A.T. said:
That is just a very complicated way to say that the proper acceleration of a clock resting in the center is zero. This is less than the proper acceleration of a clock resting on the surface. Yet the center clock runs slower than the surface clock.
Start with the Schwarzschild solution in the weak field approximation:
[tex](cd\tau)^2=(1-\frac{2\Phi}{c^2})(cdt)^2+(1-\frac{2\Phi}{c^2})^{-1}(dr)^2+...[/tex]
For the case [tex]dr=d\theta=d\phi=0[/tex] you get the well known relationship:
[tex]d\tau=\sqrt{1-\frac{2\Phi}{c^2}}dt[/tex]
Writing the above for two different gravitational potentials [tex]\Phi_1[/tex] and [tex]\Phi_2[/tex] you obtain the well-known time dilation relationship:
[tex]\frac{d\tau_1}{d\tau_2}=\sqrt{\frac{1-\frac{2\Phi_1}{c^2}}{1-\frac{2\Phi_2}{c^2}}}[/tex]
At the Earth surface :
[tex]\Phi_1=-\frac{GM}{R}[/tex]
At the Earth center:
[tex]\Phi_2=-3/2\frac{GM}{R}[/tex]
Now, due to the fact that [tex]\frac{\Phi}{c^2}<<1[/tex] you can obtain the approximation:
[tex]\frac{d\tau_1}{d\tau_2}=1-\frac{\Phi_1-\Phi_2}{c^2}=1-\frac{GM}{2Rc^2}<1[/tex]
So, [tex]f_1>f_2[/tex] where [tex]f_1[/tex] is the clock frequency on the Earth crust and [tex]f_2[/tex] is the frequency of the clock at the center of the Earth.
In addition, the time dilation depends on the difference in the gravitational field [tex]\Phi_1-\Phi_2[/tex].
Generalization:
At a distance [tex]r<R[/tex] from the center of the sphere, inside the sphere, the gravitational potential is:
[tex]\Phi_2(r)=-\frac{GM}{R}(\frac{3}{2}-\frac{r^2}{2R^2})[/tex]
The above gives:
[tex]\frac{d\tau_1}{d\tau_2}=1-\frac{\Phi_1-\Phi_2}{c^2}=1-\frac{GM}{2Rc^2}(1-\frac{r^2}{R^2})<1[/tex]
For [tex]r=0[/tex] (clock2 at the center of the Earth) you recover the results from above.
For [tex]r=R[/tex] you get the expected:
[tex]\frac{d\tau_1}{d\tau_2}=1[/tex]