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[EN VIDÉO] On Mars, the Jezero crater delta This panorama of the Jezero crater delta is the work of the Mastcam-Z on board NASA’s Perseverance rover. This delta was formed billions of years ago from sediment transported by an ancient river to the mouth of a lake that once existed in the crater. These images were taken while the rover was in the southern region of Séítah where it found traces of igneous rocks. © JPLraw
In 1976, the American landers were landing viking on the Martian surface with the objective, among other things, of determining the presence, past or present, of life on our neighboring planet. Among the various on-board experiments, the results of one of them still remain controversial today: during the experiment ” Labeled Release “, the robotic arm of the lander moistened a sample of Martian soil using a aqueous solution water enriched with a few organic molecules followed by carbon 14 (isotope radioactive carbon). Thus, an increase in the concentration of CO2 radioactive (or other gas carbonaceous) could be interpreted as the result of the metabolization of organic molecules in the solution by microorganisms present in the soil sample.
And the results of the experiments, still debated more than forty years later, were surprising to say the least: immediately after injection of the aqueous solution, a constant flow of radioactive carbon gases was measured at the outlet of the soil sample. Note that the experiment was carried out twice by the landers Viking 1 and 2, one with a sample of regoliththe other with a soil sample contained under a rock.
An abiotic origin?
But, for many exobiologists, these results do not constitute formal proof of biological activity: gas production was always measured after the sterilization of the sample (heated for 3 hours at 160°C). To top it off, further experimentation from the Viking missions revealed no trace of organic compounds in the samples. Thus, many scientists agree that these emissions of gas were probably due to abiotic chemical reactions. Some then point the finger at the presence of highly reagents and rich in oxygen in Martian soils: according to them, such compounds, such as superoxides, peroxides or even perchlorates, could react to the presence of water liquid to release oxidized ions. The presence of such compounds has already been confirmed on the surface of Mars.
A double-edged sword
Such reagents could have disastrous consequences for future manned missions: highly corrosive, these compounds could damage machinery or attack the combinations ofastronautsor even burn their skin or damage their lungs. They would also have such an effect that they would be able to erase all traces of life fossil.
A team of scientists from the National Polytechnic University of Athens and the University of Patras then sought to develop a means of detecting and mapping the presence of these compounds on the Martian surface, by designing a device the size of a pocket book in which soil samples would be brought into contact with water in order to generate reactions (boosted under the action of catalysts) similar to those observed by Viking lander experiments. In addition to reducing the surface area likely to contain traces of fossil life, mapping these compounds could be vital to allow future manned missions to avoid these potentially hazardous areas.
But the scientists do not stop there: according to them, these soils could also be used to produce almost infinite quantities of oxygen, usable for future Martian bases. The project, sponsored by theESAtherefore also includes the design of a first prototype reactor to periodically extract oxygen from the Martian soil.
The team has so far only carried out tests using soil samples from the deserts Mojave and Atacama, with characteristics close to those of Martian soils; but for the sake of accuracy, scientists are now looking to produce a synthetic Martian regolith, or to use Martian meteorites for their tests.
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