Post by Luigi FortunatiA gelatin sphere in remote space, far from any gravitational field,
maintains its spherical shape because it is in an inertial reference
frame where there are no forces that can deform it.
But if the gelatin sphere approaches a planet or a star and falls free,
it gets longer, it ovalizes.
Is this deformation of the gelatin sphere in free fall in a
gravitational field due to the action of a force or not?
There are two ways of looking at this. The Newtonian view is there is a
difference if the gravitational force across the sphere of
material. There is then a difference of force between the antipodal
points given be F - F' = -GMm(1/r^2 - 1/r'^2). Now let r' = r + d, for d
the diameter of the sphere and so using an approximation we get
F - F' = -2GMmd/r^3.
This is treated as a force.
In general relativity we have a somewhat different perspective. The geodesic equation
d^2r/ds^2 + G^r_{ab}U^aU^b = 0 ---> G^r_{ab} Christoffel symbol.
In a weak gravity field has the proper time s ~= t and U^t ~= 1 while
all other spatial U^i ~= 0. So this leads to
d^2r/ds^2 + GM/r^2 = 0,
for the Christoffel symbol of the Schwarzschild metric. This however is
considered a bit of an illusion, for the geodesic equation is a
connection coefficient based equation that is not covariant. It turns
out to give the Newtonian result in a weak spherically symmetric
case. To get the difference in force across the sphere we need to
consider the geodesic deviation equation
dU^a/ds + R^a_{bcd}U^bV^cU^c = 0.
I have to cut across stuff, for this editor is not convenient. The V^c
is the vector separating two test masses, which we take to be the
diameter, and the velocity vectors U^a have only U^t ~= 1 and we then
recover
dU^a/ds + 2GMmd/r^3 = 0.
This is the same math result, but from the interpretation of there being
a separation of neighboring geodesic flows.
The real force involved is the material resistance to this tidal
acceleration. In general relativity gravitation is not a real force. A
spring folding two masses will be distended by the different geodesic
flows. We call this the tidal acceleration or force, but really any
force involved is a resistance to this geodesic separation.