A Molniya-like constellation of orbiters, combined with a manned base, would do the trick. Phobos is invisible from even moderately high Mars latitudes - as Tennyson didn't put it, 'The moonless poles of snowy Mars' don't see either moon.
Mars moons are probably bone-dry. This is a significant downside.
Quote from: gospacex on 06/02/2016 11:11 amMars moons are probably bone-dry. This is a significant downside.We don't know that. It could be they're dry to a few metres.Kerogen would also be a nice material to find - as well as water.
Even if a station is put on Phobos, how often will it be occupied, especially after a Mars landing?
if we built an outpost on either, or both, I'd expect it was there to stay. I think that's just how Musk rolls.
Quote from: alexterrell on 06/05/2016 07:15 pmQuote from: gospacex on 06/02/2016 11:11 amMars moons are probably bone-dry. This is a significant downside.We don't know that. It could be they're dry to a few metres.Kerogen would also be a nice material to find - as well as water. The question whether they are dry or volatile-rich is a function of their mode of formation. If they are captured asteroids with a composition similar of carbonaceous chondrites, they might have a significant volatile content. If, on the other hand, they were formed from a debris disk after a Giant Impact on Mars, they will likely be dry. So if they are dry, they are dry all the way through (same if they are rich in volatiles).But then, nature has that tendency to be different from what we imagine. Lets go and see.
The biggest value of the Martian moons might be - literally - nothing at all. There is real reason to believe that they may be rock piles, with significant voids. Such voids (if stable) would be perfect places to put habitats and storage areas. Leave the dusty surface for visitors, and PV farms, burrow in, and Port Phobos is in business!
Quote from: Bob Shaw on 06/11/2016 02:01 amThe biggest value of the Martian moons might be - literally - nothing at all. There is real reason to believe that they may be rock piles, with significant voids. Such voids (if stable) would be perfect places to put habitats and storage areas. Leave the dusty surface for visitors, and PV farms, burrow in, and Port Phobos is in business!If the moon is soft - e.g. a rubble pile, voids won't be stable.However, stable voids can be made with a balloon and a supply of compressed air. Somewhere between 0.4 and 1.0 bar Oxygen / Nitrogen mix would do the job.
Quote from: Bynaus on 06/09/2016 05:00 pmQuote from: alexterrell on 06/05/2016 07:15 pmQuote from: gospacex on 06/02/2016 11:11 amMars moons are probably bone-dry. This is a significant downside.We don't know that. It could be they're dry to a few metres.Kerogen would also be a nice material to find - as well as water. The question whether they are dry or volatile-rich is a function of their mode of formation. If they are captured asteroids with a composition similar of carbonaceous chondrites, they might have a significant volatile content. If, on the other hand, they were formed from a debris disk after a Giant Impact on Mars, they will likely be dry. So if they are dry, they are dry all the way through (same if they are rich in volatiles).But then, nature has that tendency to be different from what we imagine. Lets go and see. Surely if formed from a giant impact, they would have been unstable over the course of billions of years. Phobos has a short life ahead of it. This probably means they are captured asteroids. Whether originally dry asteroids, or whether they've had moisture baked out of them, we don't know.