For what it's worth, the electrogravitic tensor E[##\vec{X}##] is the one I use the most. Basically, by picking the vector field ##\vec{X}##, it's integral curves define the motion of some reference observer, which also defines "the direction of time", and an associated (local) simultaneity convention. We don't need to know how to take the left and right duals to compute E.
If one has a static observer in a static metric, the magnetogravitic tensor ##B[\vec{x}]## is zero. This is similar to the electrostatic case in E&M. And it can be used as an approximation as well, similar to the electrostatic approximation in E&M. The decomposition process basically somewhat similar to the way we break E&M's Faraday tensor into electric and magnetic fields. It's not quite the same, there is no direct equivalent to the topogravitic part of the decomposition in E&M.
Note that we need to specify some observer to decompose the Faraday tensor into the electric part and the magnetic part - this is the role of the vector field ##\vec{X}##, to specify the observer.
Next, in exercise 14.14 of MTW, the second part of the exercise shows that in a vacuum, the topogravitic part of the tensor, called F in the exercise, is equal to the electrogravitic part, E.
So under the proper circumstances, the nonzero components of the 256 component Riemann are described by the 9 component E. I'll talk more about how that can be reduced even further.
E has a simple physical interpretation - the proper choice of coordinate axes, parallel to the eigenvectgors of the matrix, diagonalizes it. The eigenvalues in the diagonalized form corrrespond to the eignevalues.
So the eigenvectors of E define the principal stress axes of some test observer that is experiencing what we might call "tidal forces", and the eignevalues are the magnitude of these tidal forces.
This is a bit of a digression from the original point, which was basically that GRTensor could be an inspiration for things to calculate, though calclulating everything it does would probably be more ambitious than the OP wants.
Also, a change of basis (at least being able to switch between a coordinate basis and an orthonormal basis) are very useful things to be able to calculate.
For more specifics, see for instance
http://grtensor.phy.queensu.ca/Griihelp/grt_objects.help and
http://grtensor.phy.queensu.ca/Griihelp/grt_operators.help. The "objects" are self contained, the operators require additonal arguments, typically arguments that specify an observer via a vector field.