hellfire said:
I realize now you were not talking about R00, but about R1010, and R00 = R1010 + R2020 + R3030; all of them are equal in an homogeneous and isotropic space which explains the factor 3. Right? Anyway, could you explain how R1010 describes the acceleration for the geodesic deviation in this case?
That much I can do right away, I have yet to go over your previous responses. The basic idea is that the Riemann tensor can be physically interpreted in terms of tidal forces via the geodesic deviation equation.
The geodesic deviation equation
<br />
\frac{d^2 x^a}{dt^2} = R^a{}_{bcd} u^b \xi^c u^d<br />
gives the acceleration between a pair of points on neighboring geodesics. We need to specify each geodesic, which can be done by specifying a point in space, and a four-velocity, which defines the geodesic. The relative acceleration, though, depends only on the relative position. So we need to specify two four velocities, and one relative position.
Here u^b and u^d are the four-velocities (one four velocity for each geodesic), and \mbox{\xi^c} is the spatial separation of the pair of geodesics.
<br />
R^a{}_{bcd} u^b u^d<br />
maps a vector \xi^c that describes an spatial offset into a relative acceleration.
Now we assume that u^b and u^d both represent zero velocity (which means they are unit vectors in the time directon). This means we are interested in the tidal force on an object where both ends are stationary
Next, in this case, we are interested in the acceleration in the x direction introduced by a displacement between geodesics in the x direction. This mean that \mbox{\xi} is a unit vector in the x direction.
The end result is that with these values for u^b, \xi^c, u^d, we in essence "pick out" one component of the Riemann
This is R^x{}_{txt}
It gives the tidal force in the x direction due to an x offset - it's the x component of the "stretching" tidal force. By isotropy, the y and z stretching components will be equal.
Conveniently, we don't have to worry too much about scale factors with these combinations of superscripts and subscripts. If we scale everything in the x direction by a factor of .1, both the separation vector and the acceleration vector get scaled by the same amount, so the ratio remains constant. The only thing we need to worry about is that the time vector is scaled properly. Whle four velocities are always one in minkowski space they might not be one in a general metric.
In this case g_00 is -1, so there isn't a problem.
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Note that R^y{}_{txt} is zero in this case. If it existed, it would represent a tidal torque, rather than a tidal stretching force. The diagonal elements of R^a{}_{bcd} u^b u^d are all stretching or compressing tidal forces, the off-diagonal components are all tidal torques.