UHECR

How are UHECRs detected?

UHECRs are far too rare to detect directly from space with useful statistics. Instead, we use the Earth’s atmosphere as a giant calorimeter: when a UHECR strikes an air nucleus high in the atmosphere, it initiates an extensive air shower (EAS) — a cascade of billions of secondary particles spread over tens of square kilometres at ground level.

The extensive air shower

The first interaction, typically at an altitude of 15–35 km, produces a spray of hadrons — mostly pions. The cascade then develops three coupled components:

The depth of Xmax and the muon content are the primary observables used to infer the mass composition of the primary particle: proton showers penetrate deeper and fluctuate more than showers initiated by iron nuclei.

Detection techniques