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=== It's time for useful links again. That last page filled fast. NASA Phoenix Mission University of Arizona Phoenix Mars Mission University of Arizona Phoenix Mars Mission: Lander Gallery JPL Phoenix Mission News NASA Phoenix Twitter Feed NASA Phoenix Multimedia CSA Phoenix Mars Mission Planetary Society: Phoenix Mission Planetary Society: Phoenix Non-SSI Raw Images Planetary Society: Phoenix Sol-By-Sol Summary Planetary Society: Weblog Emily Lakdawalla Ustream video chat (Wednesdays) Texas A&M University Phoenix SSI Raw Images Directory Unmanned Spaceflight Forum: Phoenix 2007/8 Google Mars landing site NASA TV (or NASA TV Yahoo! source or high-resolution) NASA TV Media Channel
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I understand that relatively pure water ice can coexist with salty soils because the salts can be forced out of the ice while it is forming. That is probably one of the reasons I was reading that the ice-soil interface can be extra rich in various compounds.
I take it then that all the talk of the great variety of salts as quoted a few pages above is true, but what wasn't said then was that all these salts are in extremely low concentration. I also take it that these low salt concentrations have nothing to do with the quotes from scientists about Mars being ideal soil with all the nutrients needed for growing asparagus, etc. Correct? RBG |
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With the Ideal Gas Law in mind, it's unsurprising that pressure would depend on temperature.
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Many nutrients can present themselves to roots as salt ions within salt solutions (for instance: potassium chloride or ammonium nitrate). I'm not sure to which specific low concentrations you refer -- I don't recall seeing a breakdown of the MECA WCL results -- but I'd expect some of them to be considered nutrients.
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According to New Scientist, William Boynton suggested in the news conference that salts may have melted the ice in the soil to cause it to stick to the scoop:
Phoenix Mars lander 'tastes' first sample of water ice. Updated 19:43 01 August 2008 "On 15 July, the team used a sort of drill called a rasp attached to the scoop to cut cores out of Snow White and collect the shavings in a compartment on the back side of the scoop. But when the scoop was turned upside down, the sample stuck to the walls inside. Martian salt may have melted the ice and made the soil sticky, says Boynton." http://space.newscientist.com/articl...water-ice.html Note that the ice just turning into a gas would not make the soil sticky. Keep in mind also that salts also depress the pressure requirements for liquid water as it does the temperature requirements. Anyone have the transcript of the conference where Boynton says this? Bob Clark |
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![]() And the Optical delivery: ![]() And, near Dodo-Goldilocks, the new Cupboard trench, which probably contributed the Optical sample: ![]()
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Could someone explain what sorts of organics TEGA can detect? I understand that if you heat oils or perhaps PAH's, tholins etc volatiles will take off and then be "weighed" by the mass spec. But what about sugars, amino and nucleic acids or other really interesting organic molecules? Would they be volatilized too or just decompose at high T?
Also, could the conductivity meter on MECA discriminate among the possible group of: pure ice, salty ice, salty water? If I had an ohm meter and a freeze dryer could I devise a simulation? Finally why are the microscope pictures so fuzzy? At the modest magnification level we see, it should be razor sharp Thanks |
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Amino acids (for one) would mostly decompose, but would release more nitrogen as the temp increased. The temperature at which this release occurred would be revealing.
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I see Mars Phoenix her own self (or the Phoenix JPL-news-service-manager team member speaking through the lander sockpuppet), has twittered about the White House briefing, in reverse-chronological order, MarsPhoenix Twitter:
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More factoids to chew on, skeptically:
Wired: Science Blog: Rumors Abound About 'Potential for Life' on Mars Quote:
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My two cents: If the salt is 1 PPT, that is way too dilute to affect melting point is a significant way. The melting/freezing point for pure water will remain zero C. Pressure becomes significant when very high. Under high pressure water melts at lower temperature (as in ice skater who glides on thin film of water) But on Mars the ATM pressure is even lower than earths so the melting temperature remains zero celcius. If enough salt is present then then the melt/freeze temp is depressed downward to -21 C. Colder and it all goes to solids. Good chart at http://www.ucalgary.ca/~kmuldrew/cry...o_chap6_1.html so all water, pure or salty on Mars is solid, gas or chemically bound until it gets above -21, enough to melt saturated salt water if it exists. But from my reading of some previous posts, or at least I think one possible argument is that beneath the soil, at the point were the soil meets the ice "bedrock", there may be a salt rich interface where liquid water may exist. In direct sunlight some heat would transfer into that layer. The thin air insulates. If there is enough salt and enough heat there there will be melt water. It could exist for short periods. As it vaporized it would cool the bulk liquid and it could refreeze into an aggregate of soil and ice in the scoop thingy. Every 20 million years or so the Mars axis tilt increases to some 40 degrees off vertical. The cap melts and reforms over that time scale. The case can be made for extreme repeated freeze concentration of salt layers at the soil water interface creating boundary layers of extremely pure ice as well as saturated briney ices and precipitated solid salts. and for sufficient heat to release liquid salt water. Interesting things happen at boundary layers. But at 8 mBar and say -20 C even saturated salt water would not last long. It would boil and refreeze or have such a high vapor pressure, it would soon evaporate. Dissolved salts reduce water vapor pressure but not enough to stablize liquid at Mars ATM. So no stable liquid water unless there is an extraordinary subterranean cycle to replace it or the humidity was very high. I can't find any humidity data on the Canadian site. Is that currently measurable on Mars? It must be very low because the extreme low temperatures that the south pole currently pulling out water and co2, right? Hope this makes some sense. What I don't understand is why doesn't the solid ice bedrock sublime away? Do that have a temperature of that ice in situ? I have a freeze dryer and too much time. I might try something. Unless its all been done. So please stop me before I break something. This just in from WH: "Mars...its a Plant ...up in the sky. The General at NASA saw a lot of wet nutrinos . We own 2/3 NASA and so half that plant is mine. Run a Google on that!" ![]() |
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Sol 68 Raw Images have just begun to arrive. There are 4 so far, from MECA Optical Microscope.
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![]() I think it's time to include our trench map, the two new ones, Cupboard and Neverland, in yellow: ![]()
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Emily Lakdawalla takes her turn at the Phoenix habitability rumor mill:
Planetary Society Weblog: Apparently there's something more exciting yet to be announced by Phoenix Quote:
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Sol 69 Raw Images have begun arriving.
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One year since launch- happy anniversary, Phoenix!
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I want to go back to the moon. I don't care which rocket you use, whichever one you pick, I'll like it, I swear. "If you think the LHC will create black holes, you might as well believe Hobbits are at the bottom of your garden."- Dr. Mike Inglis Rovers forever! - ToSeek |
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Oh, I like this headline, and the illustrious source the reporter consulted (waves):
Sydney Morning Herald: NASA's next small step may be into Martian manure Quote:
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Nasa press release: perchlorate
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[Oh no. I edited when I meant to quote. Now I have to reproduce the article I wiped. Excuse me while I cry... OK, here's my reconstuction...]
The perchlorate press release (from JPL): NASA Spacecraft Analyzing Martian Soil Data Quote:
On my scorecard, I've got it: 2 MECA WCL samples: probably perchlorate. First TEGA sample, surface: probably confirmatory of perchlorate. Second TEGA sample, near ice: maybe not perchlorate everywhere. Quote:
Tuesday, August 5, 1100 PDT Tuesday, August 5, 1400 EDT Tuesday, August 5, 1800 UTC === And what does this mean for my planned asparagus farming operation? American Chemical Society, Science News: Perchlorate found in produce from around the world Quote:
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Emily Lakdawalla to the rescue...
Planetary Society Weblog: The Phoenix flap Quote:
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