CALL it the anti-Large Hadron Collider. Instead of smashing small particles together at high speeds, researchers have collided giant granite spheres at low ones.
The idea was to look into the formation of planets and asteroids, which coalesced from collisions between bits of rock in the early solar system. Previous studies showed that marble-sized stones bounce off each other like billiard balls.
In the case of boulders, however, it was assumed they would slow after impact to 50 per cent of their initial speed, as some of the collision energy would be absorbed, resulting in changes such as cracks.
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Now, Daniel Durda of the Southwest Research Institute in Boulder, Colorado, and colleagues have tested this idea. They dangled two 1-metre-wide granite spheres from cranes and knocked them together 108 times at up to 1.5 metres per second.
鈥淭here were some pretty good bowling ball cracking noises going on,鈥� Durda says. 鈥淚t was rather impressive to hear.鈥�
They found that the spheres bounced apart at an average of 83 per cent of their initial speed, similar to marbles (). Repeating the test with more porous and irregularly shaped rocks may better resemble the real coalescing process, says Durda.
