Abstract

The T2K off-axis near detector, ND280, is used to make the first differential cross section measurements of muon neutrino charged current single positive pion production on a water target at energies ${\sim}0.8$ GeV. The differential measurements are presented as a function of muon and pion kinematics, in the restricted phase-space defined by $p_{\pi^+}>200$MeV/c, $p_{\mu^-}>200$MeV/c, $\cos \theta_{\pi^+}>0.3$ and $\cos \theta_{\mu^-}>0.3$. The total flux integrated $\nu_\mu$ charged current single positive pion production cross section on water in the restricted phase-space is measured to be $\langle\sigma\rangle_\phi=4.25\pm0.48 (\mathrm{stat})\pm1.56 (\mathrm{syst})\times10^{-40} \mathrm{cm}^{2}/\mathrm{nucleon}$. The total cross section is consistent with the NEUT prediction ($5.03\times10^{-40} \mathrm{cm}^{2}/\mathrm{nucleon}$) and 2$\sigma$ lower than the GENIE prediction ($7.68\times10^{-40} \mathrm{cm}^{2}/\mathrm{nucleon}$). The differential cross sections are in good agreement with the NEUT generator. The GENIE simulation reproduces well the shapes of the distributions, but over-estimates the overall cross section normalization.

Highlights

  • The T2K long baseline neutrino experiment [1] has the primary goal to precisely measure neutrino oscillation parameters through measurements of νe appearance and νμ disappearance from a νμ beam

  • As neutrinos are chargeless and colorless, neutrino oscillation experiments rely on the detection of charged particles coming from charged current (CC) and neutral current (NC) interactions to infer neutrino properties, e.g. CC quasielastic (QE) interactions allow the calculation of the neutrino energy from the lepton kinematics

  • We present the first CC1πþ differential cross section measurements on water

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Summary

INTRODUCTION

The T2K long baseline neutrino experiment [1] has the primary goal to precisely measure neutrino oscillation parameters through measurements of νe appearance and νμ disappearance from a νμ beam. Νμ CC resonant interactions are part of the signal and sometimes of the background of oscillation experiments, and a better understanding of this channel could be beneficial to T2K, but to the neutrino community in general, as there are discrepancies between models and experimental data Both the MiniBooNE [2] and MINERvA [3] collaborations provided measurements of the CC single positive pion. A CC1πþ measurement on water will have a strong impact on the T2K oscillation analysis, as current results suffer from large cross section systematic uncertainties related to the differences in targets between near and far detectors (carbon versus water) [8] These data will be beneficial to future atmospheric and long-baseline experiments, which plan to use a water target, such as the Hyper-Kamiokande experiment [9]

T2K EXPERIMENT
Neutrino beam flux
Neutrino interaction model
Near detector
Systematic uncertainties
UNFOLDING METHOD
CROSS-SECTION RESULTS
Findings
CONCLUSION
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