W boson spotted in Antarctica

Icecube observatory spots elementary particle needle in a galactic haystack.

On 6 December 2016, a high-energy particle hurtled from outer space and through an Antarctic ice sheet, where it slammed into an electron at nearly the speed of light. The enormously energetic collision created a completely different particle, which rapidly decayed into a cascade of others.

This event might have gone unnoticed, if a massive matrix of neutrino-detectors hadn’t been sunk into the ice, ready to capture such astrophysical phenomena.

In a paper published in Nature, high-energy astrophysicists at the Icecube Observatory in Antarctica confirm that this 2016 collision provides observational evidence for a theory put forth in 1960, solidifying our understanding of the Standard Model of particle physics.

Called a Glashow resonance event, the phenomenon was first described by physicist Sheldon Glashow. He predicted that if an antineutrino with just the right amount of energy collided with an electron, it would create a thenundiscovered particle through a process called resonance.

This mysterious particle – the W boson – is an elementary particle with an electric charge. Along with the Z boson, it mediates the weak force, which is one of the four fundamental forces that govern how matter behaves.

When it was discovered 23 years later by CERN’S Large Hadron Collider via a different particle interaction, physicists realised that the W boson was much heavier than expected. This amended Glashow’s prediction: for a W-boson to be created via an antineutrino-electron interaction, the antineutrino would need to have an astonishing energy of 6.3 petaelectronvolts (PEV). This is 1000 times more energy than the Large Hadron Collider can produce – and that’s currently the most powerful particle accelerator in the world.

Since physicists couldn’t simulate a Glashow collision in the lab, they instead had to wait for a cosmic coincidence. Supermassive black holes and other extremely energetic astrophysical processes can act like natural particle accelerators, but not only do they have to accelerate an antineutrino to the right energy, and not only must it be sent on the right trajectory to collide with the Earth, it needs to hit in the square kilometre of Antarctic ice where the Icecube Observatory’s detectors are watching.

Needless to say, scientists have been waiting a while.

The Icecube Observatory was operational in 2011; this 2016 hit is its first W-boson. The results of the collision analysis show that it was one of the highest-energy events ever detected by the Icecube observatory; only two other events have had an energy greater than 5 PEV.

Glashow, now an emeritus professor at Boston University, is looking to the future. “To be absolutely sure, we should see another such event at the very same energy as the one that was seen. So far there’s one, and someday there will be more.”

It was one of the highest-energy events ever detected by the Icecube observatory; only two other events have had an energy greater than 5 PEV.

On a plateau near the South Pole, Icecube searches for elusive, nearly massless particles called neutrinos. But it isn’t your average telescope – the real work is done beneath the surface. Over 80 strings of detectors are sunk into the ice, creating a cubic-kilometre array of “eyes on the sky”.