Showing posts with label mars. Show all posts
Showing posts with label mars. Show all posts

Sunday, 20 July 2008

Ammonia on Mars could mean life

by Dr David Whitehouse, BBC

Reposted from:
http://news.bbc.co.uk/2/hi/science/nature/3896335.stm

Ammonia may have been found in Mars' atmosphere which some scientists say could indicate life on the Red Planet.


Researchers say its spectral signature has been tentatively detected by sensors on board the European Space Agency's orbiting Mars Express craft.

Ammonia survives for only a short time in the Martian atmosphere so if it really does exist it must be getting constantly replenished.

There are two possible sources: either active volcanoes, none of which have been found yet on Mars, or microbes.


Suite of molecules

"Ammonia could be the key to finding life on Mars," one US space agency (Nasa) scientist told BBC News Online.

Spectral evidence for the gas was seen by the Planetary Fourier Spectrometer (PFS) on Mars Express.

Professor Vittorio Formisano, principal investigator for the instrument, is expected to release details of new findings from the PFS at an international conference being held next week in Paris.

The PFS is sensitive to radiation in the spectral region of 1.2-5 microns and 5-50 microns - a region rich with important molecules such as water and carbon dioxide. Ammonia has a spectral line at 10 microns.

Although Mars Express has been in orbit around Mars since December 2003, scientists have so far only analysed a fraction of the data the PFS has produced.

Researchers say this is because they are still coming to terms with the complexities of the PFS as well as coping with some nagging power problems on Mars Express.

So far the PFS has observed a depletion of carbon dioxide and an enrichment of water vapour over some of the large extinct volcanoes on Mars.

But it is the detection of minor compounds, possible in the sensors high-resolution mode, which are causing excitement.

The tentative detection of ammonia comes just a few months after methane was found in the Martian atmosphere. Methane is another gas with a possible biological origin.


Ammonia is not a stable molecule in the Martian atmosphere. If it was not replenished in some way, it would only last a few hours before it vanished.

One possibility the scientists have had to rule out is that the ammonia comes from the air bags of the failed Beagle 2 mission. Analysis has revealed that the suspected ammonia's distribution is not consistent with this explanation.

Life on Mars?

The importance of ammonia is that it is a compound of nitrogen and hydrogen.

Nitrogen is rare in the Martian environment but because no form of terrestrial life can exist without it, the presence of ammonia may indicate that Martian microbial life is hoarding it.

"There are no known ways for ammonia to be present in the Martian atmosphere that do not involve life," the Nasa scientist said.

The twin US rovers that landed on the Red Planet in January will be unable to answer the question of the ammonia's origin as they are designed for geological work.

But future missions could include sensors to analyse the ammonia to determine if it has a biological or volcanic origin. Lava deposited on to the surface, or released underground, could produce the gas.


But, so far, no active volcanic hotspots have been detected on the planet by the many spacecraft currently in orbit.

Sunday, 22 June 2008

Mars probe makes 'ice discovery'

Tiny clumps of material in the bottom left of the trench on 15 June (left) are gone by 19 June (right)

Nasa's Phoenix lander has unearthed compelling evidence of ice on Mars, mission scientists believe.

Chunks of a bright material found in a trench dug by the craft have disappeared over four Martian days, suggesting they have vapourised.

While digging in another trench, the lander's arm connected with a hard surface at the same depth.

The finds lend weight to suggestions water is locked up in a permafrost layer close to the planet's surface.

Missing matter

"It must be ice,"
said Dr Peter Smith, Phoenix's principal investigator, who is based at the University of Arizona, Tucson.

"These little clumps completely disappearing over the course of a few days, that is perfect evidence that it's ice," he said.

"There had been some question whether the bright material was salt," he added.

"Salt can't do that."

The dice-sized chunks were unearthed in a trench informally known as Dodo-Goldilocks, which Phoenix dug and photographed on the 20th day of its stay on Mars.

Four days later when the trench was snapped again, some of the chunks had disappeared.

Earlier in the mission hopes of discovering ice were fading as soil samples scooped up earlier by Phoenix yielded no trace of water.

While evidence of ice on Mars has been gathered before, part of Phoenix's mission is to search out evidence to support the idea that the polar region of the planet could be habitable.

'Same depth'

Further confirmation of the ice theory came from another trench, known as Snow White 2.

Digging there was halted when the scraper on the lander's robotic arm hit a hard surface just under the soil layer.

"We have dug a trench and uncovered a hard layer at the same depth as the ice layer in our other trench," said Ray Arvidson of Washington University in St Louis, who is lead scientist for the robotic arm.

The arm also stopped three times earlier while digging in a "polygon".

This automatic reaction is a programmed response triggered when the scoop hits a hard, sub-surface region.

"Polygons" are soil features seen on Earth when permafrost layers in soil expand and contract as temperatures rise and fall.

Phoenix now seems to have confirmed that similar features on Mars are caused by the same processes as those on this planet.

Tuesday, 27 May 2008

Mars lander is 'in good health'


Polygon shape on ground (Nasa)
Polygon patterns are similar to those in permafrost regions on Earth

Nasa says its Phoenix spacecraft is in good health after making the first successful landing in the north polar region of Mars.

Images sent back show a flat valley floor with polygonal features that give the ground a "paved" appearance.

These are believed to be a sign of the water-ice that lies just beneath the surface at these high latitudes.

The ice should be within reach of the probe's 2.35m-long robotic arm, which is due to be deployed this week.

The arm can dig through the topsoil to the ice beneath and scoop up samples to return to the lander's deck for analysis.

Phoenix is set to investigate the planet's geological history and search for the chemical building blocks which could support life.

The polygons seen in the latest images have previously been spotted from space and are thought to be caused by expansion and contraction of ice. Similar features can be seen in permafrost regions on Earth.

MRO image of Phoenix parachuting through the atmosphere (Nasa)
A Nasa orbiter took this image of Phoenix parachuting to the surface
"We see the lack of rocks that we expected, we see the polygons that we saw from space, we don't see ice on the surface, but we think we will see it beneath the surface. It looks great to me," said Professor Peter Smith, principal investigator for the Phoenix mission.

But Professor Smith also mentioned that the polygons were smaller than expected.

Some scientists think there may be a large-scale polygonal structure to the Martian surface as seen from space. But from the ground, it seems there are polygons within polygons.

This suggests that water-ice could lie very near the surface indeed: the closer it is to the surface, the more fractured it becomes, leading to smaller polygon shapes.

A signal confirming the lander had reached the surface was received at 2353 GMT on 25 May (1953 EDT; 0053 BST on 26 May).

Engineers and scientists at Nasa's Jet Propulsion Laboratory (JPL) in California clapped and cheered when the landing signal came through.

Soft landing

The final seven minutes of the probe's 10-month journey to Mars were regarded as the hardest part of the mission.

The probe had to survive a fiery plunge through the planet's thin atmosphere, slowing from a speed of nearly 21,000km/h (13,000 mph).

It released a parachute, used pulsed thrusters to slow to a fast-walking speed, and then descended the last few metres to the Martian soil to land on three legs.

The Nasa team monitored each stage of the descent and landing process through radio messages relayed to Earth via the Odyssey satellite in orbit around Mars.

Phoenix lander
Phoenix carries seven science instruments

Nasa found out more about the landing when pictures from the probe reached the Earth.

The first pictures confirmed that the solar arrays needed for the mission's energy supply had unfolded properly, and masts for the stereo camera and weather station had swung into their correct vertical position.

HOW PHOENIX LANDED

Phoenix land and cruise stage hardware

Phoenix lander craft jettisons cruise- stage power equipment seven minutes before reaching Mars' atmosphere.

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"Seeing these images after a successful landing reaffirmed the thorough work over the past five years by a great team," said the mission's project manager Barry Goldstein, from JPL.

The spacecraft will begin its three-month science mission in the next few days.

Phoenix is an apt name for the current mission, as it rose from the ashes of two previous failures.

In September 1999, the Mars Climate Orbiter spacecraft crashed into the Red Planet following a navigation error caused when technicians mixed up "English" (imperial) and metric units.

A few months later, another Nasa spacecraft, the Mars Polar Lander (MPL), was lost near the planet's South Pole.

Phoenix uses hardware from an identical twin of MPL, the Mars Surveyor 2001 Lander, which was cancelled following the two consecutive failures.

The probe was launched on 4 August 2007 on a Delta II rocket from Cape Canaveral Air Force Station in Florida.

Phoenix landing site
Phoenix landed further north than previous missions