Thousands of RSL sites have been identified on Martian slopes surface, in about 50 hilly regions spread out between the north and south midlatitudes, according to the statement from NASA. The streaks appear during warm seasons and shrink or disappear during winter. Similar features on Earth are only caused by "seeping water," officials said in the statement, but "how they form in the dry Martian environment remains unclear."
The new study offers an alternative explanation to flowing water.
When sand and other granular materials are lumped into piles, the material locks into place until the pile reaches a certain height. At that point, some of the grains begin to slip and flow smoothly down the sides, forming rivulets. Those rivers of material could appear darker than the material around them, according to the statement, and thus could explain the RSL.
And there's another key piece of evidence that the authors point to in support of this hypothesis: For a given type of granular material (such as sand), there is a specific angle at which those rivulets can form, and it's known as the "angle of repose." The authors show that the RSL that have been observed so far only appear on hillsides that reach the angle of repose for sand dunes. If the RSL sites were created by water, the authors postulate that these features should also appear on gentler slopes.
"The RSL don't flow onto shallower slopes, and the lengths of these are so closely correlated with the dynamic angle of repose, it can't be a coincidence," Alfred McEwen, a professor of planetary geology at the University of Arizona, Tucson, said in the statement. McEwen is the HiRISE Principal Investigator and a co-author of the new report.
The research also relies on models of slope steepness using data from the High Resolution Imaging Science Experiment (HiRISE) camera on MRO. The paper includes examinations of 151 RSL features at 10 sites. Another study, published in March, suggested that the RSL were caused by "dry avalanches."
A home for life
The findings do not negate the detection of hydrated salts by MRO, and liquid water may still play a role in the formation and seasonal evolution of RSL streaks, according to the paper. But, similar to a 2016 study, they contend the hypothesis that the water comes from beneath the surface.
The authors propose that the water detected in the RSL is sucked from the thin Martian atmosphere, rather than supplied by underground reserves. The increase in hydration could cause changes in the granular material on these slopes that triggers some of the flow that creates the dark streaks. The dark regions could also be the result of "changes in hydration," according to the statement.
"Full understanding of RSL is likely to depend upon on-site investigation of these features," said MRO Project Scientist Rich Zurek. He noted, however, that if scientists could visit these RSL sites, they would still take precautions to prevent accidental contamination of the sites with Earth-based microbes. In other words, scientists will not completely rule out the possibility that microbes could be living in these RSL just yet.
Zurek added that "a full explanation of how these enigmatic features darken and fade still eludes us. Remote sensing at different times of day could provide important clues."
The study was published Nov. 20 in the journal Nature Geoscience.
Original article on Space.com.
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