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Experimental Status of Geo-reactor Search with KamLAND Detector

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Presentation on theme: "Experimental Status of Geo-reactor Search with KamLAND Detector"— Presentation transcript:

1 Experimental Status of Geo-reactor Search with KamLAND Detector
Jelena Maričić University of Hawaii at Manoa

2 Neutrino Geophysics, Honolulu
Outline KamLAND detector: design and features Motivation for experimental geo-reactor search in KamLAND Geo-reactor analysis anti-neutrino event selection and backgrounds Anti-neutrino flux at KamLAND Analysis Summary and conclusion December, Neutrino Geophysics, Honolulu

3 KamLAND Detector: Design and Features
December, Neutrino Geophysics, Honolulu

4 KamLAND: Purpose and Location
- KamLAND - anti-neutrino detector; built to study anti-neutrino oscillations. - Japan - natural choice for location of anti-neutrino detector : - large number of nuclear plants. - Nuclear plants - the largest man-made νe sources. - Nuclear plant December, Neutrino Geophysics, Honolulu

5 Reactors as Neutrino Sources and KamLAND
Nuclear reactor is an excellent source of electron anti-neutrinos from β decay. Average 3 GWth plant has a flux of 6•1020 anti-neutrinos/s! • KamLAND - disappearance experiment νe νe Look for a deficit of νe at a distance L νe νe nuclear reactor νe νe KamLAND νx ? νe νe νe νe detector L December, Neutrino Geophysics, Honolulu

6 Anti-neutrino Spectrum
Number of observed events (1/MeV) Reactor spectrum Observed spectrum Interaction cross- section (~10-43cm2) E (MeV) December, Neutrino Geophysics, Honolulu

7 Neutrino Geophysics, Honolulu
Detector Scheme 1kton of LS surrounded by buffer oil and acrylic Rn barrier. ” PMTs 554 20” PMTs 34% photocatode coverage 225 20” PMTs - veto water Cherenkov detector • p.e./MeV observed at the center. *KamLAND oil has the best radiopurity ever achieved in the world: U ( ) x g/g Th ( ) x g/g K < 2.7 x g/g December, Neutrino Geophysics, Honolulu

8 Motivation for the Experimental Geo-reactor Search with KamLAND

9 Neutrino Geophysics, Honolulu
Introduction Natural nuclear fission reactor with power up to 10 TW in the center of the Earth was proposed by M. Herndon as the energy source of geo-magnetic field. 4.5 billion years ago, 235U/238U ratio was high enough for the nuclear fission reaction to occur. If such a reactor exists, its anti-neutrino flux would be visible by KamLAND. 235U/238U > 5% Fast breeder nuclear reactor was simulated using the SCALE code package (by D. Hollenback and M. Herndon) and shown feasibility and sustainability for 4.5 billion years. December, Neutrino Geophysics, Honolulu

10 Motivation for Geo-reactor Search
Large error! 90% C.L. Rate from the putative geo-reactor very small! Incoming daily flux varies due to nuclear reactors varying work regime. Small positive offset of 0.03e/day with VERY LARGE ERROR may be present, for 0 ev/day expected! December, Neutrino Geophysics, Honolulu

11 Is the Event Excess for Real and if So, What is the Source ?
The possible surplus of detected events implies that there may be another source of anti-neutrinos that have not been accounted for. Proposed 3-10 TW georeactor if exists would produce anti-neutrino signal of 4-14% of the KamLAND signal. The goal of this analysis is to set the upper limit on the power of the putative geo-reactor. Is it there and if so, how large is it? December, Neutrino Geophysics, Honolulu

12 Geo-reactor Analysis Anti-neutrino Event Selection and Backgrounds
December, Neutrino Geophysics, Honolulu

13 Detection Reaction in KamLAND
Inverse beta decay reaction combined with delayed neutron capture reaction. Distinctive signature in time and space: Prompt event: e+ - e- annihilation – 2 γ rays Delayed event: 2.2 MeV γ ray about 200 μs later. ne + p+ ® e+ + n Ethreshold = MeV Prompt Event γ γ e+ γ νe p n 2.2MeV Eprompt = E MeV 200 μs Delayed Event December, Neutrino Geophysics, Honolulu

14 Neutrino Geophysics, Honolulu
Event Selection Cuts - target volume cut (R < 5.5 m) 4.61 x 1031 target protons, - inverse β decay cut - timing correlation cut (0.5μs < ΔT < 1000μs) - vertex correlation cut (ΔR < 2.0 m) - delayed energy cut (1.8MeV < Edelay < 2.6MeV) ***Efficiency of inverse β decay cut ( )% - prompt energy analysis threshold (2.6 MeV < Eprompt< 8.5 MeV)* - cosmic ray muon spallation event cut (spallation - shattering of a nucleus by a highly energetic cosmic-ray particle) *As a cross-check, analysis with lower energy threshold of 1.6 MeV prompt energy has been performed as well. Data sample increase 40%. However, lower energy threshold requires additional background subtraction. December, Neutrino Geophysics, Honolulu

15 Cosmic Ray Muon Spallation Cuts
Cosmic muon rate in KamLAND is 0.34 Hz. 2 ms veto is applied after each tagged muon 2 sec veto is applied after showering muon 2 sec veto along LS muon track with 3 m radius *** Spallation cuts introduce around 9.7% additional dead time. December, Neutrino Geophysics, Honolulu

16 Anti-neutrino Candidates
From March 9th 2002 to January 11th 2004 total livetime is: 515.1 days After applying selection cuts, the number of selected anti-neutrino candidates is: 258 events (Eprompt>2.6MeV) or 362 events (Eprompt>1.6MeV) December, Neutrino Geophysics, Honolulu

17 Estimated Systematic Uncertainties
The largest contribution Target volume % Energy threshold 2.3% Efficiency of cuts 1.6% Livetime % Reactor power % Fuel composition 1.0% Anti-neutrino spectra 2.5% Anti neutrino cross-section 0.2% Total % December, Neutrino Geophysics, Honolulu

18 Neutrino Geophysics, Honolulu
Analysis Backgrounds E > 3.4 MeV E > 2.4 MeV - Geo-neutrinos coming from the radioactive decay chains of 238U and 232Th negligible (14 + 5) Accidental backgrounds ( ) ( ) 9Li/8He Background ( ) ( ) 13C(,n)16O background ( ) ( ) Total ( ) ( ) December, Neutrino Geophysics, Honolulu

19 Anti-neutrino Flux at KamLAND
December, Neutrino Geophysics, Honolulu

20 Anti-neutrino Flux from Man-made Reactors
- 79% is within range km ave. dist. 180 km - Expected number of events in days of livetime: (syst) (syst.) in the unoscillated case. E > 3.4 MeV E > 2.4 MeV December, Neutrino Geophysics, Honolulu

21 Anti-neutrino Spectrum from Geo-reactor
Reactor spectrum for the deep Earth reactor is assumed to be a typical commercial reactor spectrum. It is assumed that its output is very stable (on the data taking scale) E > 2.4 MeV events/TW·day events/TW·day December, Neutrino Geophysics, Honolulu

22 Neutrino Geophysics, Honolulu
Analysis December, Neutrino Geophysics, Honolulu

23 Detecting a Geo-reactor
Geo-reactor signal - 0 to 14% (10 TW) of the signal at KamLAND. KamLAND can detect signature spectrum from geo-reactor, as a constant νe flux on the top of varying νe flux from terrestrial reactors. - Upper limit on the geo-reactor thermal power set using statistical approach: Maximum Likelihood Method*. *Maximum likelihood estimation (MLE) is a popular statistical method used to make inferences about parameters of the underlying probability distribution of a given data set. December, Neutrino Geophysics, Honolulu

24 Neutrino Geophysics, Honolulu
Analysis Outline The analysis is based on 776 ton-year exposure of KamLAND to neutrinos. Geo-reactor power is treated as a completely free parameter Analysis consists of 2 parts: Rate + Spectrum shape analysis using global solar solution for oscillation parameters (independent of KamLAND) for E > 3.4 MeV. Cross-check analysis with lower energy threshold E > 2.4 MeV December, Neutrino Geophysics, Honolulu

25 Two Different Choices for Global Solar Oscillation Parameters
Two different sets of oscillation parameters used. Effects on the geo-reactor power output results tested. m2 = 6.45 ·10-5 eV2 SNO old 2003 sin2 2 = 0.82 m2 = 6.5 ·10-5 eV2 SNO new 2005 sin2 2 = 0.86 December, Neutrino Geophysics, Honolulu

26 Time dependent survival probability
Survival probability changes daily due to the distance flux variation (reactors being turned off etc.). Also energy spectrum is time dependent. Difference in shape due to the difference in oscillation parameters. December, Neutrino Geophysics, Honolulu

27 Choice of Maximum Likelihood Function
Analysis takes into account both daily rate and spectrum shape information with flux time variation included. Variable parameters in the fit are: Geo-reactor rate (free) Detection efficiency (constrained) 9Li muon spallation background (constrained) 13C(α,n)16O background (constrained) Δ m2 (constrained) sin2 2θ (constrained) } BG }OP *Geoneutrino background from terrestrial uranium is also treated as a fit parameter in the lower energy cross-check analysis. December, Neutrino Geophysics, Honolulu

28 Neutrino Geophysics, Honolulu
Analysis Results Geo-reactor power < 19 TW at 90% C.L. 16 geo-reactor events in the data sample PRELIMINARY December, Neutrino Geophysics, Honolulu

29 Energy Spectrum for the Best Fit Result
Observed spectrum is time integrated, while the best fit is obtained from the time varying maximum likelihood function best fit. PRELIMINARY December, Neutrino Geophysics, Honolulu

30 The Δχ2 Test as a Function of Geo-reactor Power
The best fit with SNO old (2003) choice of mixing parameters PRELIMINARY Very wide minimum December, Neutrino Geophysics, Honolulu

31 Summary and Conclusion
December, Neutrino Geophysics, Honolulu

32 Comparison of the Best Fit Result with Geological Data
PRELIMINARY 31-44 TW 19-31 TW 0-12 TW December, Neutrino Geophysics, Honolulu

33 Neutrino Geophysics, Honolulu
Conclusion Upper limit on the power of the geo-reactor have been set for the first time. The best fit is: Upper limit on geo-reactor power is 19 TW at 90% C.L. Final result greatly influenced by the input oscillation parameters. KamLAND size detector far away from nuclear reactors needed for high confidence (>99.99%) measurement. Hawaii presents an excellent choice for a definite geo-reactor measurement (Hanohano). PRELIMINARY December, Neutrino Geophysics, Honolulu


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