expressed in the way indicated in § 5 ("absolute" values). It is to be understood that
does not change when the signs of
are reversed at the same time.
If
is the value of the vector
and if the angle between this vector and
is denoted by (
), it follows further from (11) and (12) that

In the special case of a right angle
we have

an equation expressing the connexion between a vector
and its "projection" on a line
. The angle (
) is the angle between the vector and its projection, both reckoned from the same point
.
§ 18. Let us now return to the prism
mentioned in § 16. From a point
of the boundary of the "upper face"
, we can draw a line perpendicular to
and
. Let
be the point, where it cuts thus last, plane, the "base", and
the point where this plane is encountered by the generating line through
. If then
, we have
![]() |
(13) |
The strokes over the letters indicate the absolute values of the distances
and
.
It can be shown (§ 8) that, all quantities being expressed in natural units, the "volume" of the prism
is found by taking the product of the numerical values of the base
and the "height"
.
Let now linear three-dimensional extensions perpendicular to
be made to pass through
and
. From these extensions the lateral boundary of the prism cuts the parts
and
and these parts, together with the lateral surface, enclose a new prism
, the volume of which is equal to that of
. As now the volume of
is given by the product of
and
, we have with regard to (13)

If now we remember that, if a vector perpendicular to
is projected on the generating line, the ratio between the projection and the vector itself (viz. between their absolute values) is given by
and that a connexion similar to that which was found above between a normal section
of the prism and
, also exists between
and any other oblique section, we easily find the following theorem:
Let
and
be two arbitrarily chosen linear three-dimensional sections of the prism,
and
two vectors, perpendicular to
and
resp. and of the same length,
and
the absolute values of the projections of
and
on a generating line. Then we have
![]() |
(14) |
§ 19. After these preliminaries we can show that the left hand side of (10) is equal to 0, if the numbers
are constants and if moreover both the rotation
and the rotation
are everywhere the same. For the two parts of the integral the proof may be given in the same way, so that it suffices to consider the expression
![]() |
(15) |
be the components of the vector
, expressed in
-units. From the distributive property of the vector product it then follows that each of the four components of
![\left[\mathrm{R}_{e}\cdot\mathrm{N}\right]_{x}](http://upload.wikimedia.org/math/b/d/4/bd44093782f8e815c524b5aed2170015.png)
is a homogeneous linear function of
. Under the special assumptions specified at the beginning of this § these are every where, the same functions. Let us thus consider a definite component of (15) e.g. that which corresponds to the direction of the coordinate
. We can represent it by an expression of the form

where
are constants. It will therefore be sufficient to prove that the four integrals
![]() |
(16) |
vanish.
In order to calculate
we consider an infinitely small prism, the edges of which have the direction
. This prism cuts from the boundary surface
two elements
and
. Proceeding along a generating line in the direction of the positive
we shall enter the extension
bounded by
through one of these elements and leave it through the other. Now the vectors perpendicular to
, which occur in (15) and which we shall denote by
and
for the two elements, have the same value.[12] If, therefore,
and
are the absolute values of the projections of
and
on a line in the direction
, we have according to (14)
![]() |
(17) |
Let first the four directions of coordinates be perpendicular to one another. Then the components of the vector obtained by projecting
on the above mentioned line are
and similarly those of the projection of
. But as, proceeding in the direction of
we enter
through one element and leave it through the other, while
and
are both directed outward,
and
, must have opposite signs. So we have

and because of (17) we may now conclude that the elements
and
in the first of the integrals (16) annul each other. It will be clear now that the whole integral vanishes and that similar considerations may be applied to the other three.
So we have proved that under the special assumptions made the left hand side of (10) will vanish in the special case that the directions of the coordinates are perpendicular to each other. This conclusion likewise holds for an other set of coordinates if only the assumption made at the beginning of this § is fulfilled. This is obvious, as we can pass from mutually perpendicular coordinates
to arbitrarily chosen other ones
which fulfil this latter condition by linear transformation formulae with constant coefficients. The
- and the
-components of the vector
![\left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]](http://upload.wikimedia.org/math/d/4/a/d4a5f6d4081e82b6d66617dcac8f8707.png)
are then connected by homogeneous linear formulae with coefficients which have the same value at all points of the surface
. Hence if, as has been shown above, the four
-components of the vector
![\int\left\{ \left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]\right\} d\sigma](http://upload.wikimedia.org/math/e/c/9/ec97c72f5d213de75ee9cc13ea4f9a45.png)
vanish, the four
-components are now seen to do so likewise.[13]
§ 20. The above considerations were intended to prepare a corollary which will be of use in the treatment of the integral on the left hand side of (10), if we now leave the special assumptions made above and suppose the quantities
to be functions of the coordinates while also the rotations
and
may change from point to point.
This corollary may be formulated as follows: If all dimensions of the limiting surface
are infinitely small of the first order, the integral
![\int\left\{ \left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]\right\} _{x}d\sigma](http://upload.wikimedia.org/math/6/5/a/65a7b58beb6ce50b1cebc3a148b0ac18.png)
will be of the fourth order.
In order to make this clear let us suppose that in the calculation of the integral we confine ourselves to quantities of the third order. The surface
being already of that order we may then omit all infinitesimal values in the quantities by which
is multiplied; we may therefore neglect the infinitesimal changes of the quantities
over the extension considered, and also those of
and
. By this we just come to the case considered in § 19. Thus it is evident, that as regards quantities of the third order the first part of (10) is 0. From this it follows that in reality it is at least of the fourth order.
§ 21. Let us now return to the general case that the extension
to which equation (10) refers, has finite dimensions. If by a surface
this extension is divided into two extensions
and
, the quantities on the two sides in (10) each consist of two parts referring to these extensions. For the right hand side this is immediately clear and as to the quantity on the left hand side, it follows from the consideration that the contributions of a to the integrals over the boundaries of
and
are equal with opposite signs. In the two cases namely we must take for
equal but opposite vectors.
Also, if the extension
is divided into an arbitrary number of parts, each term in (10) will be the sum of a number of integrals, each relating to one of these parts.
By surfaces with the equations
we can divide the extension
into elements which we shall denote by
. As a rule there will be left near the surface
certain infinitely small extensions of a different form. From the preceding § it is evident that, in the calculation of the integrals, these latter extensions may be neglected and that only the extensions
have to be considered. From this we can conclude that equation (10) is valid for any finite extension, as soon at it holds for each of the elements
.
§ 22. We shall now show what equation (10) becomes for one element
. Besides the infinitesimal quantities
, occurring in the equation

of the indicatrix we introduce four other quantities
, which we define by
![]() |
(18) |
or
![]() |
(19) |
with the equalities
.
To each of these quantities corresponds a definite direction, viz. that in which we have to proceed in order to make the considered quantity change in positive sense while the other three remain constant. If we denote these directions by
and in the same way the directions of the coordinates
by 1, 2, 3, 4, it is evident that
is conjugate with 2, 3 and 4,
with 3, 1 and 4, and so on; inversely 1 with
; 2 with
, and so on. From what has been said above about the algebraic signs of
it follows further that, if directions opposite to 1,
etc. are denoted by — 1,
etc., the directions — 1 and
will point to the same side of an extension
. The same may be said of the directions —2 and
or —3 and
with respect to extensions
, or
, while with respect to an extension
, the directions 4 and
point to the same side.
Finally, we shall fix (§11) as far as is necessary, which direction corresponds to three others. For that purpose we shall imagine the directions of coordinates
to pass into mutually conjugate directions, which will also be called
</math>, by gradual changes, in such a way that never three of them come to lie in one plane. We shall agree that after this change —4 corresponds to 1, 2, 3.
Let
be the numbers 1, 2, 3, 4 in an order obtained from the natural one by an even number of permutations. Then the rule of § 11 teaches us that the direction
corresponds to
. It is clear that this would be the ease with
, if
were obtained from 1, 2, 3, 4 by an odd number of permutations. If further it is kept in mind that, always in the new case, the directions
coincide with —1, —2, —3, 4, we come to the conclusion that the directions 1, 2, 3 and 4 correspond to the sets
and
respectively. The rule of gradual change (§11) involves that this holds also for the original case, in which 1, 2, 3, 4 were not yet mutually conjugate.
This is all that has to be said about the relations between the different directions. It must only be kept in mind, that whenever two of the first three directions are interchanged, the fourth must be reversed.
§ 23. In the neighbourhood of a point
of the field-figure we may introduce as coordinates instead of
the quantities
defined by (19). Line-elements or finite vectors can be resolved in the directions of these coordinates, i.e. in the directions
. Their components and the magnitudes of different extensions can now be expressed in
-nits in the same way as formerly in
-units. So the volume of a three-dimensional parallelepiped with the positive edges
is represented by the product
.
Solving
from (19) we obtain expressions of the form
![]() |
(20) |
If we use the coordinates
the coefficients
play the same part as the coefficients
when the coordinates
are used. According to (18) and (20) we have namely

so that the equation of the indicatrix may be written

§ 24. Let the rotations
and
of which we spoke in § 13 be defined by the vectors
and
respectively, the resultants of the vectors
, etc. in the directions
. Then, according to the properties of the vector product that were discussed in § 11,
![\begin{array}{ll}
\left[\mathrm{R}_{e}\cdot\mathrm{N}\right] & =\left[\mathrm{\left(A_{1^{*}}^{I}+\dots+A_{4^{*}}^{I}\right)\cdot\left(A_{1^{*}}^{II}+\dots+A_{4^{*}}^{II}\right)\cdot N}\right]\\
& =\sum(\overline{ab})\left\{ \left[\mathrm{A}_{a^{*}}^{I},\ \mathrm{A}_{b^{*}}^{II}\cdot\mathrm{N}\right]-\left[\mathrm{A}_{a^{*}}^{II},\ \mathrm{A}_{b^{*}}^{I}\cdot\mathrm{N}\right]\right\}
\end{array}](http://upload.wikimedia.org/math/4/5/5/455a1870688aea312584096eedc683c2.png)
where the stroke over
indicates that each combination of two different numbers
contributes one term to the sum. For the vector product
we have a similar equation. Now two or more rotations in one and the same plane, e.g. in the plane
, may be replaced by one rotation, which can be represented by means of two vectors with arbitrarily chosen directions in that plane, e.g. the directions
and
. We may therefore introduce two vectors
and
directed along
and
resp., so that
![]() |
(21) |
Then we must substitute in (10)
![]() |
(22) |
Here it must be remarked that the magnitude and the sense of one of the vectors
may be chosen arbitrarily; when this has been done, the other vector is perfectly determined.
In the following calculations the vector
has one of the directions
. As this is also the case with the vectors
and
, the vector product occurring in (22) can easily be expressed in
-units. After that we may pass to natural units and finally, as is necessary for the substitution in (10), to
-units.
In order to pass from
-units to natural units we have to multiply a vector in the direction
by a certain coefficient
, and a part of the extension
by a coefficient
. These coefficients correspond to
(§ 10) and
(§ 12). The factors
e.g. can be expressed by means of the minors
of the determinant
of the quantities
. If this is worked out and if the equations

are taken into consideration, we obtain the following corollary, which we shall soon use:
Let
and also
be the numbers 1, 2, 3, 4 in any order,
being not the same as
, then we have, if none of the two numbers
and
is 4,
![]() |
(23) |
and if one of the two is 4
![]() |
(24) |
§ 25. We shall now suppose (comp. § 24) that in
-units the vector
has the value +1, and we shall write
for the value that must then be given to
. If the
-components of the vectors
etc. are denoted by
etc., we find from (21)
![]() |
(25) |
This formula involves that
![]() |
(26) |
It may be remarked that
is the value that must be given to the vector
if
is taken to be 1.
The quantities
may be said to represent the rotations
.
At the end of our calculations we shall introduce instead of
the quantities t
defined by
![]() |
(27) |
In the first of these equations
are supposed to be the numbers 1, 2, 3, 4, in an order obtained from 1, 2, 3, 4 by an even number of permutations.
§ 26. We have now to calculate the left hand side of equation (10) for the case that
is the surface of an element
. For this purpose we shall each time take together two opposite sides, calculating for each pair the contributions due to the different terms on the right hand side of (22), or as we may say to the different rotations
. It is convenient now to denote by
the numbers 1, 2, 3 either in this order or in any other derived from it by a cyclic permutation, while the
-components of the vector we are calculating and which stands on the left hand side of (10) will be represented by
.
a. Let us first consider that one of the sides
which faces towards the side of the positive
. The vector
drawn outward has the direction
and in
-units the magnitude
. As the direction
corresponds to
, the rotation
gives with
a vector product represented by a vector in the direction
. The magnitude of this vector is in
-units

and in natural units

This must be multiplied by
, the magnitude of the side under consideration in natural units, and finally by
to express the vector product in
-units. Because of (24) we may write for the result

The opposite side gives a similar result with the opposite sign (
having for that side the direction
), so that together the sides contribute the term

to the component
. For shortness sake we have put here

Finally we may take,
.
facing towards the positive
. The vector
has now the direction
. We consider the vector products of this vector with the rotations
,
and
, which vector products have the directions
and 4. A calculation exactly similar to the one we performed just now gives the contributions to
. For these we thus find the products of
by

Taking also into consideration the opposite side
we find for
the contributions

This may be applied to each of the three pairs of sides not yet mentioned under
; we have only to take for
successively 1, 2, 3.
Summing up what has been said in this § we may say: the components of the vector on the left hand side of (10) are

§ 27. For the components of the vector occurring on the right hand side of (10) we may write

if
is the component of the vector
in the direction
expressed in
-units, while
represents the magnitude of the element
in natural units. This magnitude is

so that by putting
![]() |
(28) |
we find for equation (10)
![]() |
(29) |
The four relations contained in this equation have the same form as those expressed by formula (25) in my paper of last year[14]. We shall now show that the two sets of equations correspond in all respects. For this purpose it will be shown that the transformation formulae formerly deduced for
and
follow from the way in which these quantities have been now defined. The notations from the former paper will again be used and we shall suppose the transformation determinant
to be positive.
§ 28. Between the differentials of the original coordinates
and the new coordinates
which we are going to introduce we have the relations
![]() |
(30) |
and formulae of the same form (comp. § 10) may be written down for the components of a vector expressed in
-measure. As the quantities
constitute a vector and as

we have according to (28)[15]

or

Further we have for the infinitely small quantities
[16] defined by (19)

and in agreement with this for the components of a vector expressed in
-units

so that we find from (25)[17]

Interchanging here
and
, we obtain

and
![]() |
(31) |
The quantity between brackets on the right hand side is a second order minor of the determinant
and as is well known this minor is related to a similar minor of the determinant of the coefficients
. If
corresponds to
in the way mentioned in § 25, and
in the same way to
, we have

so that (31) becomes

According to (27) this becomes

for which we may write

Interchanging
and
in the second of the two parts into which the sum on the right hand side can be decomposed, and taking into consideration that

as is evident from (26) and (27), we find[18]

§ 29. Finally it can be proved that if equation (10) holds for one system of coordinates
, it will also be true for every other system
, so that
![]() |
(32) |
To show this we shall first assume that the extension
, which is understood to be the same in the two cases, is the element
.
For the four equations taken together in (10) we may then write
![]() |
(33) |
and in the same way for the four equations (32)
![]() |
(34) |
We have now to deduce these last equations from (33). In doing so we must keep in mind that
are the
-components and
the
-components of one definite vector and that the same may be said of
and
.
Hence, at a definite point (comp. (30))
![]() |
(35) |
We shall particularly denote by
the values of these quantities belonging to the angle
from which the edges
issue in positive directions. To the right hand sides of the equations (34) we may apply transformation (35) with these values of
,
-being infinitely small of the fourth order and it being allowed to confine ourselves to quantities of this order.
On the left hand sides of (34), however, we must take into consideration, the surface being of the third order, that the values of
change from point to point. Let
be the changes which
undergo when we pass from
to any other point of the surface. Then we must write for the value of the coefficient at this last point

We thus have

It will be shown presently that the last term vanishes. This being proved, it is clear that the relations (34) follow from (33); indeed, multiplying equations (33) by
respectively and adding them we find

§ 30. The proof for
![]() |
(36) |
rests on the relations
![]() |
(37) |
which follow from

The integral which occurs in (36) differs from
![]() |
(38) |
by the infinitely small factor under the sign of integration

Now we have calculated in § 26 integrals like (38) by taking together each time two opposite sides, one of which
passes through
while the second
is obtained from the first by a shift in the direction of one of the coordinates e. g. of
over the distance
. We had then to keep in mind that for the two sides the values of
, which have opposite signs, are a little different; and it was precisely this difference that was of importance. In the calculation of the integral
![]() |
(39) |
however it may be neglected. Hence, when we express the components
in terms of the quantities
, we may give to these latter the values which they have at the point
.
Let us consider two sides situated at the ends of the edges
and whose magnitude we may therefore express in
-units
if
are the numbers which are left of 1, 2, 3, 4 when the number
is omitted. For the part contributed to (38) by the side
we found in § 26

We now find for the part of (39) due to the two sides
![\psi{}_{be}\sum(c)\frac{\partial\pi{}_{ba}}{\partial x_{c}}\left[\int\limits _{2}\mathrm{x}_{c}d\sigma-\int\limits _{1}\mathrm{x}_{c}d\sigma\right]](http://upload.wikimedia.org/math/0/5/1/051feb1a202e5f3692d7801929b6c925.png)
where the first integral relates to
and the second to
. It is clear that but one value of
, viz.
has to be considered. As everywhere in
and everywhere in
it is further evident that the above expression becomes

This is one part contributed to the expression (36). A second part, the origin of which will be immediately understood, is found by interchanging
and
. With a view to (37) and because of

we have for each term of (36) another by which it is cancelled. This is what had to be proved.
§ 31. Now that we have shown that equation (32) holds for each element
we may conclude by the considerations of § 21 that this is equally true for any arbitrarily chosen magnitude and shape of the extension
. In particular the equation may be applied to an element
and by considerations exactly similar to those presented in § 26 we see that in the new coordinates as well as in the original ones we have equations of the form (29).
Whatever be our choice of the coordinates the part of the principal function indicated in § 14 can therefore be derived for a given current vector
.
III.
(Communicated in the meeting of April 1916.)[19]
§ 32. In the two preceding papers[20] we have tried so far as possible to present the fundamental principles of the new gravitation theory in a simple form.
We shall now show how Einstein's differential equations for the gravitation field can be derived from Hamilton's principle. In this connexion we shall also have to consider the energy, the stresses, momenta and energy-currents in that field.
We shall again introduce the quantities
formerly used and we shall also use the "inverse" system of quantities for which we shall now write
. It is found useful to introduce besides these the quantities

Differential coefficients of all these variables with respect to the coordinates will be represented by the indices belonging to these latter, e.g.

We shall use Christoffel's symbols
![\left[\begin{array}{c}
ab\\
c
\end{array}\right]=\frac{1}{2}\left(g_{ac,b}+g_{bc,a}-g_{ab,c}\right)](http://upload.wikimedia.org/math/3/f/7/3f748fd80fe115c2cc079d6beb9abc8d.png)
and Riemann's symbol
![\begin{array}{l}
(ik,lm)=\frac{1}{2}\left(g_{im,lk}+g_{kl,im}-g_{il,km}-g_{km,il}\right)+\\
\\
\qquad+\sum(ab)g^{ab}\left\{ \left[\begin{array}{c}
im\\
a
\end{array}\right]\left[\begin{array}{c}
kl\\
b
\end{array}\right]-\left[\begin{array}{c}
il\\
a
\end{array}\right]\left[\begin{array}{c}
km\\
b
\end{array}\right]\right\}
\end{array}](http://upload.wikimedia.org/math/3/6/7/367f432bc01d3cd636130b5cc3a9bb88.png)
Further we put
![]() |
(40) |
![]() |
(41) |

where

In the integral
, the element of the field-figure, is expressed in
-units. The integration has to be extended over the domain within a certain closed surface
;
is a positive constant.
§ 33. When we pass from the system of coordinates
to another, the value of
proves to remain unaltered; it is a scalar quantity. This may be verified by first proving that the quantities
form a covariant tensor of the fourth order[21]. Next,
being a contravariant tensor of the second order[22], we can deduce from (40) that
is a covariant tensor of the same order[23]. According to (41)
is then a scalar. The same is true[24] for
.
We remark that
[25] and
. We shall suppose
to be written in such a way that its form is not altered by interchanging
and
or
and
. If originally this condition is not fulfilled it is easy to pass to a "symmetrical" form of this kind.
It is clear that
may also be expressed in the quantities
and their first and second derivatives and in the same way in the
and first and second derivatives of these quantities.
If the necessary substitutions are executed with due care, these new forms of
will also be symmetrical.
§ 34. We shall first express the quantity
in the
's and their derivatives and we shall determine the variation it undergoes by arbitrarily chosen variations
, these latter being continuous functions of the coordinates. We have evidently

By means of the equations
and 
this may be decomposed into two parts
![]() |
(42) |
namely
![]() |
(43) |
![]() |
(44) |
The last equation shows that
![]() |
(45) |
if the variations
and their first derivatives vanish at the boundary of the domain of integration.
§ 35. Equations of the same form may also be found if
is expressed in one of the two other ways mentioned in § 33. If e.g. we work with the quantities
we shall find

where
and
are directly found from (43) and (44) by replacing
,
,
,
and
etc. by
,
etc. If the variations chosen in the two cases correspond to each other we shall have of course

Moreover we can show that the equalities

exist separately.[26]
The decomposition of
into two parts is therefore the same, whether we use
or
.
It is further of importance that when the system of coordinates is changed, not only
is an invariant, but that this is also the case with
and
separately.[27]
We have therefore
![]() |
(46) |
§ 36. For the calculation of
we shall suppose
to be expressed in the quantities
and their derivatives. Therefore (comp. (43))
![]() |
(47) |
if we put

Now we can show that the quantities
are exactly the quantities
defined by (40). To this effect we may use the following considerations.
We know that
is a contravariant tensor of the second order. From this we can deduce that
is also such a tensor.
Writing for it
we find according to (46) and (47) that

is a scalar for every choice of
.
This involves that
is a covariant tensor of the second order and as the same is true for
we must prove the equation

only for one special choice of coordinates.
§ 37. Now this choice can be made in such a way that at the point
of the field-figure
,
,
for
and that moreover all first derivatives
vanish. If then the values
at a point
near
are developed in series of ascending powers of the differences of coordinates
the terms directly following the constant ones will be of the second order. It is with these terms that we are concerned in the calculation both of
and of
for the point
. As in the results the coefficients of these terms occur to the first power only, it is sufficient to show that each of the above mentioned terms separately contributes the same value to
and to
.
From these considerations we may conclude that
![]() |
(48) |
Expressions containing instead of
either the variations
or
might be derived from this by using the relations between the different variations. Of these we shall only mention the formula
![]() |
(49) |
§ 38. In connexion with what precedes we here insert a consideration the purpose of which will be evident later on. Let the infinitely small quantity
be an arbitrarily chosen continuous function of the coordinates and let the variations
be defined by the condition that at some point
the quantities
have after the change the values which existed before the change at the point
, to which
is shifted when
is diminished by
, while the three other coordinates are left constant. Then we have

and similar formulae for the variations
.
If for
and
the expressions (48) and (44) are taken, the equation
![]() |
(50) |
is an identity for every choice of the variations.
It will likewise be so in the special case considered and we shall also come to an identity if in (50) the terms with the derivatives of
are omitted while those with
itself are preserved.
When this is done
reduces to

and, taking into consideration (44) and (48), we find after division by 
![]() |
(51) |
In the second term of (44) we have interchanged here the indices
and
.
If for shortness' sake we put, for 
![]() |
(52) |
and for 
![]() |
(53) |
we may write
![]() |
(54) |
The set of quantities
will be called the complex
and the set of the four quantities which stand on the left hand side of (54) in the cases
, the divergency of the complex.[28] It will be denoted by
and each of the four quantities separately by
.
The equation therefore becomes
![]() |
(55) |
![]() |
(56) |
§ 39. We shall now consider a second complex
, the components of which are defined by
![]() |
(57) |
Taking also the divergency of this complex we find that the difference

has just the value which we can deduce from (56) for the corresponding difference

It is thus seen that

and that we have therefore
![]() |
(58) |
for all systems of coordinates as soon as this is the case for one system.
Now a direct calculation starting from (52), (53) and (57) teaches us that the terms with the highest derivatives of the quantities
, (viz. those of the third order) are the same in
and
. Further it is evident that in the system of coordinates introduced in § 37 these terms with the third derivatives are the only ones. This proves the general validity of equation (58). It is especially to be noticed that if
and
are determined by (52), (53) and (57) and if the function defined in § 32 is taken for
, the relation is an identity.
§ 40. We shall now derive the differential equations for the gravitation field, first for the case of an electromagnetic system.[29] For the part of the principal function belonging to it we write

where
is defined by (35) (1915). From
we can derive the stresses, the momenta, the energy-current and the energy of the electromagnetic system; for this purpose we must use the equations (45) and (46) (1915) or in Einstein's notation, which we shall follow here,[30]
![]() |
(59) |
and for 
![]() |
(60) |
The set of quantities
might be called the stress-energy-complex (comp. § 38). As for a change of the system of coordinates the transformation formulae for
are similar to those by which tensors are defined, we can also speak of the stress-energy-tensor. We have namely

§ 41. The equations for the gravitation field are now obtained (comp. §§ 13 and 14, 1915) from the condition that
![]() |
(61) |
for all variations
which vanish at the boundary of the field of integration together with their first derivatives. The index
in the first term indicates that in the variation of
the quantities
must be kept constant.
If we suppose
to be expressed in the quantities
and if (42), (45) and (48) are taken into consideration, we find from (61) that at each point of the field-figure
![]() |
(62) |
If now in the first term we put
![]() |
(63) |
and if for
the value (49) is substituted, this term becomes

or if in the latter summation
is interchanged with
and if the quantity
![]() |
(64) |
is introduced,

Finally, putting equal to zero the coefficient of each
we find from (62) the differential equation required
![]() |
(65) |
This is of the same form as Einstein's field equations, but to see that the formulae really correspond to each other it remains to show that the quantities
and
defined by (63), f59) and (60) are connected by Einstein's formulae
![]() |
(66) |
We must have therefore
![]() |
(67) |
and for 
![]() |
(68) |
§ 42. This can be tested in the following way. The function
(comp. § 9, 1915) is a homogeneous quadratic function of the
's and when differentiated with respect to these variables it gives the quantities
. It may therefore also be regarded as a homogeneous quadratic function of the
. From (35), (29) and (32)[31], 1915 we find therefore
![]() |
(69) |
Now we can also differentiate with respect to the
's, while not the
's but the quantities
are kept constant, and we have e.g.
![]() |
(70) |
According to (69) one part of the latter differential coefficient is obtained by differentiating the factor
only and the other part by keeping this factor constant.
For the calculation of the first of these parts we can use the relation
![]() |
and for the second part we find

If (32) 1915 is used (67) and (68) finally become

These equations are really fulfilled. This is evident from
,
,
and
, besides, the meaning of
(§ 11, 1915) and equation (35) 1915 must be taken into consideration.
§ 43. In nearly the same way we can treat the gravitation field of a system of incoherent material points; here the quantities
and
(§§ 4 and 5, 1915) play a similar part as
and
in what precedes. To consider a more general case we can suppose "molecular forces" to act between the material points (which we assume to be equal to each other); in such a way that in ordinary mechanics we should ascribe to the system a potential energy depending on the density only. Conforming to this we shall add to the Lagrangian function
(§ 4, 1915) a term which is some function of the density of the matter at the point
of the field-figure, such as that density is when by a transformation the matter at that point has been brought to rest. This can also be expressed as follows. Let
be an infinitely small three-dimensional extension expressed in natural units, which at the point
is perpendicular to the world-line passing through that point, and
the number of points where
intersects world-lines. The contribution of an element of the field-figure to the principal function will then be found by multiplying the magnitude of that element expressed in natural units by a function of
. Further calculation teaches us that the term to be added to
must have the form
![]() |
(71) |
is given by (15) 1915. As the Lagrangian function defined by (11) 1915 equally falls under this form and also the sum of this function and the new term, the expression (71) may be regarded as the total function
. The function
may be left indeterminate. If now with this function the calculations of §§ 5 and 6, 1915 are repeated, we find the components of the stress-energy-tensor of the matter.
The equations for the gravitation field again take the form (65).
is defined by an equation of the form (63), where on the left hand side we must differentiate while the
's are kept constant. Relation (66) can again be verified without difficulty.
We shall not, however, dwell upon this, as the following considerations are more general and apply e.g. also to systems of material points that are anisotropic as regards the configuration and the molecular actions.
§ 44. At any point
of the field-figure the Lagrangian function
will evidently be determined by the course and the mutual situation of the world-lines of the material points in the neighbourhood of
. This leads to the assumption that for constant
's the variation
is a homogeneous linear function of the virtual displacements
of the material points and of the differential coefficients

these last quantities evidently determining the deformation of an infinitesimal part of the figure formed by the world-lines[32].
The calculation becomes most simple if we put
![]() |
(72) |
and for constant
's
![]() |
(73) |
Considerations corresponding exactly to those mentioned in §§ 4 — 6, 1915, now lead to the equations of motion and to the following expressions for the components of the stress-energy-tensor
![]() |
(74) |
and for 
![]() |
(75) |
are defined by

in the differentiation on the left hand side the coordinates of the material points are kept constant. To show that
and
satisfy equation (66) we must now show that

and for 

If here the value (72) is substituted for
and if (70) is taken into account, these equations say that for all values of
and
we must have
![]() |
(76) |
Now this relation immediately follows from a condition, to which
must be subjected at any rate, viz. that
is a scalar quantity. This involves that in a definite case we must find for
always the same value whatever be the choice of coordinates.
§ 45. Let us suppose that instead of only one coordinate
a new one
has been introduced, which differs infinitely little from
, with the restriction that if

the term
depends on the coordinate
only and is zero at the point in question of the field-figure. The quantities
then take other values and in the new system of coordinates the world-lines of the material points will have a slightly changed course.
By each of these circumstances separately
would change, but all together must leave it unaltered. As to the first change we remark that, according to the transformation formula for
, the variation
vanishes when the two indices are different from
, while

and for 

The change of
due to these variations is

which is a function of
only. Therefore according to (73) the second variation of
is

By putting equal to zero the sum of this expression and the preceding one we obtain (76).
§ 46. We have thus deduced for some cases the equations of the gravitation field from the variation theorem. Probably this can also be done for thermodynamic systems, if the Lagrangian function is properly chosen in connexion with the thermodynamic functions, entropy and free energy. But as soon as we are concerned with irreversible phenomena, when e.g. the energy-current consists in a conduction of heat, the variation principle cannot be applied. We shall then be obliged to take Einstein's field-equations as our point of departure, unless, considering the motions of the individual atoms or molecules, we succeed in treating these by means of the generalized principle of Hamilton.
§ 47. Finally we shall consider the stresses, the energy etc. which belong to the gravitation field itself. The results will be the same for all the systems treated above, but we shall confine ourselves to the case of §§ 44 and 45. We suppose certain external forces
to act on the material points, though we shall see that strictly speaking this is not allowed.
For any displacements
of the matter and variations of the gravitation field we first have the equation which summarizes what we found above

In virtue of the equations of motion of the matter, the terms with
cancel each other on the right hand side and similarly, on account of the equations of the gravitation field, the terms with
and
. Thus we can write[33]
![]() |
(77) |
Let us now suppose that only the coordinate
undergoes an infinitely small change, which has the same value at all points of the field-figure. Let at the same time the system of values
be shifted everywhere in the direction of
over the distance
. The left hand side of the equation then becomes
and we have on the right hand side

After dividing the equation by
we may thus, according to (74) and (75), write

By the same division we obtain from
the expression occurring on the left hand side of (51), which we have represented by

where the complex
is defined by (52) and (53). If therefore we introduce a new complex
which differs from
only by the factor
, so that
![]() |
(78) |
we find
![]() |
(79) |
The form of this equation leads us to consider
as the stress-energy-complex of the gravitation field, just as
is the stress-energy-tensor for the matter. We need not further explain that for the case
the four equations contained in (79) express the conservation of momentum and of energy for the total system, matter and gravitation field taken together.
§ 48. To learn something about the nature of the stress-energy-complex
we shall consider the stationary gravitation field caused by a quantity of matter without motion and distributed symmetrically around a point
. In this problem it is convenient to introduce for the three space coordinates
, (
will represent the time) "polar" coordinates. By
we shall therefore denote a quantity
which is a measure for the "distance" to the centre. As to
and
, we shall put
,
, after first having introduced polar coordinates
(in such a way that the rectangular coordinates are
,
,
). It can be proved that, because of the symmetry about the centre,
for
, while we may put for the quantities 
![]() |
(80) |
where
are certain functions of
. Ditferentiations of these functions will be represented by accents. We now find that of the complex
only the components
,
and
are different from zero. The expressions found for them may be further simplified by properly choosing
. If the distance to the centre is measured by the time the light requires to be propagated from to the point in question, we have
. One then finds
![]() |
(81) |
§ 49. We must assume that in the gravitation fields really existing the quantities
have values differing very little from those which belong to a field without gravitation. In this latter we should have

and thus we put now

where the quantities
and
which depend on
are infinitely small, say of the first order, and their derivatives too. Neglecting quantities of the second order we find from (81)

For our degree of approximation we may suppose that of the quantities
only
differs from 0. If we put
![]() |
(82) |
a quantity which depends on
and which we shall assume to be zero outside a certain sphere, we find from the field equations

We thus obtain
![]() |
(83) |
![]() |
(84) |
§ 50. If first we leave aside the first term of
, which would also exist if no attracting matter were present, it is remarkable that the gravitation constant
does not occur in the stress
nor in the energy
; the same would have been found if we had used other coordinates. This constitutes an important difference between Einstein's theory and other theories in which attracting or repulsing forces are reduced to "field actions". The pulsating spheres of Bjerknes e.g. are subjected to forces which, for a given motion, are proportional to the density of the fluid in which they are imbedded; and the changes of pressure and the energy in that fluid are likewise proportional to this density. In this case we shall therefore ascribe to the stress-energy-complex values proportional to the intensity of the actions which we want to explain. In Einstein's theory such a proportionality does not exist. The value of
is of the same order of magnitude as
in the matter. To our degree of approximation we find namely from (82)
.
§ 51. If we had not worked with polar coordinates but with rectangular coordinates we should have had to put for the field without gravitation
,
,
for
. Then we should have found zero for all the components of the complex. In the system of coordinates used above we found for the field without gravitation
; this is due to the complex
being no tensor. If it were, the quantities
would be zero in every system of coordinates if they had that value in one system.
It is also remarkable that in real eases the first term in (83) can be much larger than the following ones. If we consider e. g. a point
outside the attracting sphere, we can prove that the ratio of the first term to the third is of the same order as the ratio of the square of the velocity of light to the square of the velocity with which a material point can describe a circular orbit passing through
.
The following must also be noticed. In the system of polar coordinates used above there will exist in the field without gravitation the stress
. If a stress of this magnitude were produced by means of actions which give rise to a stress-energy-tensor, the passage to rectangular coordinates would give us a stress which becomes infinite at the point
. In those coordinates we should namely have

§ 52. Evidently it would be more satisfactory if we could ascribe a stress-energy-tensor to the gravitation field. Now this can really be done. Indeed, the quantities
determined by (57) form a tensor and according to (58), (79) may be replaced by
![]() |
(85) |
if
is defined by a relation similar to (78), viz.
![]() |
(86) |
Equation (85) shows that, just as well as
, we may consider the quantities
as the stresses etc. in the gravitation field. This way of interpretation is very simple. With a view to (41) we can namely derive from the equations for the gravitation field (65)

and

Further we find from (66)

and from (57) and (86)
![]() |
(87) |
At every point of the field-figure the components of the stress-energy-tensor of the gravitation field would therefore be equal to the corresponding quantities for the matter or the electro-magnetic system with the opposite sign. It is obvious that by this the condition of the conservation of momentum and energy for the whole system would be immediately fulfilled. It was in fact this circumstance that made me think of the tensor
. The way in which
was introduced in §§ 38 and 39 has only been chosen in order to lay stress on (58) being an identity, so that equation (85) is but another form of (79).
At first sight the relations (87) and the conception to which they have led, may look somewhat startling. According to it we should have to imagine that behind the directly observable world with its stresses, energy etc. there is hidden the gravitation field with stresses, energy etc. that are everywhere equal and opposite to the former; evidently this is in agreement with the interchange of momentum and energy which accompanies the action of gravitation. On the way of a light-beam e.g. there would be everywhere in the gravitation field an energy current equal and opposite to the one existing in the beam. If we remember that this hidden energy-current can be fully described mathematically by the quantities
and that only the interchange just mentioned makes it perceptible to us, this mode of viewing the phenomena does not seem unacceptable. At all events we are forcibly led to it if we want to preserve the advantage of a stress-energy-tensor also for the gravitation field. It can namely be shown that a tensor which is transformed in the same way as the tensor
defined by (57) and (86) and which in every system of coordinates has the same divergency as the latter, must coincide with
.
Finally we may remark that (78), (86), (58), (87) give

so that we have, both from (79) and from (85),
.
IV.
(Communicated in the meeting of October 28, 1916).
§ 53. The expressions for the stress-energy-components of the gravitation field found in the preceding paper call for some further remarks. If by
we denote a quantity having the value 1 for
and being 0 for
, those expressions can be written in the form (comp. equations (52) and (78))
![]() |
(88) |
They contain the first and second derivatives of the quantities
. Einstein on the contrary has given values for the stress-energy-components which contain the first derivatives only and which therefore are in many respects much more fit for application.
It will now be shown how we can also find formulae without second derivatives, if we start from (88).
§ 54. For this purpose we shall consider the complex
defined by
![]() |
(89) |
and we shall seek its divergency.
We have

or
![]() |
(90) |
if we put
![]() |
(91) |
Now
can be divided into two parts, the first of which
contains differential coefficients of the quantities
of the first order only, while the second
is a homogeneous linear function of the second derivatives of those quantities. This latter involves that, if we replace (91) by

the second and the third term annul each other. Thus
![]() |
(92) |
If now we define a complex
by the equation
![]() |
(93) |
we have
![]() |
(94) |
If finally we put

we infer from (90) and (94)
![]() |
(95) |
and from (88), (89), (93) and (92)
![]() |
(96) |
and for 
![]() |
(97) |
Formula (95) shows that the quantities
can be taken just as well as the expressions (88) for the stress-energy-components and we see from (96) and (97) that these new expressions contain only the first derivatives of the coefficients
; they are homogeneous quadratic functions of these differential coefficients.
This becomes clear when we remember that
is a function of this kind and that only
contributes something to the second term of (96) and the first of (97); further that the derivatives of
occurring in the following terms contain only the quantities
and not their derivatives.

where for the sake of simplicity it has been assumed that
. Further we have
![\Gamma_{ab}^{c}=-\left\{ \begin{array}{c}
ab\\
c
\end{array}\right\} =-\sum(e)g^{ce}\left[\begin{array}{c}
ab\\
e
\end{array}\right]](http://upload.wikimedia.org/math/5/2/4/524f53ee23cb1079852f42e56a596cef.png)
If now our formulae (96) and (97) are likewise simplified by the assumption
(so that
becomes equal to
), we may expect that
will become identical with
. This is really so in the case
for
; by which it seems very probable that the agreement will exist in general.
In the preceding paper it was shown already that the stress-energy-components
do not form a "tensor", but what was called a "complex". The same may be said of the quantities
defined by (96) and (97) and of the expressions given by Einstein. If we want a stress-energy-tensor, there are only left the quantities
defined by (86) and (57), the values of which are always equal and opposite to the corresponding stress-energy-components
for the matter or the electromagnetic field.
It must be noticed that the four equations

always express the same relations, whether we choose
or
as stress-energy-components
of the gravitation field. If however in a definite case we want to use the equations in order to calculate how the momentum and the energy of the matter and the electromagnetic field change by the gravitational actions, it is best to use
or
, just because these quantities are homogeneous quadratic functions of the derivatives
.
Experience namely teaches us that the gravitation fields occurring in nature may be regarded as feeble, in this sense that the values of the
's are little different from those which might be assumed if no gravitation field existed. For these latter values, which will be called the "normal" ones, we may write in orthogonal coordinates
![]() |
(98) |
In a first approximation, which most times will be sufficient, the deviations of the values of the
's from these normal ones may be taken proportional to the gravitation constant
. This factor also appears in the differential coefficients
; hence, according to the character of the functions
mentioned above (and on account of the factor
in (96) and (97)) these functions become proportional to
, so that in a feeble gravitation field they have low values.
§ 56. Because of the complicated form of equations (96) and (97), we shall confine ourselves to the calculation for some cases of
, i.e. of the energy per unit of volume. This calculation is considerably simplified if we consider stationary fields only. Then all differential coefficients with respect to
vanish, so that we have according to (96)
![]() |
(99) |
We shall work out the calculation, first for a field without gravitation and secondly for the case of an attracting spherical body in which the matter is distributed symmetrically round the centre.
If there is no gravitation field we may take for the quantities
the "normal" values. For the case of orthogonal coordinates these are given by (98). When we want to use the polar coordinates introduced into § 48 we have the corresponding formulae
![]() |
(100) |
If, using polar coordinates, we have to do with an attracting sphere and if we take its centre as origin, we may put
![]() |
(101) |
where
are functions of
. The
's which belong to an orthogonal system of coordinates may be expressed in the same functions.
These
's are

The "etc." means that for
we have similar expressions as for
and for
similar ones as for
.
§ 57. In order to deduce the differential equations determining
we may arbitrarily use rectangular or polar coordinates; the latter however are here to be preferred. If differentiations with respect to
are indicated by accents, we have according to (40) and (101)

for 
So we have found the left hand sides of the field equations (65). Before considering these equations more closely we shall introduce the simplification that the
's, are very little different from the normal values (100). For these latter we have
![]() |
(102) |
and therefore we now put
![]() |
(103) |
The quantities
, which depend on r, will be regarded as infinitely small of the first order and in the field equations we shall neglect quantities of second and higher orders.
Then we may write for
etc.

On the right hand-sides of the field equations (65) we may take for
the normal value; moreover we shall take for
and
the values which hold for a system of incoherent material points. We may do so if we assume no other internal stresses but those caused by the mutual attractions; these stresses may be neglected in the present approximation.
As we supposed the attracting matter to be at rest we have according to (10), (16) and (15) (1915)
,
,
,
,
.

so that of the stress-energy-components of the matter only one is different from zero, namely

Further (66) involves that, also of the quantities
, only one, namely
, is not equal to zero. As we may put
we have namely

Finally we are led to the three differential equations
![]() |
(104) |
![]() |
(105) |
![]() |
(106) |
It may be remarked that
, represents the "mass" present in the element of volume
. Because of the meaning of
(§ 48) the mass in the shell between spheres with radii
and
is found when
is integrated with respect to
between the limits —1 and +1 and with respect to
between 0 and
. As
depends on
only, this latter mass becomes
, so that
is connected with the "density" in the ordinary sense of the word, which will be called
, by the equation

The differential equations also hold outside the sphere if
is put equal to zero. We can first imagine
to change gradually to near the surface and then treat the abrupt change as a limiting case.
In all the preceding considerations we have tacitly supposed the second derivatives of the quantities
to have everywhere finite values. Therefore
and
will be continuous at the surface, even in the case of an abrupt change.
§ 58. Equation (106) gives
![]() |
(107) |
where the integration constant is determined by the consideration that for
all the quantities
and their derivatives must be finite, so that for
the product
must be zero. As it is natural to suppose that at an infinite distance
vanishes, we find further
![]() |
(108) |
The quantities
and
on the contrary are not completely determined by the differential equations. If namely equations (105) and (106) are added to (104) after having been multiplied by
and
respectively, we find
![]() |
(109) |
and it is clear that (104) and (105) are satisfied as soon as this is the case with this condition (109) and with (106). So we have only to attend to (108) and (109). The indefiniteness remaining in
and
is inevitable on account of the covariancy of the field equations. It does not give rise to any difficulties.
Equation (107) teaches us that near the centre

if
is the density at the centre, whereas from (108) we find a finite value for
itself. This confirms what has been said above about the values at the centre. We shall assume that at that point
and their derivatives have likewise finite values. Moreover we suppose (and this agrees with (109)) that
and
are continuous at the surface of the sphere.
If
is the radius of the sphere we find from (108) for an external point

Without contradicting (109) we may assume that at a great distance from the centre
and
are likewise proportional to
, so that
and
decrease proportionally to
.
§ 59. We can now continue the calculation of
(§ 56). Substituting (101) in (99) and using polar coordinates we find

whence by substituting (102) we derive for a field without gravitation

This equation shows that, working with polar coordinates, we should have to ascribe a certain negative value of the energy to a field without gravitation, in such a way (comp. § 57) that the energy in the shell between the spheres described round the origin with radii
and
becomes

The density of the energy in the ordinary sense of the word would be inversely proportional to
, so that it would become infinite at the centre.
It is hardly necessary to remark that, using rectangular coordinates we find a value zero for the same case of a field without gravitation. The normal values of
are then constants and their derivatives vanish.
§ 60. Using rectangular coordinates we shall now indicate the form of
for the field of a spherical body, with the approximation specified in § 57. Thus we put
![]() |
(110) |
By (109) and (110) we find[34]
![]() |
(111) |
Thus we see (comp. § 58) that at a distance from the attracting sphere
decreases proportionally to
. Further it is to be noticed that on account of the indefiniteness pointed out in § 58, there remains some uncertainty as to the distribution of the energy over the space, but that nevertheless the total energy of the gravitation field

has a definite value.
Indeed, by the integration the last terra of (111) vanishes. After multiplication by
this term becomes namely
![(\lambda-\mu)^{2}+2r(\lambda-\mu)(\lambda'-\mu')=\frac{d}{dr}\left[r(\lambda-\mu)^{2}\right]](http://upload.wikimedia.org/math/3/5/9/35997934cf72a253f31b149131f84e84.png)
The integral of this expression is 0 because (comp. §§ 57 and 58)
is continuous at the surface of the sphere and vanishes both for
and for
.
We have thus
![]() |
(112) |
where the value (107) can be substituted for
. If e.g. the density
is everywhere the same all over the sphere, we have at an internal point

and at an external point

From this we find

§ 61. The general equation (99) found for
can be transformed in a simple way. We have namely

and we may write
(§ 54) for the last term. Hence
![]() |
(113) |
where we must give the values 1, 2, 3 to
and
.
The gravitation energy lying within a closed surface consists therefore of two parts, the first of which is
![]() |
(114) |
while the second can be represented by surface integrals. If namely
are the direction constants of the normal drawn outward
![]() |
(115) |
In the case of the infinitely feeble gravitation field represented by
(§ 57) both expressions
and
contain quantities of the first order, but it can easily be verified that these cancel each other in the sum, so that, as we knew already, the total energy is of the second order.
From
and the equations of § 32 we find namely
![]() |
(116) |
so that we can write
![]() |
The factor
is of the first order. Thus, if we confine ourselves to that order, we may take for all the other quantities these normal values. Many of these are zero and we find
![]() |
(117) |
Here we must take
;
, while we remark that for
the expression between brackets vanishes. For
the integral becomes
do, which after summation with respect to
gives
![]() |
(118) |
representing the normal to the surface. If
and
differ from each other, while neither of them is equal to 4, we can deduce from (110) and (109)

occurring twice, i.e. combined with the two values different from
which
can take, we have in addition to (118)

so that (117) becomes

As now outside the sphere

we have for every closed surface that does not surround the sphere
, but for every surface that does
![]() |
(119) |
As to
we remark that substituting (65) in (41) and taking into consideration (64) we find,
![]() |
(120) |
From this we conclude that
is zero if there is no matter inside the surface
. In order to determine
in the opposite case, we remember that
is independent of the choice of coordinates. To calculate this quantity we may therefore use the value of
indicated in § 56, which is sufficient to calculate
as far as the terms of the first order. We have therefore

and if, using further on rectangular coordinates, we take for
the normal value
,

From this we find by substitution in (114) for the case of the closed surface a surrounding the sphere

This equation together with (119) shows that in (113) when integrated over the whole space the terms of the first order really cancel each other. In order to calculate those of the second order and thus to derive the result (112) from (113), we should have to determine the quantity
(comp. 120)), accurately to the order
. The surface integrals in (115) too would have to be considered more closely. We shall not however dwell upon this.
§ 62. From the expression for
given in (113) and the value

derived from it, it can be inferred that, though
is no tensor, we yet may change a good deal in the system of coordinates in which the phenomena are described, without altering the value of the total energy. Let us suppose e.g. that
is left unchanged but that, instead of the rectangular coordinates
hitherto used, other quantities
are introduced, which are some continuous function of
, with the restriction that
outside a certain closed surface surrounding the attracting matter at a sufficient distance. If we use these new coordinates, we shall have to introduce other quantities
instead of
however outside the closed surface the quantities
and their derivatives do not change, the value of
will approach the same limit as when we used the coordinates
, if the surface
for which it is calculated expands indefinitely. The value which we find for
after the transformation of coordinates will also be the same as before. Indeed, if
is an element of volume expressed in
-units and
the same element expressed in
-units, while
represents the new value of
, we have

It is clear that the total energy will also remain unchanged if
differ from
at all points, provided only that these differences decrease so rapidly with increasing distance from the attracting body, that they have no influence on the limit of the expression (115).
The result which we have now found admits of another interpretation. In the mode of description which we first followed (using
),
[35]) and
are certain functions of
; in the new one
,
are certain other functions of
. If now, without leaving the system of coordinates
, we ascribe to the density and to the gravitation potentials values which depend on
, in the same way as
,
depended on
just now, we shall obtain a new system (consisting of the attracting body and the gravitation field) which is different from the original system because other functions of the coordinates occur in it, but which nevertheless no observation will be able to discern from it, the indefiniteness which is a necessary consequence of the covariancy of the field equations, again presenting itself.
What has been said shows that the total gravitation energy in this new system will have the same value as in the original one, as has been found already in § 60 with the restrictions then introduced.
§ 63. If
were a tensor, we should have for all substitutions the transformation formulae given at the end of § 40. In reality this is not the case now, but from (96) and (97) we can still deduce that those formulae hold for linear substitutions. They may likewise be applied to the stress-energy-components of the matter or of an electromagnetic system. Hence, if
represents the total stress-energy-components, i. e. quantities in which the corresponding components for the gravitation field, the matter and the electromagnetic field are taken together, we have for any linear transformation
![]() |
(121) |
We shall apply this to the case of a relativity transformation, which can be represented by the equations
![]() |
(122) |
with the relation
![]() |
(123) |
In doing so we shall assume that the system, when described in the rectangular coordinates
and with respect to the time
, is in a stationary state and at rest.

which means that in the system
there are neither momenta nor energy currents in the gravitation field.
We may assume the same for the matter, so that we have for the total stress-energy-components in the system 

Let us now consider especially the components
and
in the system
For these we find from (121) and (122)
![]() |
(124) |
![]() |
(125) |
It is thus seen in the first place that between the momentum in the direction of
and the energy-current in that direction
there exists the relation

well known from the theory of relativity.
Further we have for the total energy in the system 

where the integration has to be performed for a definite value of the time
. On account of (122) we may write for this

where we have to keep in view a definite value of the time
.
If the value (125) is substituted here and if we take into consideration that, the state being stationary in the system
,

we have

if
is the energy ascribed to the system in the coordinates
. By integration of the first of the expressions (124) we find in the same way for the total momentum in the direction of 

§ 64. Equations (122) show that in the coordinates
the system has a velocity of translation
in the direction of
. If this velocity is denoted by
, we have according to (123)

If therefore we put

we find
![]() |
(126) |
When the system moves as a whole we may therefore ascribe to it an energy and a momentum which depend on the velocity of translation in the way known from the theory of relativity. The quantity
, to which the energy of the gravitation field also contributes a certain part, may be called the "mass" of the system. From what has been said in § 62 it follows that within certain limits it depends on the way in which the system and the gravitation field are described.
It must be remarked however that, if for the gravitation field we had chosen the stress-energy-tensor
(§ 52), the total energy of the system even when in motion would be zero. The same would be true of the total momentum and we should have to put
.
At first sight it may seem strange that we may arbitrarily ascribe to the moving system the momentum determined by (126) or a momentum 0; one might be inclined to think that, when a definite system of coordinates has been chosen, the momentum must have a definite value, which might be determined by an experiment in which the system is brought to rest by "external" forces. We must remember however (comp. § 52) that in the theory of gravitation we may introduce no "external" forces without considering also the material system
in which they originate. This system
together with the system
with which we were originally concerned, will form an entity, in which there is a gravitation field, part of which is due to
(and a part also to the simultaneous existence of
and
). There is no doubt that we may apply the above considerations to the total system (
) without being led into contradiction with any observation.
- ↑ A. Einstein, Zur allgemeinen Relativitätstheorie, Berliner Sitzungsberichte 1915, pp. 778 799; Die Feldgleichungen der Gravitation, ibid. 1915, p. 844.
- ↑ D. Hilbert, Die Grundlagen der Physik I, Göttinger Nachrichten, Math.-phys. Klasse, Nov. 1915.
- ↑ It will be known that in the theory of relativity Minkowski was the first who used this geometric representation in an extension of four dimensions. The name "world-line" has been borrowed from him.
- ↑ For the sake of simplicity we shall imagine the two motions not to be disturbed by this coincidence, so that e.g. two material points penetrate each other or pass each other at an extremely small distance without any mutual influence.
- ↑ In a correspondence I had with him.
- ↑ In other terms, that the data procured by astronomical observations can be extended arbitrarily and unboundedly.
- ↑ A "surface" determined by one equation between the coordinates is a three-dimensional extension. It will cause no confusion if sometimes we apply the name of "plane" to certain two-dimensional extensions, if we speak e.g. of the "plane" determined by two line-elements.
- ↑ This corresponds to the negative value which (1) gives for
. - ↑ For a radius-vector on the asymptotic cone we may take either of these values; this makes no difference, as the numerical value of a line-element in the direction of such a radius-vector becomes 0 in both cases.
- ↑ This agrees with the value of the Lagrangian function, which is to be found e.g. in my paper on "Hamilton's principle in Einstein's theory of gravitation." These Proceedings 19 (1916). p. 751.
- ↑ If, according to circumstances, different signs arc given to
, the angle whose sine occurs in the formula for the area of a parallelogram must be understood to be positive in one case and negative in the other. - ↑ From § 10 it follows that if the length of a vector
that is represented by a line (§ 17) coincides with a radius-vector of the conjugate indicatrix, it is always represented by an imaginary number. We may however obtain a vector which in natural units is represented by a real number e.g. by 1 (§ 13) if we multiply the vector
by an imaginary factor, which means that its components and also those of a vector product in which it occurs are multiplied by that factor. - ↑ In the above considerations difficulties might arise if the vector
lay on the asymptotic cone of the indicatrix, our definition of a vector of the value 1 would then fail (comp. note 2, p. 1345). With a view to this we can choose the form of the extension
(§ 13) in such a way that this case does not occur, a restriction leading to a boundary with sharp edges. - ↑ Zittingsverslag Akad. Amsterdam, 23 (1915), p. 1073; translated in Proceedings Amsterdam, 19 (1910), p. 751. Further on this last paper will be cited by l. c.
- ↑ Comp. § 7, l. c.
- ↑ For the infinitesimal quantities
occurring in (19) we have namely (comp. (30))

and taking into consideration (19) and (20), i e.

and formula (7) l. c, we may write (comp. note 2, p. 758, l. c.)

- ↑ Put
. Then we have

and similar formulae for the other three parts of (25).
- ↑ Comp. (28) l. c.
- ↑ Published September 1916, a revision having been found desirable.
- ↑ See Proceedings Vol. XIX, p. 1341 and 1354.
- ↑ Namely:

The symbol
denotes the complex of all the quantities
. - ↑ Namely:

- ↑ On account of the relation

- ↑ Similarly:

- ↑ This means that the transformation formulae for these quantities have the form

See for the notations used here and for some others to be used later on my communication in Zittingsverslag Akad Amsterdam 23 (1915), p. 1073 (translated in Proceedings Amsterdam 19 (1916), p. 751). In referring to the equations and the articles of this paper I shall add the indication 1915.
- ↑ Suppose that at the boundary of the domain of integration
and
. Then we have also
and
, so that

and from

we infer

As this must hold for every choice of the variations
(by which choice the variations
are determined too) we must have at each point of the field-figure
- ↑ This may be made clear by a reasoning similar to that used in the preceding note. We again suppose
and
to be zero at the boundary of the domain of integration. Then
and
vanish too at the boundary, so that

From

we may therefore conclude that

As this must hold for arbitrarily chosen variations
we have the equation
- ↑ Einstein uses the word "divergency" in a somewhat different sense. It seemed desirable however to have a name for the left hand side of (54) and it was difficult to find a better one.
- ↑ This has also been done by de Donder, Zittingsverslag Akad. Amsterdam, 35 (1916), p. 153.
- ↑ The notations
and
(see (27), (29) and § 11, 1915), will however be preserved though they do not correspond to those of Einstein. As to formulae (59) and (60) it is to be understood that if
and
are two of the numbers 1, 2, 3, 4,
and
denote the other two in such a way that the order
is obtained from 1 2 3 4 by an even number of permutations of two ciphers.
If
are replaced by
and if for the stresses the usual notations
, etc., are used (so that e.g. for a surface element
perpendicular to the axis of
is the first component of the force per unit of surface which the part of the system situated on the positive side of
exerts on the opposite part) then
, etc. Further
are the components of the momentum per unit of volume and
the components of the energy-current. Finally
is the energy per unit of volume. - ↑ The quantities
in that equation are the same as those which are now denoted by
. - ↑ In the cases considered in § 43,
can indeed be represented in this way. - ↑ To make the notation agree with that of § 38
has been replaced by
. - ↑ Of the laborious calculation it may be remarked here only that it is convenient to write the values (110) in the form


where
and
are infinitesimal functions of
. We then find![\begin{array}{l}
\mathfrak{t}_{4}^{'4}=\frac{c}{2\varkappa}\left\{ -\frac{1}{2}\sum(a)\left(\frac{\partial\alpha}{\partial x_{a}}\right)^{2}+\sum(a)\frac{\partial\nu}{\partial x_{a}}\frac{\partial\alpha}{\partial x_{a}}+\right.\\
\\
\qquad\left.+\frac{1}{4}\sum(aik)\left[\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{i}^{2}}\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{k}^{2}}-\left(\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{i}\partial x_{k}}\right)^{2}\right]\right\} \\
\\
\qquad\qquad(a,i,k=1,2,3)
\end{array}](//upload.wikimedia.org/math/8/4/5/84551bc6317ded6c3851ea9a8c0a272b.png)
which reduces to (111) if the relations between
and
, viz.
and the equality
involved in (109) are taken into consideration. - ↑ By
we mean here what was denoted by
in § 56. - ↑ We have
, while all the other quantities gab are independent of
. Thus we can say that the quantities
and
are equal to zero when among their indices the number 4 occurs an odd number of times. The same may be said of
,
,
(according to (116)),
and also of products of two or more of such quantities. As in the last two terms of (97) the indices
and
occur twice, these terms will vanish when only one of the indices
and
has the value 4. As to the first term of (97) we remark that, according to the formulae of § 32, each of the indices
and
occurs only once in the differential coefficient of
with respect to
, while other indices are repeated. As to the number of times which
and the other indices occur we can therefore say the same of the first term of (97) as of the other terms. The first term also is therefore zero, if no more than one of the two indices
and
has the value 4.
That
vanishes for
is seen immediately.
| This work is in the public domain in the United States because it was published before January 1, 1923.
The author died in 1928, so this work is also in the public domain in countries and areas where the copyright term is the author's life plus 80 years or less. This work may also be in the public domain in countries and areas with longer native copyright terms that apply the rule of the shorter term to foreign works. |









![\int\left\{ \left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]\right\} _{x}d\sigma=i\int\{\mathrm{q}\}_{x}d\Omega](http://upload.wikimedia.org/math/a/6/2/a629cc2a29e0fe5ca7a1da6ffe99359f.png)




![\int\left[\mathrm{R}_{e}\cdot\mathrm{N}\right]_{x}d\sigma](http://upload.wikimedia.org/math/f/f/c/ffc2dbec8944c535e07058556e5555a0.png)





![\left[\mathrm{B}_{a^{*}}\cdot\mathrm{B}_{b^{*}}\right]=\left[\mathrm{A}_{a^{*}}^{I}\cdot\mathrm{A}_{b^{*}}^{II}\right]-\left[\mathrm{A}_{a^{*}}^{II}\cdot\mathrm{A}_{b^{*}}^{I}\right]+\left[\mathrm{A}_{a^{*}}^{III}\cdot\mathrm{A}_{b^{*}}^{IV}\right]-\left[\mathrm{A}_{a^{*}}^{IV}\cdot\mathrm{A}_{b^{*}}^{III}\right]](http://upload.wikimedia.org/math/6/a/7/6a7e9c25636ea10c527763c372cca303.png)
![\left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]=\sum(\overline{ab})\left[\mathrm{B}_{a^{*}}\cdot\mathrm{B}_{b^{*}}\cdot\mathrm{N}\right]](http://upload.wikimedia.org/math/8/c/0/8c0b3a9ae76a81e3eb3447c1282b3732.png)









![\int\left\{ \left[\mathrm{R}_{e}\cdot\mathrm{N}\right]+\left[\mathrm{R}_{h}\cdot\mathrm{N}\right]\right\} _{x'}d\sigma=i\int\{\mathrm{q}\}_{x'}d\Omega](http://upload.wikimedia.org/math/2/9/2/2927e12ccd044752c4968baccba56d9f.png)















































































![\mathfrak{t}_{4}^{'4}=\frac{c}{2\varkappa}\left\{ \nu'^{2}+\frac{1}{r}(\lambda-\mu)\left[\frac{1}{r}(\lambda-\mu)+2(\lambda'-\mu')\right]\right\}](http://upload.wikimedia.org/math/0/c/9/0c9f309841b319c61416e3343d990353.png)
















.
occurring in (19) we have namely (comp. (30))


. Then we have

denotes the complex of all the quantities 



and
. Then we have also
and
, so that


are determined too) we must have at each point of the field-figure
and
vanish too at the boundary, so that



and
are two of the numbers 1, 2, 3, 4,
and
denote the other two in such a way that the order
is obtained from 1 2 3 4 by an even number of permutations of two ciphers.
and if for the stresses the usual notations
, etc., are used (so that e.g. for a surface element
is the first component of the force per unit of surface which the part of the system situated on the positive side of
, etc. Further
are the components of the momentum per unit of volume and
the components of the energy-current. Finally 

are infinitesimal functions of ![\begin{array}{l}
\mathfrak{t}_{4}^{'4}=\frac{c}{2\varkappa}\left\{ -\frac{1}{2}\sum(a)\left(\frac{\partial\alpha}{\partial x_{a}}\right)^{2}+\sum(a)\frac{\partial\nu}{\partial x_{a}}\frac{\partial\alpha}{\partial x_{a}}+\right.\\
\\
\qquad\left.+\frac{1}{4}\sum(aik)\left[\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{i}^{2}}\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{k}^{2}}-\left(\frac{\partial^{3}\beta}{\partial x_{a}\partial x_{i}\partial x_{k}}\right)^{2}\right]\right\} \\
\\
\qquad\qquad(a,i,k=1,2,3)
\end{array}](http://upload.wikimedia.org/math/8/4/5/84551bc6317ded6c3851ea9a8c0a272b.png)
and
, viz.
involved in (109) are taken into consideration.
, while all the other quantities gab are independent of
,
(according to (116)),
and also of products of two or more of such quantities. As in the last two terms of (97) the indices
has the value 4. As to the first term of (97) we remark that, according to the formulae of § 32, each of the indices
and the other indices occur we can therefore say the same of the first term of (97) as of the other terms. The first term also is therefore zero, if no more than one of the two indices
vanishes for
is seen immediately.