Super-Kamiokande atmospheric neutrino results
Toshiyuki Toshito, the Super-Kamiokande collaboration
TL;DR
Using 79 kt·yr of Super-Kamiokande atmospheric data, the analysis finds the μ-neutrino deficit is best explained by $ν_μ\rightarrowν_τ$ oscillations with $Δm^2 \approx 2.5\times10^{-3}$ eV$^2$ and maximal mixing ($\sin^22\theta \approx 1$). The data disfavors pure $ν_μ\rightarrowν_s$ oscillations at 99% C.L., with complementary samples constraining sterile admixtures via matter effects and NC/enriched channels. A search for charged-current $ν_τ$ appearance yields results consistent with $ν_τ$ appearance at ~2$\sigma$, in line with oscillation predictions. Collectively, the results affirm $ν_μ\rightarrowν_τ$ as the primary atmospheric-neutrino oscillation process and place stringent limits on sterile-neutrino scenarios.
Abstract
We present atmospheric neutrino results from a 79 kiloton year (1289 days) exposure of the Super-Kamiokande detector. Our data are well explained by $ν_μ \to ν_τ$ 2-flavor oscillations. We have been attempting to discriminate between the possible oscillating partners of the muon neutrino as being either the tau neutrino or the sterile neutrino. Pure $ν_μ\toν_s$ oscillation is disfavored at 99% C.L.. Moreover, we performed the appearance search for charged current tau neutrino interactions in the upward-going samples. Our data is consistent with $ν_τ$ appearance at roughly the two-sigma level.
