davefoc
Philosopher
Much of the comet's original volatile content may be gone by now, leaving behind a spongy mass of dust grains.
I would have guessed this wasn't possible. The idea, I guess, is that space dust mixed with frozen gases and when the frozen gases sublimate a structure of space dust is left behind. As I write this I realize there's a lot I don't know here. What is the principle constituent of the coma that we can see from earth? Is the material spewed out of the comet mostly in a liquid state? If it is mostly in a gaseous state it seems surprising that it is opaque enough to reflect light.
But in addition to measuring the comet's mass with its gravity, it ought to be possible to measure its mass distribution's departure from sphericity. That ought to have been possible in Rosetta's 10-km orbits. It's 2D instead of 3D info, but it will enable testing hypotheses about the comet's mass distribution, like how depleted its outer layers are.
I've looked around for a discussion of this kind of thing and I haven't found it, but it seems like one of the things that people would have been doing calculations and maybe simulations of. Does it exist and I haven't found it or has it just not been released yet?