Author Topic: Mars Rover Curiosity  (Read 36143 times)

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Re: Mars Rover Curiosity
« Reply #120 on: November 19, 2014, 09:56:22 AM »

Fine-Grained, Finely Layered Rock at Base of Martian Mount Sharp

This patch of Martian bedrock, about 2 feet (70 centimeters) across, is finely layered rock with some pea-size inclusions. It lies near the lowest point of the "Pahrump Hills" outcrop, which forms part of the basal layer of Mount Sharp. Curiosity's Mastcam acquired this view on Nov. 9, 2014.


Erosion Resistance at 'Pink Cliffs' at Base of Martian Mount Sharp

This small ridge, about 3 feet long, appears to resist wind erosion more than the flatter plates around it. Such differences are among the traits NASA's Curiosity Mars rover is examining at selected rock targets at the base of Mount Sharp. Curiosity's Mastcam acquired this view on Oct. 7, 2014


Ripple's Interior Exposed by Rover Wheel Track (Labeled)

A wheel track cuts through a windblown ripple of dusty sand in this Nov. 7, 2014, image from the Mastcam on NASA's Curiosity rover. The view spans about four feet across. This experiment was planned for yielding a view of the inside of the ripple for assessment of particle sizes and composition.

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Re: Mars Rover Curiosity
« Reply #121 on: November 28, 2014, 09:47:53 AM »


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This view shows the path and some key places in a survey of the "Pahrump Hills" outcrop by NASA's Curiosity Mars rover in autumn of 2014. The outcrop is at the base of Mount Sharp within Gale Crater.

The mission's in-place investigation of the layered mountain began at the low edge of the Pahrump Hills outcrop, at the target "Confidence Hills." Curiosity collected a drilled sample of rock powder at that target in September 2014 and delivered portions of the powder into analytical instruments inside the rover. Then the mission began a "walkabout" of the outcrop, similar to the way field geologists on Earth walk across an outcrop to choose the best places on it to examine in detail. The dashed gold line indicates the path the rover drove during the walkabout. Names are shown for a few of the features visited and observed by the rover. Red dots indicate stops at the end of a day's drive. White dots indicate locations of stops made during the drives to collect observations of the Pahrump Hills outcrop. The mission completed the walkabout at the site labeled "Whale Rock," and the team is now examining the observations acquired during the walkabout to decide where to return for more detailed analysis.

This view of the outcrop and other portions of Mount Sharp beyond is a mosaic of images taken by the rover's Mast Camera (Mastcam). A larger version of the mosaic is at PIA18608

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Re: Mars Rover Curiosity
« Reply #122 on: December 09, 2014, 09:23:09 AM »
http://www.newscientist.com/article/dn26675-curiosity-rover-finds-ancient-lake-in-martian-crater.html

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Curiosity rover finds ancient lake in Martian crater
21:05 08 December 2014 by Lisa Grossman

Gale Crater on Mars was once a large lake that could have stuck around long enough for life to get started. New observations from the Curiosity rover, which has been driving around the now-dry crater floor since August 2012, show evidence of multiple cycles of water flowing into a large, shallow lake that could have lasted tens of millions of years.

Since shortly after it landed, Curiosity has been driving toward Mount Sharp, the 5-kilometre-high mountain at the crater's centre. It reached the mountain's foothills in September, and the team is busy drilling and analysing the rocks there in pursuit of the rover's primary mission: finding sings that Mars was once hospitable to life.

The view from the road looked optimistic. On the way to Mount Sharp, Curiosity found evidence for flowing rivers and fresh water where simple microbes could have made themselves at home.

But two major questions remained: was that water there long enough to support the emergence of life? And how did Mount Sharp form in the first place?




Ancient basin
In a news conference today, the rover team presented a possible answer to both questions: Gale Crater was filled up with a lake that dried out and reappeared several times in the distant past, laying down the sediments that make up Mount Sharp in bursts of hundreds of thousands to millions of years.

In its drive towards the mountain, Curiosity first encountered conglomerate rocks full of pebbles that were probably deposited by rivers. But as it continued south and uphill, the landscape changed to sandstones that were all tilted in the same direction: towards the mountain.

"This presents a certain paradox," says project scientist John Grotzinger of the California Institute of Technology in Pasadena. "If Mount Sharp had been there and water had been flowing off Mount Sharp, it would be flowing downhill to the north. But the rocks that are exposed show the water flowing to the south."

The resolution of the paradox is that Mount Sharp was not there when the water started flowing. Instead, water flowed from the crater rim toward the interior, filling up an ancient lake.

"On Earth, one of the key places where we find these inclined beds are at the mouths of river channels where they feed into lakes," said Curiosity team member Sanjeev Gupta of Imperial College London. The landscape looks like small deltas stacked on top of each other, suggesting they formed over several cycles of varying climate.

Mountain of sediment
At the base of Mount Sharp, sandstone layers become much thinner and flatter, as if they were laid down more slowly and without strong currents swirling them around.

"We think that's what we're seeing here: lake floor deposits," Grotzinger says. Cycles of wet and dry periods could have filled up the crater with sediment that was later eroded, leaving the mountain that remains today.



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Re: Mars Rover Curiosity
« Reply #123 on: December 09, 2014, 11:42:04 AM »
<a href="http://www.youtube.com/v/oS99yR1cooE" target="_blank" rel="noopener noreferrer" class="bbc_link bbc_flash_disabled new_win">http://www.youtube.com/v/oS99yR1cooE</a>


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Re: Mars Rover Curiosity
« Reply #124 on: December 16, 2014, 03:25:58 PM »
Organic compounds confirmed!   8)

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Re: Mars Rover Curiosity
« Reply #125 on: December 16, 2014, 03:29:13 PM »
http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1767

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NASA's Mars Curiosity rover has measured a tenfold spike in methane, an organic chemical, in the atmosphere around it and detected other organic molecules in a rock-powder sample collected by the robotic laboratory's drill.
"This temporary increase in methane -- sharply up and then back down -- tells us there must be some relatively localized source," said Sushil Atreya of the University of Michigan, Ann Arbor, a member of the Curiosity rover science team. "There are many possible sources, biological or non-biological, such as interaction of water and rock."

Researchers used Curiosity's onboard Sample Analysis at Mars (SAM) laboratory a dozen times in a 20-month period to sniff methane in the atmosphere. During two of those months, in late 2013 and early 2014, four measurements averaged seven parts per billion. Before and after that, readings averaged only one-tenth that level.

Curiosity also detected different Martian organic chemicals in powder drilled from a rock dubbed Cumberland, the first definitive detection of organics in surface materials of Mars. These Martian organics could either have formed on Mars or been delivered to Mars by meteorites.

Organic molecules, which contain carbon and usually hydrogen, are chemical building blocks of life, although they can exist without the presence of life. Curiosity's findings from analyzing samples of atmosphere and rock powder do not reveal whether Mars has ever harbored living microbes, but the findings do shed light on a chemically active modern Mars and on favorable conditions for life on ancient Mars.

"We will keep working on the puzzles these findings present," said John Grotzinger, Curiosity project scientist of the California Institute of Technology in Pasadena. "Can we learn more about the active chemistry causing such fluctuations in the amount of methane in the atmosphere? Can we choose rock targets where identifiable organics have been preserved?"

Researchers worked many months to determine whether any of the organic material detected in the Cumberland sample was truly Martian. Curiosity's SAM lab detected in several samples some organic carbon compounds that were, in fact, transported from Earth inside the rover. However, extensive testing and analysis yielded confidence in the detection of Martian organics.

Identifying which specific Martian organics are in the rock is complicated by the presence of perchlorate minerals in Martian rocks and soils. When heated inside SAM, the perchlorates alter the structures of the organic compounds, so the identities of the Martian organics in the rock remain uncertain.

"This first confirmation of organic carbon in a rock on Mars holds much promise," said Curiosity Participating Scientist Roger Summons of the Massachusetts Institute of Technology in Cambridge. "Organics are important because they can tell us about the chemical pathways by which they were formed and preserved. In turn, this is informative about Earth-Mars differences and whether or not particular environments represented by Gale Crater sedimentary rocks were more or less favorable for accumulation of organic materials. The challenge now is to find other rocks on Mount Sharp that might have different and more extensive inventories of organic compounds."
Researchers also reported that Curiosity's taste of Martian water, bound into lakebed minerals in the Cumberland rock more than three billion years ago, indicates the planet lost much of its water before that lakebed formed and continued to lose large amounts after.

SAM analyzed hydrogen isotopes from water molecules that had been locked inside a rock sample for billions of years and were freed when SAM heated it, yielding information about the history of Martian water. The ratio of a heavier hydrogen isotope, deuterium, to the most common hydrogen isotope can provide a signature for comparison across different stages of a planet's history.

"It's really interesting that our measurements from Curiosity of gases extracted from ancient rocks can tell us about loss of water from Mars," said Paul Mahaffy, SAM principal investigator of NASA's Goddard Space Flight Center in Greenbelt, Maryland, and lead author of a report published online this week by the journal Science

The ratio of deuterium to hydrogen has changed because the lighter hydrogen escapes from the upper atmosphere of Mars much more readily than heavier deuterium. In order to go back in time and see how the deuterium-to-hydrogen ratio in Martian water changed over time, researchers can look at the ratio in water in the current atmosphere and water trapped in rocks at different times in the planet's history.

Martian meteorites found on Earth also provide some information, but this record has gaps. No known Martian meteorites are even close to the same age as the rock studied on Mars, which formed about 3.9 billion to 4.6 billion years ago, according to Curiosity's measurements.

The ratio that Curiosity found in the Cumberland sample is about one-half the ratio in water vapor in today's Martian atmosphere, suggesting much of the planet's water loss occurred since that rock formed. However, the measured ratio is about three times higher than the ratio in the original water supply of Mars, based on the assumption that supply had a ratio similar to that measured in Earth's oceans. This suggests much of Mars' original water was lost before the rock formed.

Curiosity is one element of NASA's ongoing Mars research and preparation for a human mission to Mars in the 2030s. Caltech manages the Jet Propulsion Laboratory in Pasadena, California, and JPL manages Curiosity rover science investigations for NASA's Science Mission Directorate in Washington. The SAM investigation is led by Paul Mahaffy of Goddard. Two SAM instruments key in these discoveries are the Quadrupole Mass Spectrometer, developed at Goddard, and the Tunable Laser Spectrometer, developed at JPL.
The results of the Curiosity rover investigation into methane detection and the Martian organics in an ancient rock were discussed at a news briefing Tuesday at the American Geophysical Union's convention in San Francisco. The methane results are described in a paper published online this week in the journal Science by NASA scientist Chris Webster of JPL, and co-authors.

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Re: Mars Rover Curiosity
« Reply #126 on: December 16, 2014, 03:37:17 PM »


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The 5-meter drive planned for Sol 837 placed the rover near dubbed "Whale Rock" as intended.

Front Hazcam images show blocks that appear to have fallen from the outcrop and in-place bedrock patches; both can be reached by the arm instruments, so the Sol 840 plan includes MAHLI images from 25 cm standoff distance of the block and bedrock targets "San Andreas," "Tecoya," "Gem Hill" and "San Bernardino."  The arm will also be used to image the wheels and clean out CHIMRA (the sample handling equipment).

I'm SOWG Chair today, and all has gone well so far.  But, as usual, the risk of rover slip must be assessed before arm activities can be planned.  The rover is now tilted over 18 degrees, more than it has been tilted for any arm activities during the mission so far, so slip risk assessment requires more time and effort than it has in the past.  As I write this, we are still "go" for arm activities, and of course I'm hoping that won't change. 

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Re: Mars Rover Curiosity
« Reply #127 on: December 16, 2014, 08:58:10 PM »
Per BBC:

Methane 'belches' detected on Mars




Nasa's Curiosity rover has detected methane on Mars - a gas that could hint at past or present life on the planet.

The robot sees very low-level amounts constantly in the background, but it also has monitored a number of short-lived spikes that are 10 times higher.

Methane on the Red Planet is intriguing because here on Earth, 95% of the gas comes from microbial organisms.

Researchers have hung on to the hope that the molecule's signature at Mars might also indicate a life presence.

The Curiosity team cannot identify the source of its methane, but the leading candidate is underground stores that are periodically disturbed.

Curiosity scientist Sushil Atreya said it was possible that so-called clathrates were involved.

"These are molecular cages of water-ice in which methane gas is trapped. From time to time, these could be destabilised, perhaps by some mechanical or thermal stress, and the methane gas would be released to find its way up through cracks or fissures in the rock to enter the atmosphere," the University of Michigan professor told BBC News.

He was reporting the discovery here at the American Geophysical Union Fall Meeting.

The question remains, of course, of how the methane (CH4) got into the clathrate stores in the first place.

It could have come from Martian bugs; it could also have come from a natural process, such as serpentinisation, which sees methane produced when water interacts with certain rock types.

At the moment, it is all speculation. But at least Curiosity has now made the detection.
Enriched samples

It was concerning that for many months the robot could not see a gas that was being observed by orbiting spacecraft at Mars and by telescopes at Earth.

People were beginning to wonder if the other sightings were reliable.

Curiosity is located in a deep bowl on Mars' equator known as Gale Crater.

It has been sucking in Martian air and scanning its components since shortly after landing in August 2012.

For gases that have very low concentrations in the atmosphere, the robot can employ a special technique in which it expels the most abundant molecule - carbon dioxide - before analysing the sample.

This has the effect of enriching and amplifying any residual chemistry.

And in doing this for methane, Curiosity finds that there is a persistent signature of about 0.7 parts per billion by volume (ppbv).

"The background figure suggests there are about 5,000 tonnes of methane in the atmosphere," said Dr Chris Webster, from Nasa's Jet Propulsion Laboratory, who led the investigation.

"You can compare that with Earth where there are about 500 million tonnes. The concentration here at Earth is about 1,800 ppbv."
Life's preference

The spikes in methane that Curiosity saw occurred on four occasions during the course of a two-month period.

They varied between about 7 and 9 parts per billion by volume.

It is likely, the team says, that the gas is being released relatively nearby, either within the crater or just outside.

Curiosity's weather station suggests it is blowing in from the north, from the direction of the crater rim.

One way to investigate whether the methane on Mars has a biological or a geological origin would be to study the types, or isotopes, of carbon atom in the gas.

On Earth, life favours a lighter version of the element (carbon-12), over a heavier one (carbon-13).

A high C-12 to C-13 ratio in ancient Earth rocks has been interpreted as evidence that biological activity existed on our world as much as four billion years ago.

If scientists could find similar evidence on Mars, it would be startling. But, sadly, the volumes of methane detected by Curiosity are simply too small to run this kind of experiment.

"If we had enriched our sample during one of the peaks, we might have had a shot at looking at these isotopes," explained Dr Paul Mahaffy, the lead investigator on Curiosity's Surface Analysis at Mars (SAM) instrument, which did the measurements.

"I think there is still some hope. If the methane comes back, and we can enrich it, we'll certainly be trying."
Long quest

The other big Curiosity discovery announced here in San Francisco is that the rover has also confirmed the detection of organic (carbon-rich) compounds in the rock samples it has been drilling.

It is the first definitive detection of organics in surface materials at the Red Planet.

The SAM instrument saw evidence for chlorobenzine in the powered rock it pulled up from a mudstone slab dubbed Cumberland.

Chlorobenzine is a carbon ring with five hydrogen atoms and one chlorine atom attached.

The team cannot be sure if the chemical was specifically present in Cumberland or synthesised during the heating of analysis. But even if the latter is the case, the scientists seem confident the molecule would at the very least have been derived from larger carbon structures that were in place.

Once again, scientists are interested in seeing such organics because life as we know it can only exist if it has the capacity to trade in carbon molecules.

If they are not present then neither will there be any biology. However, just as with the methane detection, this does not of itself automatically point to life on Mars, now or in the past, because there are plenty of abiotic processes that will produce complex carbon structures as well.

"It's a big day for us - it's a kind of crowning moment of 10 years of hard work - where we report there is methane in the atmosphere and there are also organic molecules in abundance in the sub-surface," commented Curiosity project scientist Prof John Grotzinger.

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Re: Mars Rover Curiosity
« Reply #128 on: January 08, 2015, 10:20:35 AM »


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Re: Mars Rover Curiosity
« Reply #129 on: January 15, 2015, 01:57:44 PM »
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The "mini-drill" test on the Mojave rock target completed successfully, but MAHLI images taken after the test showed that the rotary-percussive drilling fractured the rock.  This was not expected, so the tactical team had to quickly change the Sol 869-870 plan.  While we were hoping to drill a deeper hole and acquire a sample of the drill cuttings before the upgrade of the software onboard the rover next week, the rock fragments dislodged by the mini-drill activity provided a rare opportunity to examine freshly-broken surfaces.  Field geologists usually carry rock hammers so that they can break rocks and examine the fresh surfaces.  On Mars, the drill has served as MSL's rock hammer!  So the Sol 869 plan includes ChemCam measurements of the fresh chunk of rock and the bottom of the mini-drill hole, followed by MAHLI close-up images of the dislodged rocks, both during the day and at night (illuminated by the LEDs).  On Sol 870, the brush will be used to clean off another potential mini-drill target, dubbed "Funk Valley."  MAHLI images of this new target will be taken before and after the brushing, then the drill will be "preloaded" (pushed down) against Funk Valley and a potential full drill target to determine whether the rock is strong enough to safely drill.  Finally, MAHLI images will be acquired to see the results of the preload tests and the APXS will be placed on the brushed spot for an overnight integration. 

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Re: Mars Rover Curiosity
« Reply #130 on: January 30, 2015, 08:12:40 AM »




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Re: Mars Rover Curiosity
« Reply #131 on: February 09, 2015, 09:56:14 AM »


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02.05.2015

NASA's Curiosity Analyzing Sample of Martian Mountain

-- Analysis underway of Curiosity's second drilled rock sample at Mount Sharp
 -- Preliminary results suggest acidic ancient conditions
 -- New drilling technique uses less-forceful hammering on fragile rock

The second bite of a Martian mountain taken by NASA's Curiosity Mars rover hints at long-ago effects of water that was more acidic than any evidenced in the rover's first taste of Mount Sharp, a layered rock record of ancient Martian environments.

The rover used a new, low-percussion-level drilling technique to collect sample powder last week from a rock target called "Mojave 2."

Curiosity reached the base of Mount Sharp five months ago after two years of examining other sites inside Gale Crater and driving toward the mountain at the crater's center. The first sample of the mountain's base layer came from a target called "Confidence Hills," drilled in September.

A preliminary check of the minerals in the Mojave 2 sample comes from analyzing it with the Chemistry and Mineralogy (CheMin) instrument inside Curiosity. The still-partial analysis shows a significant amount of jarosite, an oxidized mineral containing iron and sulfur that forms in acidic environments.

"Our initial assessment of the newest sample indicates that it has much more jarosite than Confidence Hills," said CheMin Deputy Principal Investigator David Vaniman, of the Planetary Science Institute, Tucson, Arizona. The minerals in Confidence Hills indicate less acidic conditions of formation.

Open questions include whether the more acidic water evident at Mojave 2 was part of environmental conditions when sediments building the mountain were first deposited, or fluid that soaked the site later.

Both target sites lie in a outcrop called "Pahrump Hills," an exposure of the Murray formation that is the basal geological unit of Mount Sharp. The Curiosity mission team has already proposed a hypothesis that this mountain, the size of Mount Rainier in Washington, began as sediments deposited in a series of lakes filling and drying.

In the months between Curiosity's drilling of these two targets, the rover team based at NASA's Jet Propulsion Laboratory, Pasadena, California, directed the vehicle through an intensive campaign at Pahrump Hills. The one-ton roving laboratory zig-zagged up and down the outcrop's slope, using cameras and spectrometer instruments to study features of interest at increasing levels of detail. One goal was to select which targets, if any, to drill for samples to be delivered into the rover's internal analytical instruments.

The team chose a target called "Mojave," largely due to an abundance of slender features, slightly smaller than rice grains, visible on the rock surface. Researchers sought to determine whether these are salt-mineral crystals, such as those that could result from evaporation of a drying lake, or if they have some other composition. In a preparatory drilling test of the Mojave target, the rock broke. This ruled out sample-collection drilling at that spot, but produced chunks with freshly exposed surfaces to be examined.

Mojave 2, an alternative drilling target selected at the Mojave site, has the same type of crystal-shaped features. The preliminary look at CheMin data from the drilled sample material did not identify a clear candidate mineral for these features. Possibly, minerals that originally formed the crystals may have been replaced by other minerals during later periods of wet environmental conditions.

The drilling to collect Mojave 2 sample material might not have succeeded if the rover team had not recently expanded its options for operating the drill.

"This was our first use of low-percussion drilling on Mars, designed to reduce the energy we impart to the rock," said JPL's John Michael Morookian, the team's surface science and sampling activity lead for the Pahrump Hills campaign. "Curiosity's drill is essentially a hammer and chisel, and this gives us a way not to hammer as hard."

Extensive tests on Earth validated the technique after the team became concerned about fragility of some finely layered rocks near the base of Mount Sharp.

The rover's drill has six percussion-level settings ranging nearly 20-fold in energy, from tapping gently to banging vigorously, all at 30 times per second. The drill monitors how rapidly or slowly it is penetrating the rock and autonomously adjusts its percussion level. At the four targets before Mojave 2 -- including three before Curiosity reached Mount Sharp -- sample-collection drilling began at level four and used an algorithm that tended to remain at that level. The new algorithm starts at level one, then shifts to a higher level only if drilling progress is too slow. The Mojave 2 rock is so soft, the drill reached its full depth of about 2.6 inches (6.5 centimeters) in 10 minutes using just levels one and two of percussion energy.

Curiosity has also delivered Mojave 2 powder to the internal Sample Analysis at Mars (SAM) suite of instruments, for chemical analysis. The rover may drive to one or more additional sampling sites at Pahrump Hills before heading higher on Mount Sharp.

NASA's Mars Science Laboratory Project is using Curiosity to assess ancient habitable environments and major changes in Martian environmental conditions. JPL, a division of the California Institute of Technology in Pasadena, built the rover and manages the project for NASA's Science Mission Directorate in Washington.

For more information about Curiosity, visit:

http://www.nasa.gov/msl
http://mars.nasa.gov/msl/

You can follow the mission on Facebook and Twitter at:

http://www.facebook.com/marscuriosity
http://www.twitter.com/marscuriosity

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Re: Mars Rover Curiosity
« Reply #132 on: February 17, 2015, 10:43:57 AM »
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Re: Mars Rover Curiosity
« Reply #133 on: March 04, 2015, 11:00:25 AM »

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This raw-color view from Curiosity's Mastcam shows the rover's drill just after finishing a drilling operation at "Telegraph Peak" on Feb. 24, 2015. Three days later, a fault-protection action by the rover halted a process of transferring sample powder that was collected during this drilling. Credit: NASA/JPL-Caltech/MSSS

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NASA's Curiosity Mars rover is expected to remain stationary for several days of engineering analysis following an onboard fault-protection action on Feb. 27 that halted a process of transferring sample material between devices on the rover's robotic arm.
Telemetry received from the rover indicated that a transient short circuit occurred and the vehicle followed its programmed response, stopping the arm activity underway at the time of the irregularity in the electric current.

"We are running tests on the vehicle in its present configuration before we move the arm or drive," said Curiosity Project Manager Jim Erickson, of NASA's Jet Propulsion Laboratory in Pasadena, California. "This gives us the best opportunity to determine where the short is."

A transient short in some systems on the rover would have little effect on rover operations. In others, it could prompt the rover team to restrict use of a mechanism.

When the fault occurred, the rover was conducting an early step in the transfer of rock powder collected by the drill on the arm to laboratory instruments inside the rover. With the drill bit pointed up and the drill's percussion mechanism turned on, the rock powder was descending from collection grooves in the bit assembly into a chamber in the mechanism that sieves and portions the sample powder. The sample powder is from a rock target called "Telegraph Peak." The same transfer process was completed smoothly with samples from five previous drilling targets in 2013 and 2014.

NASA's Mars Science Laboratory Project is using Curiosity to assess ancient habitable environments and major changes in Martian environmental conditions. JPL, a division of the California Institute of Technology in Pasadena, built the rover and manages the project for NASA's Science Mission Directorate in Washington. For more information about Curiosity, visit:

http://www.nasa.gov/msl
http://mars.nasa.gov/msl/

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Re: Mars Rover Curiosity
« Reply #134 on: March 13, 2015, 09:37:43 AM »
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MARS SCIENCE LABORATORY MISSION STATUS REPORT

NASA's Curiosity Mars rover used its robotic arm Wednesday, March 11, to sieve and deliver a rock-powder sample to an onboard instrument. The sample was collected last month before the team temporarily suspended rover arm movement pending analysis of a short circuit.

The Chemistry and Mineralogy (CheMin) analytical instrument inside the rover received the sample powder. This sample comes from a rock target called "Telegraph Peak," the third target drilled during about six months of investigating the "Pahrump Hills" outcrop on Mount Sharp. With this delivery completed, the rover team plans to drive Curiosity away from Pahrump Hills in coming days.

"That precious Telegraph Peak sample had been sitting in the arm, so tantalizingly close, for two weeks. We are really excited to get it delivered for analysis," said Curiosity Project Scientist Ashwin Vasavada of NASA's Jet Propulsion Laboratory, Pasadena, California.

The rover experienced a short circuit on Feb. 27 while using percussion action in its drill to shake sample powder from the drill into a sample-processing device on the arm. Subsequent testing at JPL and on Curiosity has identified the likely cause as a transient short in the motor for the drill's percussion action. During several tests on the rover in the past 10 days, the short was reproduced only one time -- on March 5. It lasted less than one one-hundredth of a second and did not stop the motor. Ongoing analysis will help the rover team develop guidelines for best use of the drill at future rock targets.

The rover's path toward higher layers of Mount Sharp will take it first through a valley called "Artist's Drive," heading southwestward from Pahrump Hills. The sample-processing device on the arm is carrying Telegraph Peak sample material at the start of the drive, for later delivery into the Sample Analysis at Mars (SAM) suite of instruments. The delivery will occur after SAM prepares for receiving the sample.

Curiosity's drill has used a combination of rotary and percussion action to collect samples from six rock targets since the rover landed inside Gale Crater in 2012. The first sampled rock, "John Klein," in the Yellowknife Bay area near the landing site, provided evidence for meeting the mission's primary science goal. Analysis of that sample showed that early Mars offered environmental conditions favorable for microbial life, including the key elemental ingredients for life and a chemical energy source such as used by some microbes on Earth. In the layers of lower Mount Sharp, the mission is pursuing evidence about how early Mars environments evolved from wetter to drier conditions.

JPL, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory project for NASA's Science Mission Directorate, Washington, and built the project's Curiosity rover. For more information about Curiosity, visit:

http://www.nasa.gov/msl
http://mars.nasa.gov/msl/


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Curiosity Heading Away from 'Pahrump Hills'

This area at the base of Mount Sharp on Mars includes a pale outcrop, called "Pahrump Hills," that NASA's Curiosity Mars rover investigated from September 2014 to March 2015, and the "Artist's Drive" route toward higher layers of the mountain. Credit: NASA/JPL-Caltech/Univ. of Arizona