In June, 1998 the Super-Kamiokande collaboration announced the
observation of a significant, angle dependent deficit of upward-going
muon neutrinos relative to downward going ones. Since neutrinos are
produced isotropically in the Earth's atmosphere, this deficit has
been interpreted as a manifestation of a process known as "neutrino
oscillations". In this phenomenon, the observed electron, muon or tau
neutrino is thought to be composed of a mixture of definite mass
neutrino eigen-states. Since the masses of these eigen-states are
different, the mixture changes character as the neutrinos travel from
their point of production. As a consequence, a muon neutrino, for
example, can change into an electron or tau neutrino as a function of
distance and experimentally, the number of observed muon neutrinos
could change with distance from the production point in the
atmosphere.
Since this phenomenon can only occur if the neutrino has a mass, the experimental observation is the first definitive demonstration of neutrino mass. The theoretical implications are still being worked out and more experimental information is necessary before we can fully understand what is happening, but it is safe to say that these results have opened a new chapter in the understanding of one of the fundamental constituents of matter.
The UC Irvine team is composed of experiment co-spokesperson Hank
Sobel and research physicists Dave Casper, Wojtek Gajewski, Danuta
Kielczewska, Bill Kropp, LeRoy Price, and Mark Vagins; post-doctoral
fellows Michael Smy and Shin'uchi Mine and graduate student Tomasz
Barszczak.
In 1999 the UCI group is starting a long baseline neutrino oscillation experiment pointing a neutrino beam from the KEK accelerator in the direction of the SuperK detector which is 250 km away. This experiment "K2K" is intended as a check of the atmospheric neutrino results.