jeudi 29 septembre 2016
Curiosity Finds Evidence of Mars Crust Contributing to Atmosphere
NASA - Mars Science Laboratory (MSL) logo.
Sept. 29, 2016
Image above: This low-angle self-portrait of NASA's Curiosity Mars rover shows the vehicle at the site from which it reached down to drill into a rock target called "Buckskin." The MAHLI camera on Curiosity's robotic arm took multiple images on Aug. 5, 2015, that were stitched together into this selfie. Image Credits: NASA/JPL-Caltech/MSSS.
NASA's Curiosity rover has found evidence that chemistry in the surface material on Mars contributed dynamically to the makeup of its atmosphere over time. It’s another clue that the history of the Red Planet’s atmosphere is more complex and interesting than a simple legacy of loss.
The findings come from the rover’s Sample Analysis at Mars, or SAM, instrument suite, which studied the gases xenon and krypton in Mars’ atmosphere. The two gases can be used as tracers to help scientists investigate the evolution and erosion of the Martian atmosphere. A lot of information about xenon and krypton in Mars’ atmosphere came from analyses of Martian meteorites and measurements made by the Viking mission.
Image above: Chemistry that takes place in the surface material on Mars can explain why particular xenon (Xe) and krypton (Kr) isotopes are more abundant in the Martian atmosphere than expected. The isotopes – variants that have different numbers of neutrons – are formed in the loose rocks and material that make up the regolith. The chemistry begins when cosmic rays penetrate into the surface material. If the cosmic rays strike an atom of barium (Ba), the barium can lose one or more of its neutrons (n0). Atoms of xenon can pick up some of those neutrons – a process called neutron capture – to form the isotopes xenon-124 and xenon-126. In the same way, atoms of bromine (Br) can lose some of their neutrons to krypton, leading to the formation of krypton-80 and krypton-82 isotopes. These isotopes can enter the atmosphere when the regolith is disturbed by impacts and abrasion and gas escapes from the regolith. Image Credits: NASA's Goddard Space Flight Center.
“What we found is that earlier studies of xenon and krypton only told part of the story,” said Pamela Conrad, lead author of the report and SAM’s deputy principal investigator at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “SAM is now giving us the first complete in situ benchmark against which to compare meteorite measurements.”
Of particular interest to scientists are the ratios of certain isotopes – or chemical variants – of xenon and krypton. The SAM team ran a series of first-of-a-kind experiments to measure all the isotopes of xenon and krypton in the Martian atmosphere. The experiments are described in a paper published in Earth and Planetary Science Letters.
The team’s method is called static mass spectrometry, and it’s good for detecting gases or isotopes that are present only in trace amounts. Although static mass spectrometry isn’t a new technique, its use on the surface of another planet is something only SAM has done.
Overall, the analysis agreed with earlier studies, but some isotope ratios were a bit different than expected. When working on an explanation for those subtle but important differences, the researchers realized that neutrons might have gotten transferred from one chemical element to another within the surface material on Mars. The process is called neutron capture, and it would explain why a few selected isotopes were more abundant than previously thought possible.
In particular, it looks as if some of the barium surrendered neutrons that got picked up by xenon to produce higher-than-expected levels of the isotopes xenon-124 and 126. Likewise, bromine might have surrendered some of its neutrons to produce unusual levels of krypton-80 and krypton-82.
Image above: The Sample Analysis at Mars instrument suite on NASA’s Curiosity rover. Image Credits: NASA's Goddard Space Flight Center.
These isotopes could have been released into the atmosphere by impacts on the surface and by gas escaping from the regolith, which is the soil and broken rocks of the surface.
“SAM’s measurements provide evidence of a really interesting process in which the rock and unconsolidated material at the planet’s surface have contributed to the xenon and krypton isotopic composition of the atmosphere in a dynamic way,” said Conrad.
The atmospheres of Earth and Mars exhibit very different patterns of xenon and krypton isotopes, particularly for xenon-129. Mars has much more of it in the atmosphere than does Earth.
“The unique capability to measure in situ the six and nine different isotopes of krypton and xenon allows scientists to delve into the complex interactions between the Martian atmosphere and crust,” said Michael Meyer, lead scientist for the Mars Exploration Program at NASA Headquarters in Washington. “Discovering these interactions through time allows us to gain a greater understanding of planetary evolution.”
NASA’s Mars Science Laboratory Project is using Curiosity to determine if life was possible on Mars and study major changes in Martian environmental conditions. NASA studies Mars to learn more about our own planet, and in preparation for future human missions to Mars. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the project for NASA’s Science Mission Directorate in Washington.
For more information about SAM, visit: http://ssed.gsfc.nasa.gov/sam/
SAM experiment data are archived in the Planetary Data System, online at: http://pds.nasa.gov/
For more information about Curiosity, visit: http://www.nasa.gov/msl
The research paper is available at: http://dx.doi.org/10.1016/j.epsl.2016.08.028
Images (mentioned), Text, Credits: NASA’s Goddard Space Flight Center, written by Elizabeth Zubritsky/JPL/Guy Webster/Karl Hille.
Publié par Orbiter.ch à 15:52