A few pointers
lightarrow said:
Inside a spherical cavity centered at the Earth's centre, the space-time curvature is 0 or =/= 0?
I know Newtonian gravitational field is omogeneously 0, so no field variation, but does GR give a different answer?
This was going to be an exercise in the "What is the Theory of Elasticity?" thread, which seems to have died for lack of interest. Some brief pointers:
1. The case of a thin uniform spherical shell in the
weak-field approximation is treated in many places, e.g. the problem book by Lightman et al. The field vanishes inside such a shell, but this gets quite tricky if the shell is "rotating".
2. The interior of a massive object is most often modeled in gtr as a perfect fluid, and the static spherically symmetric perfect fluids are not only known but a rare example of a well understood portion of the solution space of the EFE! The simplest model is the Schwarzschild constant density fluid ball; but the Tolman IV fluid is probably even better example. Qualitatively:
a. The pressure and density are maximal at the center and decrease monotonically as radius increases, with pressure falling to zero at the surface of the fluid ball (where we can match to a Schwarzschild vacuum exterior solution).
b. The acceleration of bits of fluid vanishes at the center (as must happen by symmetry), and depending on boundary conditions may reach a maximum under the surface (this happens for parameters appropriate for neutron star models).
c. The tidal tensor components are maximal (and positive) at the center and the tensor is in fact diagonal there (wrt any reasonable frame field). The components fall of as r increases, but E_{11} decays faster than E_{22}, \, E_{33} and may even go negative before reaching the surface (again, this happens for parameters appropriate for neutron star models).
d. Similar remarks hold for the three-dimensional Riemann tensor of the spatial hyperslices orthogonal to the world lines of the fluid elements. Put more vividly, near the center, the orthogonal hyperslice always resembles a three-spherical "cap" (see the pictures in MTW, which illustrate the Schwarzschild fluid, where each slice is locally isometric to S^3 everywhere).
e. The minimal radius for a static spherically symmetric fluid ball is r=9/4 \, m, i.e. larger than r=2m (Buchdahl's theorem).
3. A perfect fluid cannot sustain a cavity at the center of a spherically symmetric body. However, an elastic solid can do so. A slight modification of an example I gave in the "What is the Theory of Elasticity?" thread gives the displacements and stresses for the exact solution in Newtonian elastostatics which models an spherically symmetric body with a spherical cavity at the ceenter which is made of an isotropic homogeneous material, such as steel. If I ever take up that thread again, at some point I'd get to weak-field approximation and then fully nonlinear elasticity. Static spherically symmetric elastic bodies are one of the few examples which can be treated fairly readily. The basic features of the stress tensor are similar to the above.
4. It is possible to create simple models of collapsing dusts with (shrinking) spherical cavities using the FRW dusts, or more generally the LTB dusts. The Carter-Penrose diagrams exhibiting the conformal structrure of such solutions possesses some interesting features.
Even in Newtonian theory, it is not so easy to generalize this to an oblate spheroid with centrifugal forces. In fact, it is not so easy to find the interior or exterior potentials of a homogeneous ellipsoidal solid. (The exact solutions can be given in terms of elliptic functions, but this apparently wasn't done explicitly until long after Newton! However, Newton did know the potential inside a homogeneous density thin ellipsoidal shell, which I'll let curious students puzzle over.) Nor is it trivial to investigate the stability of a rotating perfect fluid body even in Newtonian theory, with hydrostatic forces in static equilibrium with centrifugal "forces". (McLaurin and Jacobi discovered that there is an interesting sequence of sudden changes as the angular velocity increases.)