
The small asteroid Itokawa is just a loosely packed pile of rubble that collected after a collision between asteroids, according to a slew of new studies based on data from Japanâs Hayabusa spacecraft. The asteroid appears to be plagued by recurring impacts and tremors today, making its continued survival a mystery.
Hayabusa made two attempts to collect samples from the 535-metre-long space rock in November 2005. The attempts appear to have failed, but that will not be clear unless the spacecraft can be returned to Earth, which scientists are hoping to do in 2010. But during its approach, the spacecraft did take images and other data on Itokawaâs topology, composition and gravity field.
What they found was completely unexpected. âFive years ago, we thought that we would see a big chunk of monolithic rock, that something so small doesnât have the ability to hold onto any pieces,â says Erik Asphaug, a planetary scientist at the University of California in Santa Cruz, US, who is not involved with the mission. âEverything we suspected about it turned out to be wrong.â
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The spacecraft showed a surface littered with boulders and gravel, suggesting it was made of the debris from a larger asteroid that was shattered in a past collision. The latest observations from Hayabusa put an approximate size limit on that parent body.
Hot heart
Onboard gamma-ray and infrared spectrometers reveal the asteroid is composed of the âraw materialsâ of planets, such as olivine, pyroxene and metallic iron, says Asphaug. But these materials do not appear to have melted and separated, as would be expected if the parent body was larger than about 200 kilometres across, he says.
Nonetheless, Hayabusaâs cameras reveal that some large boulders appear layered, âlike youâd broken off a rock from the side of a river bed,â he says. That suggests Itokawaâs parent body was large enough to heat up at its centre and develop some internal structure, even if it wasnât large enough to melt. âThere could have been hydrothermal processes conducting water around, similar to on Earth, where steam passes through rocks and alters their compositions,â he told New ĐÓ°ÉÔ´´.
Measurements of the asteroidâs gravity field also suggest it coalesced from the debris of a previous collision. Hayabusa scientists used the data â combined with measurements of the space rockâs size â to estimate its density. It appears to be 40% porous, or filled with empty space.
âThat is astonishing,â says Asphaug, adding that a handful of sand has a porosity of 20%. âItâs very hard to get porosities greater than that. Youâve got to start balancing things delicately, like you were building a house of cards,â he says. âThe only way to do it is to gently pack the stuff together.â
Tamping down
But that raises another mystery, he says, since repeated impacts with other space rocks over millions of years should have made Itokawa denser. âEvery time you have an impact, youâre going to tamp it down,â he says.
And Itokawa certainly appears to have had its share of cosmic run-ins, even though it does not show many craters. New craters are thought to be buried by gravel that flows into them when Itokawa shudders after being struck by a space rock. This shaking is also thought to have buried the powdery dust created in such impacts, leaving only larger boulders and gravel-sized rocks visible.
Only one other asteroid has been studied so extensively, a 33-kilometre-long rock called Eros. Rather than being a pile of rubble that reassembled after an impact, that asteroid appears to be a single rock that was shattered, with its pieces kept in place. Asphaug argues that more asteroids should be visited by spacecraft, in part to determine how to nudge one out of the way if it threatened to collide with Earth.
Itokawa does cross the Earthâs orbit during its 1.5-year-long path around the Sun, but calculations show it will probably never hit the planet. But Asphaug says an asteroid the size of Itokawa is expected to strike the Earth once every 50,000 years, making robotic â or even human â missions to asteroids of compelling interest. âYou want to be ahead of the gameâ in the event that an asteroid is found on an impact course, he says.
Journal reference: Science (vol 312, p 1328 to 1353)