Measuring Oscillations with a Million Atmospheric Neutrinos
Illustrated tale of a hard and beautiful project
C.A. Argüelles, Pablo F., I. Martínez-Soler, Miaochen Jin 2022/11/23– XIV CPAN days
[arXiv:2211.02666]
Introduction
● Sensitivity achievable by the current and near-
future water(ice)-Cherenkov atmospheric neutrino experiments in the context of standard three-flavor neutrinos oscillations
● Perform an in-depth analysis of the current shared systematic uncertainties arising from the common flux and neutrino-water interactions
● Develop the atmospheric neutrino simulations for Super-Kamiokande (SK), with and without
neutron-tagging capabilities (SuperK-Gd), IceCube-Upgrade, and ORCA experiments
● Implement the systematic uncertainties of each experiment
Neutrino (3f) Oscillations
Atm. neutrinos are good discovery experiments, they cover ten orders of magnitude in the ratio of baseline to energy, L/Eν
This broad range of L/Eν and the fact that atmospheric neutrinos go through the largest amounts of matter allow them to measure neutrino osc. parameters In the 3ν scenario, neutrino evolution is described by six parameters: two
mass-squared differences, three mixing angles, and a complex phase parameterizing the violation of the CP-symmetry
This analysis focuses on the study of θ23, Δm312 (including the MO) θ13 and δCP
Pνl→νl'
(
LE)
≈∑
i , j UPMNSl ' i (UPMNSli )(Ul ' jPMNS)UPMNSlj e−iΔ2mEij2LNeutrino (3f) Oscillations
The ordering and θ13
Ordering flips the MSW resonance between neutrinos (NO) and antineutrinos (IO) Position and intensity depends on θ13
Neutrino (3f) Oscillations
● CP-violation results in a different normalization of the probability and a shift in the oscillation phase.
Broad in energy and more relevant at sub-GeV
● In the multi-GeV scale, the neutrino oscillation is dominated by ∆m31 and θ23 the oscillation
amplitude is controlled by sin22θ23
2
Atm. neutrino flux
Atmospheric neutrinos are produced by the collision of cosmic rays with Earth’s atmosphere
The primary spectrum of cosmic rays spans from MeV to EeV energies and is composed of free protons ( 80%) and bound nuclei ( 20%)∼ ∼
Their interaction with nuclei in the atmosphere
initiates hadronic showers on average about 20 km above the surface, producing numerous mesons Neutrinos are produced predominantly from the decay of muon, pion, and kaon;
which dominate the muon neutrino flux below 10, 100, and 106 GeV
Cross-sections
All three experiments considered in this work also share the neutrino cross-sections on water
In WC detectors, mainly neutrinos interacting charged current (CC) are reconstructed. Only a small fraction of neutral current (NC) interactions can produce a
detectable signal
The flavor of CC neutrinos can be very efficiently
reconstructed through the corresponding charged-lepton, whereas in NC no flavor information can be extracted.
The wide energy range of atm neutrinos cover many interaction channels:
● Charged current quasi-elastic (CCQE)
● Resonance production (CC RES)
● Deep Inelastic Scattering (CC DIS)
Experiments: IceCube-Upgrade
IceCube is a 1 km3 ice-Cherenkov detector at the South Pole with 5160 optical sensors at depths between 1450 m and 2450 m
DeepCore is a ~10 Mton denser sub-array in the inner part of the detector
IceCube is planning an upgrade that will add strings to have a denser region, lowering the threshold to 1 GeV
There are two event morphologies:
● Tracks: propagation of muons
● Cascades: produced by the propagation of electrons, taus, or hadronic cascades
We use the official IC-Upgrade simulation published by the collaboration
Experiments: IceCube-Upgrade
Experiments: KM3NeT/ORCA
Water-Cherenkov neutrino telescope under construction in the Mediterranean sea,
KM3NeT
● ARCA: TeV-PeV neutrino astronomy
● ORCA will be a ~8 Mton detector with 64170 PMTs, achieving an energy
threshold of ~2 GeV
Already an official projection of its sensitivity to neutrino oscillations
Well advanced analysis with a third event category in addition to tracks and
cascades
Unfortunately, no public MC simulation; we produced our own by re-weighting and
extending the MC from IC-Up to reproduce their results
Experiments: KM3NeT/ORCA
Tracks
Experiments: Super-Kamiokande
Super-Kamiokande is a Japanese 50-kton cylindrical water-Cherenkov detector,
instrumented with ~11,000 20-inch PMTs facing inwards
The large photo-coverage and more
controlled medium enables a (n effective) energy threshold of 0.1 GeV for atm.
neutrinos
Now, being upgraded dissolving Gd to tag neutrons very efficiently (Nataly’s talk)
More than 15 rather complex event categories with no publicly available simulation… things get interestingly hard
Using publicly available information, we produced simulations for SK, SK with neutron tagging on H, and SK with neutron tagging on Gd
Experiments: Super-Kamiokande
δCP senstivity MO senstivity
Experiments: Super-Kamiokande
Results
We conservatively assume the running of SuperK until the last reported
exposure time, the SK-Gd and IceCube- Upgrade data-taking period extending from 2025 until 2030, and ORCA from 2027 to 2030
Assuming latest global fit values:
The “atmospheric” parameters
Resolving the θ23 octant and measure Δm312 with great precision
Results
Sensitivity to θ13 comparable with
LBL experiments Synergies between experiments
most relevant in δCP sensitvity
Results
Measurement of the ordering
before the end of the decade Significant fraction of δCP excluded at 99% CL (largely depends on the actual value)
Results; present and future
Independent, comparable (even better) sensitivities than current LBL experiments (ideal for weighing in tensions)
Very valuable input for next-generation experiments and the precise measurement of the CP-phase
Results; present and future
Current ancillary measurements (both flux and cross-section) for next-generation experiments could significantly reduce relevant systematic uncertainties dragging the sensitivity to the CP-phase
Bonus: Intermediate WC Detector (IWCD)
Of particular (and biased) interest is the IWCD, within the HyperK project
● ~400 ton instrumented with ~500 mPMTs, located ~750 m from J-PARC ν-beam
● Large statistics of muon and electron (anti)neutrinos in the subGeV region
● Crucial for reducing CCQE systematics
Conclusions
First in-depth analysis of the potential of a combined fit with data from current and soon-to-operate WC atm. neutrino experiments
● Strong constraints on the atmospheric mixing parameters
– Resolves the octant of θ23
– Precise measurement of Δm31
– Measurement of the mass ordering above 5σ
– Measurement of θ13 with similar precision as current LBL experiments
– Significant constraints on of δCP independently/complementary to LBL experiments
● Provides a comprehensive picture of the 3-flavor mixing and very valuable input for next-generation neutrino oscillation experiments (DUNE and HyperK)
● Ordering information also crucial for next-generation ββ0ν searches
2
Conclusions
● Provides input for the key improvements in flux and cross-section uncertainties, especially for the sensitivity to δCP
– Will benefit from ongoing task force systematic errors reduction towards next-generation experiments
● Machinery ready for properly including atm. neutrinos in global fits, crucial requirement for complete description of neutrino mixing with current data
● Opens the door to other very interesting analyses… (coming soon)