The ExoMars Entry, Descent, and Landing Demonstator Module. Credit and Copyright ESA.
This week’s Science journal included an article on the challenges
facing the Curiosity rover in its hunt for organic molecules on Mars. (Unfortunately, the article is available by
subscription only.) Complex organic
molecules would be a clue that Mars may have once harbored life or at least the
conditions that allowed for complex pre-biotic chemistry to occur. Three spacecraft, the two Viking landers and
the Phoenix lander, have so far tested Martian soil for organic molecules and
come up with negative results. (Although
some argue that the natures of the failures suggest instrument limitations
rather than the lack of complex organics.) The failure to find organic molecules suggests
that processes on Mars are destroying organic molecules since the surface is
subject to a steady rain of meteorites that contain less complex organic
molecules. Per the article, researchers
have identified three mechanisms that may be destroying organic molecules at
and near the surface of Mars: oxidizers in the soil including the perchlorate
salts found by Phoenix, ultraviolet radiation, and cosmic rays. The article states, “With decomposed
perchlorates, cosmic rays, and ultraviolet radiation ganging up on Martian
organic matter, Curiosity's chances of finding it when it scoops up its first
soil samples are looking slim. And ‘if we find [soil] organics, it almost
certainly will have nothing to do with life,’ says astrobiologist Christopher
McKay of NASA Ames. The most likely organics in soils would be those of cosmic
dust because they are continually resupplied, so detecting organics is not
detecting life,’ he says.”
One of the challenges facing Curiosity’s hunt for organic molecules is
that its drill can sample only 10 centimeters into a rock or into the regolith,
not deep enough to avoid the agents that destroy organic molecules. ESA’s ExoMars rover has been designed to
sample up to two meters beneath the surface, below the reach of surface destroyers
of organic molecules.
ESA has continued to redesign the ExoMars mission with Russia as its
only partner after the U.S. declined to participate. European financing for the total bill remains
a challenge and the final resolution isn’t expected until this Fall.
ESA recently published a newsletter on the current state of the mission definition. The 2016 Orbiter will carry two European
instruments – the NOMAD spectrometer to map trace gases and a high resolution
stereo color camera. Russia will supply
two additional instruments for the orbiter – the Atmospheric Chemistry Suite
that will map the structure of the atmosphere (the ESA publication doesn’t
discuss why a chemistry instrument will map structure, which typically is
measured in terms of temperature and pressure) and a neutron detection
instrument to refine measurements of near surface water ice.
A major goal of the 2016 mission has been to test European technologies
for landing mid-sized payloads such as geophysical stations. (The seven minutes of terror to get a payload
to the surface of Mars exists for any space agency wanting to land on
Mars. Developing and proving a landing
capability enables future lower cost missions, much as the demonstration of the
Phoenix system enabled the recent selection of the InSight mission.) At one time, there was discussion of
including a Russian radioisotope power supply to enable a long-lived
lander. Now the plan has reverted to a
battery powered lander with a short (few days at most) lifetime.
Russia will also supply two new instruments for the 2018 rover mission
– an infrared spectrometer and a neutron spectrometer. (Russia also supplied a neutron spectrometer
for NASA’s Curiosity rover to search for near surface hydrogen deposits that would
indicate the presence of H2O.)
The brief newsletter also talks about a surface science platform in
addition to the ExoMars rover. It’s
unclear what this might be, although a geophysical station might be a
possibility. The supporting web site simply
says, “the two space agencies have
agreed to send a large capsule to Mars with a surface science platform and a
rover carrying both European and Russian instruments. The two science stations
will operate in parallel.” (At
one time, before the first descope to reduce costs, the ExoMars mission
included a sophisticated geophysical station in addition to the rover.)
Russia will have the leading role in delivering the rover and science
station to the surface: “the descent
and surface modules will be developed by Roscosmos in cooperation with ESA.”
Editorial Thoughts: First, I hope that enlightened selection of
sampling locations (with maybe a large helping of luck) will enable the
Curiosity rover to find the organic molecules its instrument suite is designed
to find. A success would enhance chances
for funding a robust future Mars program, while a fourth strike won’t be
helpful.
Given the challenges of finding intact organic molecules – assuming
they exist – I remain a fan of the ExoMars rover mission and hope it secures it
European funding this fall. I am
concerned about the 2018 landing mission becoming too complex – ESA has never
done a rover mission and Russia has never successfully landed a mission on
Mars. Now the mission has become more
complex with a surface science station. NASA
hit a home run with the Curiosity landing and subsequent rover operations, but
that was after a string of six successful, and simpler, landings. ESA’s track record for planetary missions has
been excellent, providing confidence for the ESA 2016 orbiter and 2018
rover. Russia, after the failure of the
Phobus-GRUNT mission last year, reportedly is in the process of reforming its
design processes. Landing a good-sized
rover and surface station on your first try at a Martian landing in over 40
years is an ambitious goal. (A recent article in the Guardian makes the same point, but less diplomatically. Until I hear otherwise, I presume that ESA and RSA are aware of the challenges and taking appropriate steps.)
My fingers are crossed that the budgetary and technical stars align for
ExoMars. The search for signs of pre- or
actual biotic organics on the second most Earth-like planet in the solar system
is important to the future of planetary exploration.
10cm deep hole is not enough. By today's estimate, what is the minimum depth you have to go to find native organics and I'm sure it must vary with materials (rocks, soil et cetera)?
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