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  • While not hard vacuum, the low [[Martian atmosphere|atmospheric surface pressure on Mars]] (7 mb) is inimical to Terran biology
    1 KB (151 words) - 04:02, 21 January 2009
  • ...rs by synthesizing a breathable atmosphere and propellant from the Martian atmosphere.
    4 KB (680 words) - 04:02, 21 January 2009
  • ...well as the rocket's. However, it can lift the rocket above much of the [[atmosphere]] (and its consequent [[atmospheric drag|drag]]), and provides considerable
    689 bytes (105 words) - 04:02, 21 January 2009
  • ...on occurs, means that the vehicle is able to collect the oxidizer from the atmosphere with less [[drag]] than would be typical of a other air breathing vehicles ...e vehicle up to speed and take the scram jet from the upper portion of the atmosphere to space.
    3 KB (551 words) - 04:02, 21 January 2009
  • ...eposits are frequently exposed to water frost condensed from the [[Martian atmosphere]]. Under microscopic examination, some Martian soil samples exhibit cement
    11 KB (1,766 words) - 04:02, 21 January 2009
  • ...p>2</sup>, compared to 1370 W/m<sup>2</sup> in Earth orbit. The [[martian atmosphere]] is thin, but so dusty that it cuts an average 25% of the incident sunligh
    14 KB (2,351 words) - 04:02, 21 January 2009
  • ...is 804 J/kgK Thus, by the formula above, the specific heat of the Martian atmosphere at that temperature is roughly 805 J/kgK, or nearly the same as that of car
    4 KB (638 words) - 04:02, 21 January 2009
  • ...much as the oxidizer. The vehicle would build up speed at the edge of the atmosphere breathing in air until it has reached orbital velocity. Prototypes of the s
    10 KB (1,764 words) - 04:02, 21 January 2009
  • ...arbon dioxide is plentiful on mars and the main constituent of the Martian atmosphere.
    4 KB (711 words) - 04:02, 21 January 2009
  • ...that the temperature of the walls is the same temperature as the [[Martian atmosphere|Martian air]].
    5 KB (783 words) - 04:02, 21 January 2009
  • ...ource utilization]] on [[Mars]]. It is a trace component of the [[Martian atmosphere]], and appears relatively abundant as ice in the Martian polar regions. Hy
    5 KB (758 words) - 04:02, 21 January 2009

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