MEASUREMENT OF THE NEUTRINO MASS HIERARCHY IN THE DEEP SEA J. Brunner.

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Presentation transcript:

MEASUREMENT OF THE NEUTRINO MASS HIERARCHY IN THE DEEP SEA J. Brunner

Matter effects & Mass Hierarchy Solar Neutrinos : Matter effects inside sun  m 2 > m 1 Matter effects in Earth (not yet measured !)  m 3 >< m 1,m 2 Normal Hierarchy Inverted Hierarchy

Matter effects & Mass Hierarchy e see additional potential due to W-exchange in +e  +e scattering Illustration for constant electron density n e At resonant energy  13 maximal A changes sign with n e via / A changes sign with  m 2  mass hierarchy !

Example Earth Matter Effect : P( µ  e ) cos  = 0.6 Baseline = 7645 km Inclination = 36.9˚ Resonance energy Earth mantle : 6-7 GeV NH IH GLOBES

Example Earth Matter Effect : P( µ  µ ) cos  = 0.6 Baseline = 7645 km Inclination = 36.9˚ Resonance energy Earth mantle : 6-7 GeV NH IH GLOBES

Sensitivity Calculation Fit of event count in Energy-Zenith space Color code : bin-by-bin significance of hierarchy difference W. Winter : arXiv: Oscillation parameter fixedOscillation parameter fitted

ORCA Dense Mton detector with KM3Net design Oscillation Research with Cosmics in the Abyss Less than 20 MEuro with current KM3Net technology

Effective Mass From ORCA simulations (preliminary) Same function used for all CC interaction Same light output for µ and e  ok Conservative for  due to escaping neutrinos NC evaluated at E/2 A. Trovato (LNS)

PINGU – ORCA : Energy Energy reconstruction from total light yield Ice is a better calorimeter due to scattering Energy reconstruction from fitted track length PINGU ORCA ICRC 2013 : Contribution 164 ICRC 2013 : Contribution 555

PINGU – ORCA : Zenith angle Resolution close to kinematical limit Water is a better tracker due to absence of scattering PINGU ORCA ICRC 2013 : Contribution 555 ICRC 2013 : Contribution 164

Sensitivity Calculation A. Heijboer

PINGU : Sensitivity combined

ORCA Sensitivity  Comparable or Better ! Muons only 6 years Cascades Muons No particle ID Cascades better than Muons Combination improves sensitivity by about a factor 2

Huber : Sensitivity over time ArXiv:

A NEUTRINO BEAM TOWARDS ORCA

Why consider Beams ? PINGU / ORCA Motivations Fast : Construction within few years Significant measurement after few years Stay within low budget Neutrino Beams Expensive & long(er) Timescale  counter intuitive Matter effects with Atmospheric Nu’s More challenging than originally hoped for Beam allows for complementary measurement Neutrino Beams Easier to motivate if pointing towards an existing detector Maybe possible in “parasitic mode”

Why consider Beams ? Recently : change of paradigm for European LBL program Opens new, so far neglected options

Optimal Baseline ? For L>2000km the oscillation probabilities are always well separated for both MH hypotheses To find optimal baseline calculate event rates N ~ 1/L 2 N ~ E (cross section) Fixed beam profile ORCA detector response NH IH

Optimal Baseline L=2600km maximizes the difference in event rates between two MH hypotheses Event rate difference NH - IH

Oscillation Probabilities All relevant oscillation probabilities taken into account Full 3-flavour treatment CP-phase variations included

Optimal Energy Range ? Cross section weighted sum of oscillation probabilities Allows to find optimal energy range for MH determination No flavour tagging or CC/NC separation used Kinematical suppression of  exploited NH / IHRatio of Integrals IH/NH (2.5 GeV - E max )

Optimal Energy Range “Event counting”, no flavour ID : 2-6 GeV 11-14% suppression of IH w.r.t. NH Ratio of Integrals IH/NH (2.5 GeV - E max )

Proton Accelerator Complex Protvino Presentation S. Ivanov (IHEP) on CERN  Talk Wednesday

Proton Accelerator Complex Protvino Presentation S. Ivanov (IHEP) on CERN

Protvino – ORCA Baseline 2588km ; beam inclination : 11.7˚ (cos  = 0.2) Deepest point 134km : 3.3 g/cm 3

SKAT bubble chamber Courtesy: R. Nahnhauer p target focus Decay pipe 55m Shielding SKAT 140m 270m 245m

Beam parametrisation (1988) Neutrino Focus Anti-Neutrino Focus Scaling to ANTARES site (0.245/2600) 2 Z. Phys. C 40 (1988) 487

Beam parametrisation (1988) Very clean µ beam Less than 1% contaminations from other flavours Most neutrinos between 2-8 GeV Z. Phys. C 40 (1988) 487

Off-Axis Beam : suppress HE tail Beam optimisation still to be done Off-axis or combination on-axis/off-axis might be favorable

Event rates - Signal Event numbers for p.o.t.s (3 years NOVA beam) 20  statistical separation of both Mass Hierarchy hypotheses from signal muon events for beam normalisation 3.5% separation between MH hypotheses Other contributions:  : /- 13 ; /- 8 ; NC : 4732 µ CC e CC NH /- 255 IH 497 +/- 100 NH /- 24 IH /- 43

Event rates – All Flavours & Mis-ID Event numbers for pots 9-18% difference for NH/IH 7  statistical separation of MH hypotheses Can allow for 3-4 % syst. uncertainty No requirement of energy reconstruction trackscascades NH /- 200 IH /- 80 NH /- 45 IH /- 15

Flavour identification & Neutrino Energy Need to separate “tracks” from “cascades” Villars : C2GT project (F. Dydak) CERN to Gulf of Taranto

Flavour identification Villars : C2GT project (F. Dydak) Clean separation of µ CC and e CC at 0.8 GeV OM spacing 3m

Dense detector 3x3 with cone display Electron-Neutrino Event, C-Cone clearly visible E = 5 GeV ; E e = 4 GeV 50nsec 100 nsec

Synergies between potential Sites Modane 2393km Antares 2588km Gran Sasso 2189km Nemo 2574km Protvino 4.1˚ 11.0˚ 13.6˚

Conclusion Preliminary Performance Figures of ORCA encouraging Mass hierarchy measurement in the deep sea possible Upgraded proton accelerator at Protvino well suited for LBL towards Mediterranean Sea Needed : p.o.t. within few years Perfect subject for Russian Mega-Science program Synergy with Underground Labs in the same beam Complementary to measurement with atmospheric Complementary between ORCA / PINGU  High Significance determination of Mass Hierarchy

Possible Timescale : Finalize optimization work for both options Currently active groups : CPPM, APC, ECAP (Erlangen)  Publish comprehensive document ~2016 : Planning “Phase II” of KM3Net Parallel : Contact with Russian partners, LoI ? First encouraging contact 08/2013 (Y. Kudenko, INR) Start contact with Modane project(s) (ex LBNO) First discussion 08/2013

Backup

Neutrinos from Beams Eliminate ambiguities Improve mass hierarchy sensitivity arXiv: Narrow band beam 6-9 GeV p.o.t.

P( µ  µ ) cos  = 0.1 Baseline = 1274 km Inclination = 5.7˚ GLOBES NH IH

P( µ  µ ) cos  = 0.2 Baseline = 2548 km Inclination = 11.5˚ GLOBES NH IH

P( µ  µ ) cos  = 0.3 Baseline = 3823 km Inclination = 17.4˚ GLOBES NH IH

P( µ  µ ) cos  = 0.4 Baseline = 5097 km Inclination = 23.6˚ GLOBES NH IH

P( µ  µ ) cos  = 0.5 Baseline = 6371 km Inclination = 30.0˚ GLOBES NH IH

P( µ  µ ) cos  = 0.6 Baseline = 7645 km Inclination = 36.9˚ GLOBES NH IH

P( µ  µ ) cos  = 0.7 Baseline = 8919 km Inclination = 44.4˚ GLOBES NH IH

P( µ  µ ) cos  = 0.8 Baseline = km Inclination = 53.1˚ GLOBES NH IH

P( µ  µ ) cos  = 0.9 Baseline = km Inclination = 64.2˚ GLOBES NH IH Beam to IceCube

P( µ  µ ) cos  = 1.0 Baseline = km Inclination = 90.0˚ GLOBES NH IH

Counting Muons from Beam Neutrinos Optimal Beamline : km Favoured Option: FermiLab – KM3Net site in Mediterranean Sea 1300 versus 950 events for both mass hierarchy hypotheses in Mton underwater detector (ORCA)  Inverse approach : Counting “Electrons” arXiv:

P( µ  e ) cos  = 0.1 Baseline = 1274 km Inclination = 5.7˚ GLOBES (CP-phase varied in steps of 30˚) NH IH

P( µ  e ) cos  = 0.2 Baseline = 2548 km Inclination = 11.5˚ GLOBES NH IH

P( µ  e ) cos  = 0.3 Baseline = 3823 km Inclination = 17.4˚ GLOBES NH IH

P( µ  e ) cos  = 0.4 Baseline = 5097 km Inclination = 23.6˚ GLOBES NH IH

P( µ  e ) cos  = 0.5 Baseline = 6371 km Inclination = 30.0˚ GLOBES NH IH

P( µ  e ) cos  = 0.6 Baseline = 7645 km Inclination = 36.9˚ GLOBES NH IH

P( µ  e ) cos  = 0.7 Baseline = 8919 km Inclination = 44.4˚ GLOBES NH IH

P( µ  e ) cos  = 0.8 Baseline = km Inclination = 53.1˚ GLOBES NH IH

P( µ  e ) cos  = 0.9 Baseline = km Inclination = 64.2˚ GLOBES NH IH Beam to IceCube

P( µ  e ) cos  = 1.0 Baseline = km Inclination = 90.0˚ GLOBES NH IH

Oscillation parameters Taken from Global Fit (Fogli et al.) for both hierarchy options CP phase left free

Neutrino Cross sections Simple parton scaling assumed (QE, Res. ignored) Flavour universality m  threshold NC approximation

Neutrino Cross sections Simple parton scaling assumed (QE, Res. ignored) Flavour universality m  threshold NC approximation NC, CC: e µ  Solid : neutrino, dashed : antineutrino

Event rates Here : no flavour misidentification CC Rates NC Rates

Event rates Include Background and Flavour tagging Total Background : Total Event Rate :

Flavour identification Misidentification probability : assume same for both directions 50% at 2 GeV  random ; 20% at 5 GeV ; 10% at GeV

V. Ludwig (ECAP)

Systematic Uncertainties Detector Response Water parameters – Extensively studied in ANTARES Neutrino flux – Can be monitored with muon events Neutrino Cross Section – Ongoing and planned short baseline Experiments Oscillation parameters – ORCA with atmospheric neutrinos