J
j05h
Guest
We been touching on this subject in "Mars 9 tons at a time", and it seems time to bring the old subject back up. Should we go to Mars' moons first? Accessing Phobos and Deimos is definitely easier than the surface of Mars and cheaper in delta-V than getting to the lunar surface. <br /><br />I covered this argument extensively in spring '06 in the thread "Private Mars Missions" and it's also been touched on lately in "Mars 9 tons..."<br /><br />The argument breaks down to one thing: volatiles. If Phobos or Deimos has any amount of accessible water or other hydrates, these bodies will immediately become competitive as a target for industrial development. We know there is water on Mars, but it requires surface-access. Lunar volatiles, if they exist, are in dark polar craters - the hydrogen readings from our sensors have not confirmed water, it could be locked up in rocks. We already know how to function in freefall and some of the modules for this are off-the-shelf (Russian FGB), helping the utilization of these mini-moons. The real question: where's the water?<br /><br />Another aspect is building a "base camp" in Martian orbit. Stockpiling supplies and locally-produced volatiles (propellant, potable water and breathing atmosphere) in Mars orbit provides strong efficiencies for rocket transport and supply production heading to cis-lunar space. It also provides huge safety margins for any Mars surface activity. Instead of thinking of a single Mars base, supplies on-orbit can provide global surface access. <br /><br />So, what are the advantages and disadvantages of using and exploring the Martian Moons? What timeframe can they be accessed in? <div class="Discussion_UserSignature"> <div align="center"><em>We need a first generation of pioneers.</em><br /></div> </div>