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A mission to Mercury

Jonathan Amos ,Dec 4, 2012 New York Times Syndicate

SPACE

Any spacecraft that plans to visit the innermost planet, Mercury, gets double the trouble.

On one side, it’s baked by the sun, receiving some 14,000 watts per square meter, about ten times what a spacecraft in orbit around Earth would receive.

But the spacecraft is also baked on the other side because the planet itself is a “hot potato,” where surface temperatures can reach 470 celsius. It’s a hellish nightmare and designing a probe that could handle this extreme environment very nearly flummoxed Europe’s best engineers.

The Bepi Colombo mission’s difficulty in arriving at technical solutions to meet the thermal challenge greatly increased costs and brought the venture perilously close to cancellation. Bepi is now progressing well through its construction phase – albeit way behind on the original schedule – and should be ready for launch in 2015.

The European Space Agency mission is a joint venture with Jaxa, the Japanese national space agency.

Europe is providing a Mercury Planetary Orbiter which will carry 11 scientific instruments. It will fly in a polar orbit around the planet, imaging the surface, generating height profiles, and collecting data on surface composition and the wispy “atmosphere.”

Japan’s contribution is the Mercury Magnetospheric Orbiter. This will have five instruments and will investigate the planet’s magnetic field.


Mercury is the only terrestrial planet apart from earth to have global magnetic field. The UK has a prominent role in the mission. Its engineers have been responsible for the construction of the Mercury Planetary Orbiter’s structure and propulsion system. British brains have also done the complex mission analysis to work out how to fly into the deep gravity well of the inner solar system.

Bepi Colombo will have to swing by earth once, Venus twice and Mercury four times to get itself into the right position to map the planet. The Mercury Planetary Orbiter has an unusual shape for a planetary probe but, again, that’s a consequence of where it needs to operate. The long edge along the bottom will be the location for a big radiator that will be kept pointed away from the sun at all times.

“We have lots and lots of heat pipes on board,” explained Astrium spacecraft systems engineer Jess Marshall. “These have a small amount of ammonia in them. This evaporates, whizzes up the tubes and then condenses at the radiator.

Everything about this spacecraft is about staying cool.” Bepi is unusual in that, for it will look white. Our spacecraft normally have a gold-coloured, multilayered insulation. Bepi’s insulation will have to be much more robust – it will be a lot thicker and a lot heavier. The white outer covering will reflect a lot of heat away, but we must be very careful also that there are no holes anywhere – no gaps – or that heat will creep in.

Springing surprises


“Many people’s reaction to Mercury is that it is a bit of a dullard. Unlike Mars with its many earth-like vistas, the inner world appears very one-dimensional. The US Messenger probe now in orbit has gone a long way, I think, to countering that viewpoint. It has thrown up many surprises and challenged our assumptions about what the closest planet to the sun should be like. Messenger has revealed Mercury’s rich volcanic history.

It has confirmed the existence of great lava plains, but also uncovered evidence for explosive volcanism. The probe has identified lots of sulphur (two to four per cent) in the surface. That wasn’t expected.

Indeed, there are many more volatile substances in Mercury’s surface than one would expect. They simply shouldn’t be there in a planet that orbits so close to the sun, or one that, according to the popular idea, was involved in a mighty collision that ripped away its uppermost layers.

And then there are these dramatic hollows that have been discovered. This strange pockmarked terrain is evidence of the release of volatile material evaporating away into space. “We’re not quite sure yet what that material is yet,” said Dave Rothery.

The Open University researcher is chief scientist on Bepi Colombo’s Mercury Imaging X-ray Spectrometer. With Bepi, we’ll have sufficiently high spatial resolution with the X-ray telescope to see what the elemental distribution is within these quite small hollowed areas. “Messenger can’t do that – it has a much cruder, coarser resolution.

So, we’ll learn a lot more when we get a more sophisticated spacecraft there, but we already know it’s an absolutely fascinating planet which is not doing what it ought to do.

“That’s the joy of planetary exploration – you work out what you should expect to see to test your hypotheses and then you go there and find, ‘Crikey, this wasn’t what we expected at all’. “We’ve got to have a big rethink and until we understand how Mercury formed, we won’t understand how our own planet formed.”

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