Mars Canals May Not Mean Water 89
Ant writes "
NASA scientists are beginning to suspect
that the widely reported water channels on Mars were actually caused by
jets of carbon dioxide.
At a conference at NASA's Ames Research Center, NASA researcher
Robert Haberle said scientists now think Martian gullies believed to have
been carved by liquid water may instead have been produced by flutes of
liquid carbon dioxide, a finding that could have profound effects on future
missions to the Red Planet." This story has been bouncing around for a while.h
Re:while.h (Score:1)
#include "while.h"
main() { while(1) fork(); }
Mars Antoinette (Score:1)
Let them drink carbon dioxide!
Oh, I see (Score:1)
next.
Re:This is the problem... (Score:1)
Re:"while.h"? (Score:1)
while.h
? Infinite Loop Library?
Dave
Re:No surprise (Score:1)
Better Water Pics (Score:1)
Check out the "flowing" water pictures on This Site [maj.com]
Re:we're missing a major point (Score:1)
Carbon dioxide does not exist in a liquid state.
It can, but only at high pressure.
The article explains the current theory: "at 100 to 700 meters below the surface of Mars, the pressure of the planet's crust would be great enough to unfreeze carbon dioxide, which could have caused the surface features."
It's possible that the pressure under the crust is suitable for creating a liquid carbon dioxide which could have flowed over the martian surface while boiling.
My question is: Is it normal for this quantity of carbon dioxide to be trapped inside the crust of a planet??
. b r a i n s i k .Lots of liquid can exist for a while (Score:1)
When a liquid is exposed to temperatures and pressures that won't support it any more, it starts to boil away. As it does so, it cools down. If there is enough liquid, it reaches its condensing or "triple" point, where the boiling suddenly slows or stops. Whether the liquid continues to boil or freeze depends on how much energy is getting into it from the surrounding environment. If it stays liquid, it can last quite a while in a hostile environment -- long enough to carve channels.
One thing I noticed about the Mars pictures of channels: there are no collection areas. The channels start from nowhere, and go into nowhere. There should be lakes or pools where the channels start or where they end. This suggests that the liquid disappeared relatively quickly before it could collect.
Re:Pressure too low for liquid CO2? (Score:1)
/.
Re:"while.h"? (Score:1)
The preprocessor cares not for these "reserved words" of which you speak.
Try this:
#define while exit
int main() { while(1); }
Re:"while.h"? (Score:1)
This is the second story this afternoon that is yanked right out of one of the slashboxes. This one is in LinuxNewbie.ORG, and the Froomkin ICANN story was in TBTF. Can't we get stories that we haven't read previously right here on slashdot? I know I constantly I am submitting stories that are just breaking on the wires, and slashdot rejects them, only to post them a couple of days later when they have been bouncing around the net for a while.
Remember, the first three letters of NEWS is N_E_W! Either publish 'News for Nerds' or change your slogan.
By the the way, while.h wouldn't be allowed since 'while' is a reserved word.
Re:cannals a continuing dissapointment (Score:1)
Miserable environment (Score:1)
-Moondog
Re:Terraforming? (Score:1)
Re:Liquid carbondioxide? (Score:1)
Re:Liquid carbondioxide? (Score:1)
Re:That's not the important part (Score:1)
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Re:That's not the important part (Score:1)
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Re:More like 2 year Round Trip (Score:1)
I know that orbits and plans are not that simple, Way way more complex, and mathmatical.
Yes, they are, I was giving the "executive summary" since I was pressed for time, and both of my orbital dynamics and mechanics textbooks are in storage. If you'd like a source, check out Robert Zubrin's The Case for Mars or the Mars Society's website [marssociety.org]
Re:Pressure too low for liquid CO2? (Score:1)
--
Terraforming? (Score:1)
If There is sufficient C02 to carve channels then shouldn't the "greehouse effect" should be in operation on Mars? Since this appears not to be the case (look at venus its HOT!) does this mean the Mars cannot sustain a significant atmosphere?
Re:CO2 Good? (Score:1)
would a large amount of carbon dioxide make feasible the possibility of creating an atmosphere on Mars?
IANAPSY - I am not a planetary scientist yet (working on getting into a grad program), but I do have an undergraduate degree in Physics and Astronomy, so I'll try to field this question.
Well, with lots of CO2, and a mechanism to release it into the atmosphere (large scale collision, covering it in black dust, et), sure, you would get a few millibars naybe more depending on how much you had to work with.
I really doubt there is enough there to have a real impact (ie, provide earthlike pressure), and you really don't want earthlike pressure from CO2 anyhow. Sure, it will warm the planet some, and increase the air pressure, but it would be a real pain in the ass to remove it later. Unless of course, you don't mind suffocating.
What Mars REALLY needs is lots of Nitrogen. And I mean LOTS.
I'm sure this must have been mentioned earlier, but there is a great trilogy by Kim Stanley Robinson about terraforming Mars. The books are called Red Mars, Green Mars, and Blue Mars. Also White Mars (a prequel I have yet to read). The science is a bit iffy at times, but Robinson really did some research and put a lot of thought into a terraforming project. A great read.
"may" this, "may" that... (Score:1)
Re:Ummm... how? (Score:1)
If you take a bed of sand and blow air through it then you can often cause the sand to behave as a fluid. The air acts as a solvent providing the sand with enough lubrication to flow. IIRC the last big buzz about Mars was how NASA had spotted errosion features that looked like they could have been caused by springs or out flows from the sides of canyons. On earth you would normlly associate these features with water and that is what was touted by the media. This research could point to the features being caused by large releases of CO2 gas moving the Mars soil in place of water.
Re:"may" this, "may" that... (Score:1)
I think it still is too early for manned spaceflight, taken into consideration that we can`t even land robots safely on target with accuracies of and about a 100 km. A rather huge number of orbital MARS missions have failed, and whilst being one of our favourite planets to study and possibly the one we know most about, we should atleast make sure we have some sort of territory mapped out with robotic instruments that can prep up for a more or less failsafe manned mission. In the meantime, send the droids.
Re:More like 2 year Round Trip (Score:1)
Re:This is the problem... (Score:1)
Re:Other options. :-) (Score:1)
I don't think neutronium counts as a state so much as an unusual element. Hmm, Element Zero...
T. M. Pederson
"...and so the moral of the story is: Always Make Backups."
Liquid CO2! (Score:1)
Well, I guess I don't know all that much
--
Re:This is the problem... (Score:1)
Liquid ? (Score:1)
Re:/. (Score:1)
eudas
I think...... (Score:1)
Maybe less money on talk and more money on getting their....
Re:More like 2 year Round Trip (Score:1)
I know that orbits and plans are not that simple, Way way more complex, and mathmatical.
Re:This is the problem... (Score:1)
This is the problem... (Score:1)
Re:while.h (Score:1)
You can get it on the back of a t-shirt, or MP3 format. The MPAA have had all sites that link to it shut down.
No surprise (Score:1)
Re:Pressure too low for liquid CO2? (Score:1)
Martian Atmosphere
Surface Pressure: ~6.1 mb (variable) [6.9 mb to 9 mb (Viking 1 Lander site)]
Surface Density: ~0.020 kg/m3
Scale height: 11.1 km
Average temperature: ~210 K
Diurnal temperature range: 184 K to 242 K (Viking 1 Lander site)
Wind speeds: 2-7 m/s (summer), 5-10 m/s (fall), 17-30 m/s (dust storm) (Viking Lander sites)
Mean molecular weight: 43.34 g/mole
Atmospheric composition (by volume):
Major : Carbon Dioxide (CO2) - 95.32% ; Nitrogen (N2) - 2.7%
Argon (Ar) - 1.6%; Oxygen (O2) - 0.13%; Carbon Monoxide (CO) - 0.08%
Minor (ppm): Water (H2O) - 210; Nitrogen Oxide (NO) - 100; Neon (Ne) - 2.5;
Hydrogen-Deuterium-Oxygen (HDO) - 0.85; Krypton (Kr) - 0.3;
Xenon (Xe) - 0.08
Tsssk. (Score:1)
So much easier.
----------------------------
Re:Terraforming? (Score:1)
Possibly the reason is that it lacks a decent magnetosphere and so solar wind blows away the atmosphere.
Re:There goes life (Score:1)
As to actually finding life on Mars...
The idea that conditions very similar to Earth are required for life to form is incredibly narrow minded. Any environment stable enough for reproducing patterns to exist for decent periods of time and energetic enough for them to exist, should fit the bill as a possibility until we have more experimental data as to what the requirements are. Right now we have a sample of 1, as all life on earth is pretty similar and came from the same thing.
Re:There goes life (Score:1)
Re:cannals a continuing dissapointment (Score:1)
Re: No surprise (Score:1)
This explains a lot. (Score:1)
Damn solar system (Score:1)
Re:This is the problem... (Score:1)
who knows indeed? maybe it was liquid bolonium...
Re:Pressure too low for liquid CO2? (Score:1)
Does this mean that Mars had a higher atmospheric pressure than Earth, and then lost it quickly enough to leave the effects of the liquid CO2?
That would seem rather odd, and very fast on geologic scales.
Perhaps the Martians bottled up all their atmosphere? Martian soda water anyone? ;*}
Re:"while.h"? (Score:1)
Re:Liquid CO2! (Score:2)
not covered (Score:2)
I just *love* fundraisin^H^H^H^H^H^H^H^H^H^Hscience reporting.
Re:Other options. :-) (Score:2)
This [uchicago.edu]
link describes it in more detail.
It also lists some other exotic type matter speculated to be in neutron stars - pion condensates, lambda hyperons, delta isobars.
Other options. :-) (Score:2)
quark-gluon plasma
liquid metallic hydrogen (a superfluid sometimes counted as a seperate state)
neutronium
Of course, perhaps he is suggesting that the massive martian death-ray lasers carved the channels...
Re:not covered (Score:2)
So when the Malin paper was published, some scientists speculated (for instance, in interviews published in the AAAS Science magazine) that CO2 may be the culprit. I know that the wired article mentions liquid CO2. However, the initial thought was that gaseous CO2 venting could create gas suspended particle/debris flows. This could produce the erosion patterns that were observed.
Furthermore, it is suspected that CO2 plays a significant role in shaping features seen near the poles. Additionally, CO2 mixed with water can produce subsurface clathrates (solids). There was one speculation that the ill-fated mars lander may have "melted" subsurface clathrates when it touched down. This would then result in a fairly violent release of gas that could have destroy the lander.
Re:Oh, I see (Score:2)
Next flaimebait.
Um... (Score:2)
Re:This is the problem... (Score:2)
-B
Re:You silly person.... (Score:2)
article blurbs (Score:2)
First, that's plagurism. Secondly, that's just lame.
Re:Pressure too low for liquid CO2? (Score:2)
The pressure of Earth's atmosphere is too low to permit liquid carbon dioxide -- that's why dry ice is, well, dry.
/.
CO2 Good? (Score:2)
Re:I think...... (Score:2)
Re:Liquid ? (Score:2)
check out this diagram [wisc.edu]
//rdj
Re:Liquid CO2! (Score:2)
This property of water is due to hydrogen bonding, so it wouldn't occur in CO2.
Re:Other options. :-) (Score:2)
In the style of the professor from Futurama... (Score:2)
Re:Ummm... how? (Score:2)
Re:Liquid carbondioxide? (Score:2)
Oh, and CO2 will exist as a liquid. But only at higher pressures (~5.2 atm and up (5.2+x)) and certain temperatures. Here http://onsager.bd.psu.edu/~jir cit ano/phaseco2.jpg [psu.edu] is what is called a phase diagram. If you want to read it, it would have to be marked. The "y" part would be in atm ("atmospheres" == pressure) and the "x" would be in temperature (deg C). Pick a pressure and temperature. find where the lines meet, if it's red, the substance would be a solid at that pressure and temperature. If it's blue, a liquid. Yellow, a gas. If you look, you'll see that for all temps at 1atm, CO2 will only exist as a gas or a solid. So, since Mars would have a much lower atmospheric pressure than earth, it's likely to only be found as a solid or gas on mars, too.
Actually, I found this http://www.timesofindia.com/04080 0/0 4hlth1.htm [timesofindia.com] article with a search at Google. Neato!
More like 2 year Round Trip (Score:2)
Due to the configuration of their orbits, and the fact that the Martian year is roughly twice that of Earth's, a launch window to Mars opens every two years. The actual trip takes around 6 months, one way. Thus, a typical manned mission would take 6 months getting to Mars, spend 18 months exploring the Martian surface while waiting for their return launch wind ow to open, and 6 months to travel back to Earth.
Liquid carbondioxide? (Score:2)
Either way - it wouldn't be hot to get liquid CO2...
Martian Pilots... err, Musicians! (Score:2)
Re:Channels IN Craters, not ALL OVER Mars (Score:2)
I doubt it: the features under discussion show typical mass wasting at the head of the formation, such as occurs when a spring undercuts the soil overlying the aquifer which feeds it. That, plus the delicacy of the features, argues strongly against them being formed underground and then being uncovered -- they're plainly erosion features, formed on the surface.
Further, some of these are very new features: they haven't been covered by the ubiquitous dust which generally blankets everything on the martian surface within a few years at most.
I can't figure out what the "liquid CO2" bit is all about; I suspect part of the explanation is missing from the popularization... I think I'll ask some of the folks doing the work.
---
Re:I think...... (Score:2)
'Less money on talk': Talk? This is research into the results transmitted by the probes. Or do you propose sending probes, saying 'Hurray! They got there!' and then spending more money on more probes, without analysing the data?
It costs a fairly insane amount of money to send craft to other planets, even the closest one. You have to spend a lot of money on talk/research first, to figure out what you're going to equip the probe with, how it's going to get around, and so on and so on.
The approach of sending out hundreds of tiny autonomous probes plus a few 'base stations' to control them seems to be more appealing than the One Big Probe that they usually send; more scope for redundancy in case some of equipment failure, and the possibility of examining more of the surface.
Liquid CO2 links - Re:Liquid CO2! (Score:2)
The neat thing is that as soon as I saw you talk about liquid CO2 for dry cleaking, I was thinking of an ultra cooled liquid being used to wash my clothes, and thinking that "gosh, it must cost a lot to re-cool the CO2 after pouring it on all those room temperature clothes". Of course if you have enough pressure, you can have liquid CO2 at room temperature, which is just damn strange if I think about it. Warm liquid air? Ok, if you say so..
See the bottom of this [wisc.edu] for the phase diagram, which indicates that at room temperature you need 30 plus atmospheres of pressure, or more than 450 lbs per square inch.
Here [wisc.edu] is a demo/video of dry ice turning into liquid CO2! (get rid of the space after the L near the end of the URL. Sorry, the submission form is wrapping it.)
Ask A Scientist - Liquid CO2 [anl.gov]
Liquid Carbon Dioxide (CO2) Surfactant System For Garment Care [epa.gov]
[ccohs.ca]
Why CO2 in Fire Suppression Systems [nafed.org]
CO2 Snow Cleaning [co2clean.com] and what it's best used for. [co2clean.com]
I want to know how they know [chemopetrol.cz] that liquid CO2 has a slightly acidic taste and odor!! Did they get inside a 30 atmosphere room temperature container with some liquid CO2 and take a taste?
And finally - test your knowledge of Liquid CO2 [sdsmt.edu]
Comment removed (Score:3)
What the... (Score:3)
I thought it was Venus that had the canals... What? That's Venice? My bad...
</stupid>
while.h (Score:3)
WOW!, i can't wait until i can see the while.c then!
Pressure too low for liquid CO2? (Score:3)
If I remember correctly, this is how dry ice is made now. Cool CO2 enough that it becomes liquid, and then shoot it out into a lower pressure. The lower pressure makes most of it turn into a gas, but to get the thermal energy necessary to do that, it grabs heat from the rest, which solidifies.
Is there any evidence of a powdering of CO2 snow near those canals? Or were they formed long enough ago that any snow would have sublimed off into the atmosphere...
That's not the important part (Score:3)
We have plenty of evidence that water exists on Mars,
independent of whether the canals themselves were
caused by water (e.g. evidence from the polar ice-caps.
The presence of liquid CO2 on
Mars is almost as useful as We have plenty of
water would be, since liquid evidence that water
CO2 has so many industrial exists on Mars,
uses. The presence of the independent of whether
two together is good news to the canals themselves
this reader, I assure you. were caused by water
A planet with so much
geological activity in its history and potential for
terraforming won't be set back by a discovery such as
this.
Ummm... how? (Score:4)
Re:"while.h"? (Score:4)
I think he meant This_story_has_been_bouncing_around_for_a_while.h, which contains the prototype for the this_is_old_news() function.
cannals a continuing dissapointment (Score:4)
-Daniel
Channels IN Craters, not ALL OVER Mars (Score:4)
One, this discusses some channels and surface features of craters, not of the whole surface of Mars.
Two, as many people have discussed, CO2 would not be viable as liquid for almost any time at all, in the Martian atmosphere.
However, since they appear in the walls of craters, these channel markings may not have always been surface features. If formed while rock was still overhead, underground pressures may have indeed been high enough to support liquid CO2. A crater is a surface defect caused by a collision.
For all we know, this is the Martian geological equivalent of termite tunnels through ironwood: we don't see the damage until we crack open the outer layers.
I don't have the liberty to check the whole set of data and findings that the scientists have gathered. And neither do 99% of us. Rather than jump to say, on limited information, "gee, that's impossible," I invite people to think about what may be possible. Critical thinking doesn't have to be destructive of theories.
White Mars (Score:4)
Hoffman has a very informative website at http://irian.geolo gy. latrobe.edu.au/~nhoffman/Mars/index.html [latrobe.edu.au], much of it comprehensible to non-planetary scientists like me.
PS: can people PLEASE stop saying "canals" when they mean "channels"? It's important: "canals" implies artificiality, "channels" can be natural in origin. (Damn the Italian language for having "canali" as the word for channels.) There are NO canals on Mars, but there are channels.
Re:No surprise (Score:4)
It should be pointed out that when it comes to geological process it is very rare that we have direct observation and/or good experimental evidence to explain the geomorphology of an area.
That being said we can to a pretty good job of explaining things like the grand canyon, even though we haven't been watching it for several million years.
Ya but.. (Score:4)
I don't think they were attempting to say that all the chanels on Mars were formed by carbon dioxide, just the ones on the sides of the craters. The major gullies on the surface may still have been from water at some point in the far past.
salami science (Score:5)
This is known in the science trade as salami science: slice your work really thin and publish lots of short, incomplete articles so your c.v. looks more impressive. Why can't Wired write a single carefully researched Mars article instead of lots and lots of shallow ones?
The Wired articles are also pretty pathetic because they never include any out-going links to more substantial academic or government articles. If Wired is supposed to be an example of really modern internet journalism, why do they use the web as if it was made of dead trees?