Abstract

We derive predictions for the Nadir angle ( θ n ) dependence of the ratio N μ − / N μ + of the rates of the μ − and μ + multi-GeV events, and for the μ − – μ + event rate asymmetry, A μ − μ + = [ N ( μ − ) − N ( μ + ) ] / [ N ( μ − ) + N ( μ + ) ] , in iron-magnetized calorimeter detectors (MINOS, INO, etc.) in the case of 3-neutrino oscillations of the atmospheric ν μ and ν ¯ μ , driven by one neutrino mass squared difference, | Δ m 31 2 | ∼ ( 2.0 – 3.0 ) × 10 −3 eV 2 ≫ Δ m 21 2 . The asymmetry A μ − μ + (the ratio N μ − / N μ + ) is shown to be particularly sensitive to the Earth matter effects in the atmospheric neutrino oscillations, and thus to the values of sin 2 θ 13 and sin 2 θ 23 , θ 13 and θ 23 being the neutrino mixing angle limited by the CHOOZ and Palo Verde experiments and that responsible for the dominant atmospheric ν μ → ν τ ( ν ¯ μ → ν ¯ τ ) oscillations. It is also very sensitive to the type of neutrino mass spectrum which can be with normal ( Δ m 31 2 > 0 ) or with inverted ( Δ m 31 2 < 0 ) hierarchy. We find that for sin 2 θ 23 ≳ 0.50 , sin 2 2 θ 13 ≳ 0.06 and | Δ m 31 2 | = ( 2 – 3 ) × 10 −3 eV 2 , the Earth matter effects produce a relative difference between the integrated asymmetries A ¯ μ − μ + and A ¯ μ − μ + 2 ν in the mantle ( cos θ n = 0.30 – 0.84 ) and core ( cos θ n = 0.84 – 1.0 ) bins, which is bigger in absolute value than approximately ∼15%, can reach the values of ( 30 – 35 ) % , and thus can be sufficiently large to be observable. The sign of the indicated asymmetry difference is anticorrelated with the sign of Δ m 31 2 . An observation of the Earth matter effects in the Nadir angle distribution of the asymmetry A μ − μ + (ratio N μ − / N μ + ) would clearly indicate that sin 2 2 θ 13 ≳ 0.06 and sin 2 θ 23 ≳ 0.50 , and would lead to the determination of the sign of Δ m 31 2 .

Highlights

  • There has been a remarkable progress in the studies of neutrino oscillations in the last several years

  • We find that for sin2 θ23 >∼ 0.50, sin2 2θ13 >∼ 0.06 and |∆m231| = (2− 3)× 10−3 eV2, the Earth matter effects produce a relative difference between the integrated asymmetries Aμ−μ+ and A2μν−μ+ in the mantle and core bins, which is bigger in absolute value than approximately ∼ 15%, can reach the values of (30 − 35)%, and can be sufficiently large to be observable

  • In the present article we study possibilities to obtain information on the value of sin2 θ13 and on the sign of ∆m231 using the data on atmospheric neutrinos, which can be obtained in experiments with detectors able to measure the charge of the muon produced in the charged current (CC) reaction by atmospheric νμ or νμ

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Summary

Introduction

There has been a remarkable progress in the studies of neutrino oscillations in the last several years. In the present article we study possibilities to obtain information on the value of sin θ13 and on the sign of ∆m231 using the data on atmospheric neutrinos, which can be obtained in experiments with detectors able to measure the charge of the muon produced in the charged current (CC) reaction by atmospheric νμ or νμ. The matter effects in the Nadir angle distribution of the ratio of the multi-GeV μ−like and e−like events, Nμ/Ne, which can be measured in the Super-Kamiokande or other waterCerenkov detectors, are smaller than the matter effects in the Nadir angle distribution of the ratio of the multi-GeV μ− and μ+ events, N (μ−)/N (μ+), which can be measured in MINOS, INO, or any other atmospheric neutrino experiment with sufficiently good muon charge identification. Such a “dilution” of the magnitude of the matter effects does not take place in the samples of the multi-GeV μ− and μ+ events, which can be collected in MINOS and INO experiments, i.e., in the experiments with muon charge identification

Subdominant 3-ν Oscillations of Multi-GeV Atmospheric Neutrinos in the Earth
Enhancing Mechanisms
Results
Conclusions
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