Gravitational Field in a Cavity

Back to Physics World
Back to General Relativity


Consider a sphere of uniform mass density r shown below

It is well known that the gravitational acceleration field g1= g(r1) within the sphere is given by

The field is determined at the displacement r1 measured from the center of the sphere. Consider now a spherical region contained entirely within the sphere above. Let the displacement of the center of this region from the center of the sphere be d. The gravitational field g2 = g(r2) due just to this region is

where the field is determined within the region at the displacement r2 measured from the center of the region. That is r1 = r2 + d (note d = R j = constant).

Note: r1 and r2 have different origins.

Next let the spherical region be subtracted from the sphere to form a cavity. The resulting gravitational field g at any point within the cavity at the displacement r1 is

where F = gz + constant, g = (4/3)pGrR.

This same result could have been obtained by integration of over the source, i.e. sphere with uniform mass density r with a cavity. In situations when the sources of gravity are static and the gravitational field weak enough such that objects cannot accelerate to relativistic velocities the gravitational field may be approximated to a high degree of accuracy using the so-called weak field limit. In this case the gravitational field in a cavity will be highly uniform. However the situation is more complicated since spherical cavity will not have a well-defined meaning. It can be shown [1] that in this approximation the integral for the Newtonian potential is the same as it is in Newtonian gravity, where the mass density r is now the rest mass density. The variables of integration are more akin to "addresses" rather than to "distances" as they were in Newtonian gravity. These "addresses" serve to label the spatial co-ordinates of the sources. The Newtonian potential in the weak field limit will still be F = gz + constant. Such a distribution of mass is finite and thus represents a realistic source in general relativity for a uniform gravitational field to a high degree of accuracy.


References

[1] Gravitation, Charles. W. Misner, Kip S. Thorne, John Archibald Wheeler, (1973), sect 6.6.


Back to General Relativity
Back to Physics World

Hosted by www.Geocities.ws

1