One of our patrons found this NASA paper on Curiosity wheel damage.
It's a study on how the rover could shed part of a wheel against a rock in order to prevent it from mangling up and damaging cabling.
The pictures are wild.
https://www-robotics.jpl.nasa.gov/publications/Arturo_Rankin/Rimmed_Wheel_Performance_on_the_Mars_Science_Laboratory_Scarecrow_Rover.pdf
Note that this test was an existence proof, not a systematic development. They showed that it is in fact possible to shed a detached inner rim after months of trial and error with immediate direct visual feedback. The singular success was not repeated.
First You See It, Then You Don’t: Scientists Closer to Explaining Mars Methane Mystery
Jun 29, 2021
Why do some science instruments detect the gas on the Red Planet while others don’t?
Reports of methane detections at Mars have captivated scientists and non-scientists alike. On Earth, a significant amount of methane is produced by microbes that help most livestock digest plants. This digestion process ends with livestock exhaling or burping the gas into the air.
While there are no cattle, sheep, or goats on Mars, finding methane there is exciting because it may imply that microbes were, or are, living on the Red Planet. Methane could have nothing to do with microbes or any other biology, however; geological processes that involve the interaction of rocks, water, and heat can also produce it.
Before identifying the sources of methane on Mars, scientists must settle a question that’s been gnawing at them: Why do some instruments detect the gas while others don’t? NASA’s Curiosity rover, for instance, has repeatedly detected methane right above the surface of Gale Crater. But ESA’s (the European Space Agency) ExoMars Trace Gas Orbiter hasn’t detected any methane higher in the Martian atmosphere.
“When the Trace Gas Orbiter came on board in 2016, I was fully expecting the orbiter team to report that there’s a small amount of methane everywhere on Mars,” said Chris Webster, lead of the Tunable Laser Spectrometer (TLS) instrument in the Sample Analysis at Mars (SAM) chemistry lab aboard the Curiosity rover.
The TLS has measured less than one-half part per billion in volume of methane on average in Gale Crater. That’s equivalent to about a pinch of salt diluted in an Olympic-size swimming pool. These measurements have been punctuated by baffling spikes of up to 20 parts per billion in volume.
“But when the European team announced that it saw no methane, I was definitely shocked,” said Webster, who’s based at NASA’s Jet Propulsion Laboratory in Southern California.
The European orbiter was designed to be the gold standard for measuring methane and other gases over the whole planet. At the same time, Curiosity’s TLS is so precise, it will be used for early warning fire detection on the International Space Station and for tracking oxygen levels in astronaut suits. It’s also been licensed for use at power plants, on oil pipelines, and in fighter aircraft, where pilots can monitor the oxygen and carbon dioxide levels in their face masks.
Still, Webster and the SAM team were jolted by the European orbiter findings and immediately set out to scrutinize the TLS measurements on Mars.
Some experts suggested that the rover itself was releasing the gas. “So we looked at correlations with the pointing of the rover, the ground, the crushing of rocks, the wheel degradation – you name it,” Webster said. “I cannot overstate the effort the team has put into looking at every little detail to make sure those measurements are correct, and they are.”
Webster and his team reported their results today in the Astronomy & Astrophysics journal.
As the SAM team worked to confirm its methane detections, another member of Curiosity’s science team, planetary scientist John E. Moores from York University in Toronto, published an intriguing prediction in 2019. “I took what some of my colleagues are calling a very Canadian view of this, in the sense that I asked the question: ‘What if Curiosity and the Trace Gas Orbiter are both right?’” Moores said.
Moores, as well as other Curiosity team members studying wind patterns in Gale Crater, hypothesized that the discrepancy between methane measurements comes down to the time of day they’re taken. Because it needs a lot of power, TLS operates mostly at night when no other Curiosity instruments are working. The Martian atmosphere is calm at night, Moores noted, so the methane seeping from the ground builds up near the surface where Curiosity can detect it.
The Trace Gas Orbiter, on the other hand, requires sunlight to pinpoint methane about 3 miles, or 5 kilometers, above the surface. “Any atmosphere near a planet’s surface goes through a cycle during the day,” Moores said. Heat from the Sun churns the atmosphere as warm air rises and cool air sinks. Thus, the methane that is confined near the surface at night is mixed into the broader atmosphere during the day, which dilutes it to undetectable levels. “So I realized no instrument, especially an orbiting one, would see anything,” Moores said.
Immediately, the Curiosity team decided to test Moores’ prediction by collecting the first high-precision daytime measurements. TLS measured methane consecutively over the course of one Martian day, bracketing one nighttime measurement with two daytime ones. With each experiment, SAM sucked in Martian air for two hours, continuously removing the carbon dioxide, which makes up 95% of the planet’s atmosphere. This left a concentrated sample of methane that TLS could easily measure by passing an infrared laser beam through it many times, one that’s tuned to use a precise wavelength of light that is absorbed by methane.
“John predicted that methane should effectively go down to zero during the day, and our two daytime measurements confirmed that,” said Paul Mahaffy, the principal investigator of SAM, who’s based at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. TLS’ nighttime measurement fit neatly within the average the team had already established. “So that’s one way of putting to bed this big discrepancy,” Mahaffy said.
While this study suggests that methane concentrations rise and fall throughout the day at the surface of Gale Crater, scientists have yet to solve the global methane puzzle at Mars. Methane is a stable molecule that is expected to last on Mars for about 300 years before getting torn apart by solar radiation. If methane is constantly seeping from all similar craters, which scientists suspect is likely given that Gale doesn’t seem to be geologically unique, enough of it should have accumulated in the atmosphere for the Trace Gas Orbiter to detect. Scientists suspect that something is destroying methane in less than 300 years.
Experiments are underway to test whether very low-level electric discharges induced by dust in the Martian atmosphere could destroy methane, or whether abundant oxygen at the Martian surface quickly destroys methane before it can reach the upper atmosphere.
“We need to determine whether there’s a faster destruction mechanism than normal to fully reconcile the data sets from the rover and the orbiter,” Webster said.
News Media Contact
Andrew Good
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-2433
[email protected]
Written by Lonnie Shekhtman
NASA’s Goddard Space Flight Center, Greenbelt, Md.
2021-130
Freely accessible article:
'Alien burp' may have been detected by NASA's Curiosity rover
https://www.livescience.com/curiosity-finds-alien-methane-source.html
Related paper:
Mars Methane Sources in Northwestern Gale Crater Inferred from Back-Trajectory Modeling
Abstract
During its five years of operation, the Sample Analysis at Mars (SAM) Tunable Laser Spectrometer (TLS) on board the Curiosity rover has detected six methane spikes above a low background abundance in Gale crater. The methane spikes are likely the consequence of nearby surface emission. Here we use inverse Lagrangian modeling techniques to identify probable upstream emission regions for these methane spikes at an unprecedented spatial resolution. Inside Gale crater, the northwestern crater floor casts the strongest influence on the detections. Outside Gale crater, the emission region with the strongest influence extends towards the north. The contrasting results from two consecutive methane measurements point to an active emission region to the west and the southwest of the Curiosity rover on the northwestern crater floor. The observed spike magnitude and frequency also favor emission sites on the northwestern crater floor, unless fast methane removal mechanisms that are unknown to date are at work.
https://www.researchsquare.com/article/rs-569847/v1
Some excitement about carbon-12-enriched samples having been detected by Curiosity on Gale surface highs is making the rounds. Apart from the much-hyped biological explanations everyone is jumping at, the possibility of the enrichment coming from UV-CO2 interactions (and a reducing early Martian atmosphere) is not ruled out and IMO much more likely. The cosmic coincidence of Mars passing through a typically 12C-enriched interstellar dust cloud is also plausible.
https://www.science.org/content/article/mars-rover-detects-carbon-signature-hints-past-life-source
Some excitement about carbon-12-enriched samples having been detected by Curiosity on Gale surface highs is making the rounds. Apart from the much-hyped biological explanations everyone is jumping at, the possibility of the enrichment coming from UV-CO2 interactions (and a reducing early Martian atmosphere) is not ruled out and IMO much more likely. The cosmic coincidence of Mars passing through a typically 12C-enriched interstellar dust cloud is also plausible.
https://www.science.org/content/article/mars-rover-detects-carbon-signature-hints-past-life-sourceOn what basis do you conclude it’s much more likely, show your working as they say?
After all reading the NASA press release as linked to below no one there appears to be offering one hypothesis as a preferable explanation over another at the moment.
https://www.nasa.gov/feature/goddard/2022/nasa-s-curiosity-rover-measures-intriguing-carbon-signature-on-mars
What's more, these processes mediated by life "require multiple steps with the CH4 consumed by the methanotrophs to be biological CH4 from microbial methanogenesis", in addition to an a-priori composition of the source CO2 more akin to magmatic rock carbon than that of the Martian atmosphere. So, a very fine-tuned set of unlikely hypothesis.
What's more, these processes mediated by life "require multiple steps with the CH4 consumed by the methanotrophs to be biological CH4 from microbial methanogenesis", in addition to an a-priori composition of the source CO2 more akin to magmatic rock carbon than that of the Martian atmosphere. So, a very fine-tuned set of unlikely hypothesis.Do those steps occur in terrestrial ecosystems or are supported by chemical analysis of very ancient geological chemistry on Earth?