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Mars May Have Been 1/3 Ocean

coondoggie sends in a snippet from Network World, as is his wont: "It's possible that a huge ocean covered one-third of the surface of Mars some 3.5 billion years ago, a finding likely to reignite an old argument about that amount of water on the red planet, according to a new report. The study by the University of Colorado at Boulder is the first to integrate multiple data sets of river deltas, valley networks and topography from a cadre of NASA and European Space Agency orbiting missions of Mars dating back to 2001, the researchers claim." The National Geographic coverage of the news gives some air time to those doubtful that this study will prove definitive.

27 of 118 comments (clear)

  1. maybe it's time to enlist the Japanese by ChipMonk · · Score: 2, Insightful

    They just proved they can bring back material from an asteroid. Let's see if they can duplicate the feat on Mars.

    1. Re:maybe it's time to enlist the Japanese by JoshuaZ · · Score: 5, Insightful

      We don't know if the capsule from Hayabusa does contain material yet. Also note that a sample-return mission to Mars will be much more difficult than a sample-return mission to an asteroid. The gravity of an asteroid is negligible. But Mars has gravity that is around a third that of Earth. That's a lot. So a sampling robot would need to land on Mars and then return fighting against the large Martian gravity well. It would probably need to carry its fuel with it which means it would need to have a lot of mass to start with and which would make a safe landing even more difficult. We'll probably have successful sample-return from Mars before a human mission their but the technical difficulty with even a sample-return mission is immense.

    2. Re:maybe it's time to enlist the Japanese by JWSmythe · · Score: 4, Funny

          Escape velocity, fuel supply, navigation. People always bring up those pesky problems. Gimme a spaceship that runs on dilithium crystals that you can run a starship at multiples of the speed of light indefinitely (or at least until the episode plot calls for them to be used up).

      --
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    3. Re:maybe it's time to enlist the Japanese by symbolset · · Score: 5, Interesting

      Update: it's been opened. It contains material. The report is due six months or so, so set a tickle.

      Mars is easier than an asteroid. At Mars you have a planet to cancel your Delta-V with its gravity and atmosphere (limited though Mars' atmosphere is, it does help). Hitting an asteroid and returning is roughly twice as hard as hitting Mars and returning because you have to halt your motion at the asteroid using propulsion. It's a miracle Hyabusa returned at all - and it was three years late - because it missed its return window and had to wait for Earth to come back into position. The efforts of the ground team could be considered heroic - if some blood had been spilled.

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    4. Re:maybe it's time to enlist the Japanese by denmarkw00t · · Score: 2, Interesting

      You could, in theory, work around these issues in different ways. You could include fuel containers in the payload with parachutes - if we can give the robot some way to find them it can navigate to and attach them when ready. You could also send multiple rockets, some with fuel and one for the robot, but having them find eachother would be more challenging and landing areas would be much more prone to error in the proximity.

      Still, it isn't impossible.

    5. Re:maybe it's time to enlist the Japanese by MichaelSmith · · Score: 3, Interesting

      One plan for Mars sample return I read about involves automatic docking in low Mars orbit. One stage lands and a rover loads it up with material. An ascent stage (really just a missile) lifts off for low orbit. It docks with an orbiter which has enough juice to return to Earth.

      All in all it is probably more productive to send better surface labs.

    6. Re:maybe it's time to enlist the Japanese by takev · · Score: 2, Funny

      Someone probably slashed their finger open on the inside of a computer case, dropping blood on the motherboard. So in all likelihood blood has been spilled by the ground crew.

    7. Re:maybe it's time to enlist the Japanese by stevelinton · · Score: 2, Insightful

      Getting to Mars is, in some was, easier than getting to an asteroid, because you can stop for free at Mars. Getting home again is much harder. There's no cheap way OFF Mars.

    8. Re:maybe it's time to enlist the Japanese by Teun · · Score: 2, Insightful
      Oh?

      Then why have parachutes been deployed on virtually every successful Mars landing?

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    9. Re:maybe it's time to enlist the Japanese by Hognoxious · · Score: 2, Funny

      Or attach it to a really long leash.

      [This post brought to you by the institute of cord spinners, rope braiders and string twisters]

      --
      Confucius say, "Find worm in apple - bad. Find half a worm - worse."
    10. Re:maybe it's time to enlist the Japanese by stevelinton · · Score: 3, Informative

      Let's do the numbers.

      The ascent stage (ie the Mars to Low Mars Orbit transport) needs about 4.1 km s^-1 of delta-V. About twice what you need from the Moon, but less than half what you need from Earth. The Mars orbit return vehicle, which doesn't need to land on Mars needs about 2.3 km s^-1 to get into a transfer orbit back to Earth. (figures from wikipedia).

      This is definitely challenging, ascent stage most challenging of all. We need a rocket that can survive launch from Earth, 9 months coasting, aerocapture and aerobraking at Mars, impact with the Mars surface, a few months sitting on Mars and then take off with no support systems, deliver 4+kms^-1 of delta-V and automatically dock with the orbiting component of the system. The durability requirement pretty much rules out cryogenic fuels, and even relatively stable liquid fuels like kerosene/nitric acid might give trouble, both due to the cold conditions on Mars and the extra mass of tankage robust enough to survive the journey, so you're probably looking at solids.

      A few quick checks reveal that good solid rockets have an ISP of maybe 265s, giving a mass ratio of perhaps 10 for Mars to Low Mars orbit, so we need an ascent stage roughly 90% of which is solid rocket propellant (or multiple ascent stages, adding complexity). Suppose we can get the payload capsule + docking system down to 10kg and our solid rocket motors are 95% propellant (5% nozzles and casing -- this might be optimistic) we get a mass of 200kg launching from Mars. This is actually less bad than I'd feared. Seems that a Viking sized lander could probably do it. A 1 ton or so lander includes a digging tool and maybe a mini-rover to collect 5kg of rock and load them into a 5kg capsule with some tiny thrusters on it. That sits on a 200kg solid fuel rocket that gets into Low Mars Orbit and drops the capsule, which docks with a similar sized vehicle with 100kg of solid fuel some batteries and electronics and a heat shield for Earth reentry.

      So we need two launches to Mars transfer, each about 1 ton payload, plus heat shields for aero-braking/aero-capture on Mars. Should be doable as two medium large launches from Earth

    11. Re:maybe it's time to enlist the Japanese by blair1q · · Score: 2, Interesting

      The report is due six months or so

      Oh, horseshit.

      I hate when an experiment is performed and nobody says a word on what happened, even from a qualitative view.

      They can at least describe what it looks like. "Grey dirt" would be plenty to hold me for the 6 months it takes to produce a full assay.

    12. Re:maybe it's time to enlist the Japanese by zlexiss · · Score: 2, Funny

      Good plan

  2. We'll Never Know by WrongSizeGlass · · Score: 5, Insightful

    The National Geographic coverage of the news gives some air time to those doubtful that this study will prove definitive.

    3.5 billion years ago is too long ago for us to ever *know* definitively. We won't get to Mars for decades and it would be decades after that before any real "hands on" research could even bring us closer to a "definitive" answer (which will still inly be a best guess).

    1. Re:We'll Never Know by MichaelSmith · · Score: 2, Insightful

      The National Geographic coverage of the news gives some air time to those doubtful that this study will prove definitive.

      3.5 billion years ago is too long ago for us to ever *know* definitively. We won't get to Mars for decades and it would be decades after that before any real "hands on" research could even bring us closer to a "definitive" answer (which will still inly be a best guess).

      Are you a geologist?

    2. Re:We'll Never Know by TheKidWho · · Score: 2, Funny

      It's going to take us decades to figure out what happened billions of years ago? I don't know about you, but that sounds pretty quick to me.

    3. Re:We'll Never Know by camperdave · · Score: 2, Insightful

      There's radioactive carbon dating. Oh, won't work. Well, you can look at the sedimentation layers. Oh, won't work. Well, there's always guesswork.

      Carbon dating and sedimentation layer examination are both guesswork. Educated guesswork, possibly even accurate guesswork, but guesswork nonetheless.

      --
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    4. Re:We'll Never Know by polymeris · · Score: 2, Informative

      Nah, we could date it really easily. There's radioactive carbon dating. Oh, won't work. Well, you can look at the sedimentation layers. Oh, won't work. Well, there's always guesswork. :)

      There are other radiometric dating methods besids carbon-14, specially for things that old. One of them is rubidium-strontium (50 billion yeras half life?). It works on inorganic stuff too, although i don't know if it works for martian inorganic stuff, but I'm sure one could adapt it.

      Really, the dating itself isn't as important as if water was or was not there.

      I agree.

  3. Always curious about where the water went by Low+Ranked+Craig · · Score: 3, Informative

    So I finally looked it up. Interesting. http://phoenix.lpl.arizona.edu/mars151.php

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    1. Re:Always curious about where the water went by Anonymous Coward · · Score: 4, Funny

      It is all underground, frozen and waiting for someone to turn the melting reactor on.

  4. Intelligent life by owlstead · · Score: 2, Funny

    OK, the ocean has been established. Maybe we can go and look for oil pollution to see if there was intelligent life on mars already?

    1. Re:Intelligent life by Psaakyrn · · Score: 3, Insightful

      What sort of intelligent life would cause oil pollution?

  5. Re:Not funny by Zocalo · · Score: 4, Informative

    Earth has an atmosphere where mars does not

    Mars has an atmosphere, not much of one to be sure, but it does have one. Why else do you think so many landers used parachutes to help slow their descent?

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  6. Re:If the earth is only 6,000 years old... by owlstead · · Score: 2, Funny

    Because it was retroactively made 3.5 billion years old 6000 years ago. Oh ye of little faith.

  7. Once upon a time... by Anonymous Coward · · Score: 4, Interesting

    Philip K. Dick wrote several short stories about how we lived on Mars and didn't remember to reduce, reuse, recycle, curb our species appetites for violence (war) and sex (overpopulation). So we burned up the oceans when it all went kaboom!. But not before we sent people to live on Earth...

    Now there are "billions and billions" of us. (sigh)

  8. Re:Not funny by Rakshasa+Taisab · · Score: 2, Funny

    Those were lovechutes; the good energies radiating from Mother Mars slowed the descent.

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  9. Related TED talk by Anonymous Coward · · Score: 2, Interesting

    One of the recent TED talks about returning to Mars mentioned this.

    In http://www.ted.com/talks/lang/eng/joel_levine.html (16 minute video) Joel Levine describes how

    * We've found plumes of methane in the Mars atmosphere above some of the coastal and structures mentioned in this article
    * On Earth, over 99.9% of methane is produced by living systems
    * Our next mars mission should not be a lander, but a robotic aerial flyer that can give more precise measurements of methane and other gasses along with improved ground images
    * Results from such a mission could be used to pinpoint with much higher confidence an appropriate location to send a followup lander for sample collection