Appendix D: Analysis of Geodesic Equations

            This appendix supplements Chapter 4, which discusses the application of the geodesic equations to the Yilmaz theory. The following summarizes the material in this appendix.         

            Section D.1 gives the general formula for the geodesic equations. It derives from this the general formulas for the second derivatives in spherical coordinates that correspond to a static, spherically symmetric gravitational field. Section D.2 applies the results of Section D.1 to the Yilmaz theory. It calculates the four specific formulas for the second derivatives in polar coordinates for the Yilmaz solution of a single star and the Yilmaz cosmology model. Section D.3 shows that the geodesic equation for time can be solved directly. Hence, the geodesic equations relative to time are expressed in terms of the first derivative of time.

            Section D.4 derives formulas for the geodesic equations of the general static Yilmaz theory expressed in rectangular coordinates. Since these equations do not require a gravitational field with spherical symmetry, they can be applied to multi-body applications. For example, they can be used to calculate the accurate orbits of planets and other bodies in our solar system.

              Within our solar system, the derivative dt/ds along a geodesic trajectory can be very accurately approximated by considering only the gravitational field produced by the sun. The reason for this is that dt/ds is very close to unity. By applying this approximation to the geodesic equations derived in Section D.4, much simpler geodesic equations are derived in Section D.5 that can be used to calculate the orbits of bodies in our solar system.

  D.1 Geodesic Equations for a Static, Spherically Symmetric Gravitational Field

            This section considers the general formula that specifies the geodesic equations. It derives from this the four geodesic equations in spherical coordinates that apply to a static, spherically symmetric gravitational field. These four equations specify the second derivatives of the four space-time variables in spherical coordinates (t, R, q, y), where these derivatives are with respect to differential motion ds along the path of the body.

            The general formula for the geodesic equations is given as follows by Tolman [2] (p. 495, Eq. 20):

            d2xa/ds2  =  -  Sm Sn Gmna um un           (D-1)

  where the variable um represents the following derivativ

            um  =  dxm/ds                                                               (D-2)

The two summations shown in Eq. D-1 are not stated implicitly in Tolman's equation. However, they are implied, because the indices m and n are repeated. We will solve Eq. D-1 for values of the index a equal to 0, 1, 2, 3.

Table D-1: Non-zero Christoffel Symbols for Static, Spherically Symmetric Gravitational Fiel

G010  =  G100                        G221                                 G332
G
001                                      G331                        G313  =  G133
G
111                              G212  =  G122                  G323  =  G233     

       Table D-1 lists the non-zero Christoffel symbols when the gravitational field is static and spherically symmetric. The following discussion applies this information to Eq. D-1, and derives the four geodesic equations for this case. When one considers only the Christoffel symbols given in Table D-1, the Geodesic formula of Eq. D-1 yields the following equations when the index a is set equal to 0, 1, 2, 3:                                                          

d2x0/ds2  =  - {  G100 u1 u0 + G010 u0 u1 }                                  (D-3)

d2x1/ds2  =  - {G001u0u0 + G111u1u1 + G221u2u2 + G331u3u3}    (D-4)

d2x2/ds2  =  - {  G122 u1u2 + G212 u2 u1 + G332 u3 u3 }             (D-5)

d2x3/ds2  =  - ( G133u1u3 + G313u3u1 + G233u2u3 + G323u3u2}   (D-6)

In Eqs. D-1 to D-6, apply the equality relations for the Christoffel symbols given in Table D-1 and combine terms. This yiel

  d2x0/ds2  =  - 2 G010 u0u1                                                       (D-7)

  d2x1/ds2  =  - G001 (u0)2 - G111(u1)2 - G221(u2)2 - G331(u3)2  (D-8)

    d2x2/ds2  =  - 2 G122 u1u2 - G332 (u3)2                                (D-9)

     d2x3/ds2  =  - 2 G133 u1 u3 - 2 G233 u2 u3                          (D-10)

             Replace the generic xm coordinates by the following specific names for the spherical coordinates:

            x0  =  t,  x1  =  r,  x2  =  q,  x3  =  y                           (D-11)

In accordance with Eq. D-2, replace the um variables by the following

            u0  =  dx0/ds  =  dt/ds                                                 (D-12)

            u1  =  dx1/ds  =  dr/ds                                                  (D-13)

            u2  =  dx2/ds  =  dq/ds                                                 (D-14)

            u3  =  dx3/ds  =  dy/ds                                                 (D-15)

Equations D-7 to D-10 become

d2t/ds2  =  - 2 G010 (dt/ds) (dr/ds)                                           (D-16) 

d2r/ds2  =  - G001 (dt/ds)2 - G111(dr/ds)2 - G221(dq/ds)2 - G331(dy/ds)2 

                                                                                             (D-17)

  d2q/ds2  =  - 2 G122 (dr/ds) (dq/ds) - G332 (dy/ds)2               (D-18)

d2y/ds2  =  - 2 G133 (dr/ds)(dy/ds) - 2 G233 (dq/ds)(dy/ds)      (D-19)

These are the general expressions for the geodesic equations in spherical coordinates for a static spherically symmetric gravitational field.

D.2 Geodesic Equations for Spherically Symmetric Applications of Yilmaz Theory

            Let us apply these geodesic equations to the Yilmaz theory. Table D-2 gives the formulas for the Christoffel symbols of the Yilmaz theory that apply to a static, spherically symmetric gravitational field, which were obtained from Table B-2 of Appendix B. Applying these values to Eqs. D-16 to D-19 gives the following geodesic equations:

d2t/ds2  =  2 1f (dt/ds) (dr/ds)                                      (D-20) 

d2r/ds2  =  e-4f 1f (dt/ds)2 - 1f (dr/ds)2 + r2(1f + 1/r)(dq/ds)2

+ r2 sin2q(1f + 1/r)(dy/ds)2                               (D-21)

d2q/ds2  =  - 2 (1f + 1/r)(dr/ds) (dq/ds) + sinq cosq (dy/ds)2   

                                                            (D-22)

d2y/ds2  =  - 2 (1f + 1/r] (dr/ds) (dy/ds)

- 2 cot q (dq/ds) (dy/ds)             (D-23)  

Table D-2: General formulas for Christoffel Symbols of the Yilmaz theory, for a static, spherically symmetric gravitational field

Symbol     Formula                        Symbol           Formula                       

G001      - e-4f 1f                  G010 = G100      - 1f 
G111      1f                              G212  =  G122      (1f + 1/r)
G221      - r2(1f + 1/r)              G313  =  G133      (1f + 1/r) 
G331      - r2 sin2q(1f + 1/r]      G323  =  G233      cot q
G332      - sinq cosq

            These geodesic equations can be simplified by replacing the differential angular variables by differential linear displacements in the q and y directions, which are denoted dxq and dxy and are equal to

            dxq  =  r dq                                               (D-24) 

            dxy  =  r sinq dy                                       (D-25) 

  Differentiating these gives the following second derivatives

d2xq  =  d(dxq)  =  r d2q  + dr dq                            (D-26)

d2xy  =  d(dxy)

         =  r sinq d2y  + sinq dr dy + r cosq dq dy       (D-27)  

Solving Eq. D-26 for (r d2q) give

r d2q  =  d2xq - dr dq  =  d2xq - (1/r)dr (rdq)

          =  d2xq - (1/r) dr dxq                                  (D-28)

Solving Eq. D-27 for (r sinq d2y) gives

r sinq d2y  =  d2xy - sin q dr dy - r cos q dq dy                   

       =  d2xy - (1/r) dr (r sin q dy) - (1/r) cot q (r dq)(r sin q dy)  

       =  d2xy - (1/r) dr dxy - (1/r) cot q dxq dxy                   (D-29)

Let us use these relations to simplify the geodesic equations. Applying Eqs D-24, D-25 to Eq. D-21 gives

d2r/ds2  =  e-4f 1f (dt/ds)2 - 1f (dr/ds)2

+ (1f + 1/r) { (rdq/ds)2 + (r sin q dy/ds)2  }          (D-30)

   =  e-4f 1f(dt/ds)2 - 1f (dr/ds)2 + (1f + 1/r)(dxq/ds)2 + (dxy/ds)2}

Multiply Eq. D-22 by r:                                 (D-31)    

r d2q/ds2  =  - 2 (1f + 1/r)(dr/ds) (r dq/ds)  + (1/r) cot q (r sin q dy/ds)2

Applying Eqs. D-24, D-25, D-28 to this gives

d2xq/ds2 - (1/r)(dr/ds)(dxq/ds) 

         =  - 2 (1f + 1/r)(dr/ds)(dxq/ds) + (1/r) cot q (dxy/ds)2   (D-32)

  Solving for d2xq/ds2 gives

d2xq/ds2  =  - (2 1f + 1/r)(dr/ds)(dxq/ds) + (1/r) cot q (dxy/ds)2   (D-33)

Multiply Eq. D-23 by (r sin q):

(r sin q)(d2y/ds2)  =  - 2 (1f + 1/r] (dr/ds) (r sin q dy/ds)  

- (2/r) cot q (r dq/ds) (r sin q dy/ds)                          (D-34)

Applying Eqs. D-24, D-25, D-29 to this gives

d2xy/ds2 - (1/r) (dr/ds)(dxy/ds)  - (1/r) cot q (dxq/ds)(dxy/ds)  (D-35)

            =  - 2 (1f + 1/r] (dr/ds) (dxy/ds) - (2/r) cot q (dxq/ds) (dxy/ds)

Solving for d2xy/ds2 gives                                       (D-36)

d2xy/ds2  =  - (21f + 1/r] (dr/ds) (dxy/ds) - (1/r) cot q (dxq/ds) (dxy/ds)

         Further simplification of the geodesic equations is achieved by expressing the differential linear displacements in the q and y directions (dxq, dxy) by the total differential tangential displacement, which is denoted dxt, and is given by

            (dxt)2  =  (dxq)2 + (dxq)2                       (D-37)

Differentiating this gives

dxt d2xt  =  dxq d2xq + dxy d2xy               (D-38)