New findings from NASA's Mars Reconnaissance Orbiter (MRO) provide the
strongest evidence yet that liquid water flows intermittently on
present-day Mars.
Using an imaging spectrometer on MRO, researchers detected signatures
of hydrated minerals on slopes where mysterious streaks are seen on the
Red Planet. These darkish streaks appear to ebb and flow over time.
They darken and appear to flow down steep slopes during warm seasons,
and then fade in cooler seasons. They appear in several locations on
Mars when temperatures are above minus 10 degrees Fahrenheit (minus 23
Celsius), and disappear at colder times.
"Our quest on Mars has been to 'follow the water,' in our search for
life in the universe, and now we have convincing science that validates
what we've long suspected," said John Grunsfeld, astronaut and associate
administrator of NASA's Science Mission Directorate in Washington.
"This is a significant development, as it appears to confirm that water
-- albeit briny -- is flowing today on the surface of Mars."
These downhill flows, known as recurring slope lineae (RSL), often
have been described as possibly related to liquid water. The new
findings of hydrated salts on the slopes point to what that relationship
may be to these dark features. The hydrated salts would lower the
freezing point of a liquid brine, just as salt on roads here on Earth
causes ice and snow to melt more rapidly. Scientists say it's likely a
shallow subsurface flow, with enough water wicking to the surface to
explain the darkening.
"We found the hydrated salts only when the seasonal features were
widest, which suggests that either the dark streaks themselves or a
process that forms them is the source of the hydration. In either case,
the detection of hydrated salts on these slopes means that water plays a
vital role in the formation of these streaks," said Lujendra Ojha of
the Georgia Institute of Technology (Georgia Tech) in Atlanta, lead
author of a report on these findings published Sept. 28 by Nature
Geoscience.
Animation of Seasonal Flows in Hale Crater, Mars
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Ojha first noticed these puzzling features as a University of Arizona
undergraduate student in 2010, using images from the MRO's High
Resolution Imaging Science Experiment (HiRISE). HiRISE observations now
have documented RSL at dozens of sites on Mars. The new study pairs
HiRISE observations with mineral mapping by MRO's Compact Reconnaissance
Imaging Spectrometer for Mars (CRISM).
The spectrometer observations show signatures of hydrated salts at
multiple RSL locations, but only when the dark features were relatively
wide. When the researchers looked at the same locations and RSL weren't
as extensive, they detected no hydrated salt.
Ojha and his co-authors interpret the spectral signatures as caused
by hydrated minerals called perchlorates. The hydrated salts most
consistent with the chemical signatures are likely a mixture of
magnesium perchlorate, magnesium chlorate and sodium perchlorate. Some
perchlorates have been shown to keep liquids from freezing even when
conditions are as cold as minus 94 degrees Fahrenheit (minus 70
Celsius). On Earth, naturally produced perchlorates are concentrated in
deserts, and some types of perchlorates can be used as rocket
propellant.
Perchlorates have previously been seen on Mars. NASA's Phoenix lander
and Curiosity rover both found them in the planet's soil, and some
scientists believe that the Viking missions in the 1970s measured
signatures of these salts. However, this study of RSL detected
perchlorates, now in hydrated form, in different areas than those
explored by the landers. This also is the first time perchlorates have
been identified from orbit.
MRO has been examining Mars since 2006 with its six science instruments.
"The ability of MRO to observe for multiple Mars years with a payload able to see the fine detail of these features has enabled findings such as these: first identifying the puzzling seasonal streaks and now making a big step towards explaining what they are," said Rich Zurek, MRO project scientist at NASA's Jet Propulsion Laboratory in Pasadena, California.
For Ojha, the new findings are more proof that the mysterious lines
he first saw darkening Martian slopes five years ago are, indeed,
present-day water.
"When most people talk about water on Mars, they're usually talking
about ancient water or frozen water," he said. "Now we know there's more
to the story. This is the first spectral detection that unambiguously
supports our liquid water-formation hypotheses for RSL."
The discovery is the latest of many breakthroughs by NASA's Mars missions.
"It took multiple spacecraft over several years to solve this
mystery, and now we know there is liquid water on the surface of this
cold, desert planet," said Michael Meyer, lead scientist for NASA's Mars
Exploration Program at the agency's headquarters in Washington. "It
seems that the more we study Mars, the more we learn how life could be
supported and where there are resources to support life in the future."
There are eight co-authors of the Nature Geoscience paper, including
Mary Beth Wilhelm at NASA's Ames Research Center in Moffett Field,
California and Georgia Tech; CRISM Principal Investigator Scott Murchie
of the Johns Hopkins University Applied Physics Laboratory in Laurel,
Maryland; and HiRISE Principal Investigator Alfred McEwen of the
University of Arizona Lunar and Planetary Laboratory in Tucson, Arizona.
Others are at Georgia Tech, the Southwest Research Institute in
Boulder, Colorado, and Laboratoire de Planétologie et Géodynamique in
Nantes, France.
The agency's Jet Propulsion Laboratory in Pasadena, California, a
division of the California Institute of Technology, manages the Mars
Reconnaissance Orbiter Project for NASA's Science Mission Directorate,
Washington. Lockheed Martin built the orbiter and collaborates with JPL
to operate it.
More information about NASA's journey to Mars is available online at:
https://www.nasa.gov/topics/journeytomars
For more information about the Mars Reconnaissance Orbiter, visit:
http://mars.nasa.gov/mro
Guy Webster / DC Agle
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6278 / 818-393-9011
guy.w.webster@jpl.nasa.gov. / agle@jpl.nasa.gov
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6278 / 818-393-9011
guy.w.webster@jpl.nasa.gov. / agle@jpl.nasa.gov
Dwayne Brown / Laurie Cantillo
NASA Headquarters, Washington
202-358-1726 / 202-358-1077
dwayne.c.brown@nasa.gov / laura.l.cantillo@nasa.gov
NASA Headquarters, Washington
202-358-1726 / 202-358-1077
dwayne.c.brown@nasa.gov / laura.l.cantillo@nasa.gov
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