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A New Angle on Martian Methane 95

dusty writes "A recent hypothesis paper entititled 'Martian CH4: Sources, Flux, and Detection' delves into the production of methane on Mars. This hypothesis compares Mars with South Africa, and draws the conclusion that the radiolysis of martian ice and water while reacting with carbon dioxide can produce enough methane to account for recently observed concentrations. Methane is important because it is hard to explain. It has a short half-life and must be replenished frequently. As recently as 2005 the public line from NASA/JPL was that the methane could be produced by volcanism. Mars' dormant Olympus Mons is the largest volcano in the solar system but auspiciously quiet. A recent study from NOAA throws into question the whole idea stating, 'If Mauna Loa is a valid terrestrial analog, our findings suggest that volcanic activity is not a significant source of methane to the Martian atmosphere.'"
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A New Angle on Martian Methane

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  • Re:Radioactive? (Score:3, Insightful)

    by MadCow42 ( 243108 ) on Friday October 06, 2006 @07:32AM (#16334585) Homepage
    According to the article (first paragraphs even...), Methane is chemically broken down by sunlight over a few hundred years.

    MadCow.
  • Re:No life? (Score:4, Insightful)

    by z0idberg ( 888892 ) on Friday October 06, 2006 @07:33AM (#16334593)
    I think the point is that the source of methane could potentially have been produced by living organisms but there is no other evidence at all of living organisms. Hence the search for what else could be the source.
  • Re:No life? (Score:4, Insightful)

    by MichaelSmith ( 789609 ) on Friday October 06, 2006 @07:42AM (#16334629) Homepage Journal
    methane could potentially have been produced by living organisms

    Given that we know the rate of destruction of Methane on Mars we also know the rate of production, which should make it possible to estimate the mass of Methane producing bacteria, assuming that is the source.

  • Good science (Score:5, Insightful)

    by Da3vid ( 926771 ) on Friday October 06, 2006 @08:23AM (#16334863)
    "'If Mauna Loa is a valid terrestrial analog, our findings suggest that volcanic activity is not a significant source of methane to the Martian atmosphere.'"

    Man, I wish more of our scientific quotes sounded like this one. It lays it out straight and simple. Here is our source of info: analogy with Mauna Loa. Here is our assumption: we can project info from it onto Olympus Mons. Here is our conclusion: there is something else other than volcanic activity producing methane on Mars. I like how all that info was neatly packaged into a simple sentence. I also like how he admits the assumption... if. The thing that comes to mind are all the dinosaur shows explaining their day to day lives, zodiac signs and favorite take-out places.
  • by splutty ( 43475 ) on Friday October 06, 2006 @08:26AM (#16334895)
    Uhm. Since always? Science is the whole idea of making a (thought out or not) statement, and then setting about disproving it. If you fail to disprove it, you end up with the 'last option is that it's true' idea.
  • by Gospodin ( 547743 ) on Friday October 06, 2006 @09:39AM (#16335567)

    It's called: Remarkable claims require remarkable evidence.

    Science isn't about believing anything is possible until proved otherwise. I think many scientists would agree that it's possible there is or was life on Mars. But life evolving independently anywhere other than Earth would be a major breakthrough for science, so they want to be very careful about claiming it until it is really, unquestionably proved. IMO this is just good science.

  • Re:Radioactive? (Score:5, Insightful)

    by radtea ( 464814 ) on Friday October 06, 2006 @10:09AM (#16335925)
    The term can be applied to anything which decays with time, though radioactive decay would probably give the most attractive decay curve.

    You get the same curve from anything that has a probability of decay that is independent of time.

    If the probability of decay, destruction or loss for an individual atom is L per unit time, then for N atoms the rate of change of N is:

    dN/dt = -L*N

    and integrating gives N = No*exp(-L*t) where No is the number of atoms at some arbitrary t=0.

    So for any situation where you have a constant decay probability you will get the same curve. For methane in the Martian atmosphere the rate of decay is pretty much constant due to solar ultra-violet radiation breaking up the molecules. Therefore, if there were no source the amount of methane in the atmosphere would drop exponentially.

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