Neutrino astronomy Measuring the Sun’s Core

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Presentation transcript:

Neutrino astronomy Measuring the Sun’s Core TeVPA – Columbus, Ohio, USA – 7th August 2017 Neutrino astronomy Measuring the Sun’s Core Based on J.H.Davis, Phys.Rev.Lett. 117 (2016) 211101  Jonathan davis (king’s college london) Jonathan.h.m.davis@gmail.com

Neutrino astronomy In order to do astronomy with neutrinos we need to be able to work out where they are coming from in the sky. Interested in two cases: supernova neutrinos and solar neutrinos. If a supernova goes off in our galaxy and we detect its neutrinos, can we work out where in the galaxy it happened? Can we use neutrino directionality to probe the sun’s core?

Detection of neutrinos I will focus on water Cherenkov detectors such as Super Kamiokande (SK). Very large detectors such as SK mean that it is possible to obtain large statistics even though neutrinos interact weakly. They are good for solar and supernova neutrinos and they have directional sensitivity for incoming neutrinos.

Detection of solar neutrinos An MeV-energy neutrino scatters elastically off an electron. The electron emits Cherenkov light, which is observed by photomultiplier tubes. Emits Cherenkov Light In H2O

Detection of neutrinos The elastic scattering cross section is strongly forward- peaked for MeV-scale neutrinos, especially for higher recoil energies. Hence the electron after scattering will point back towards the original direction of the neutrino. Ando and Sato, arXiv:hep-ph/0110187v4

The angular resolution of neutrino detectors Unfortunately the actual resolution is much worse, since the electron scatters in the water multiple times. Hence the observed electron direction is only weakly correlated with the incident neutrino direction. This multiple scattering contributes almost all of the angular resolution, and is well- understood due to calibration data. See e.g. Calibration of Super-Kamiokande using an electron LINAC, Nuclear Instruments and Methods in Physics Research A 421 (1999) 113-129. R. Tomas et al. , Phys.Rev. D68 (2003) 093013

Case study: supernova pointing with neutrinos Since the multiple-scattering of the electron is well-known, we can reconstruct the supernova direction. Obtain a simple approximate formula for the angular resolution for SN pointing: R. Tomas et al. , Phys.Rev. D68 (2003) 093013 S. Ando and K. Sato, Prog.Theor.Phys. 107 (2002) 957 J. Beacom and P. Vogel, Phys.Rev. D60 (1999) 033007

Solar neutrinos Solar neutrinos are produced via fusion reactions occurring in the Sun’s core. The solar core has a radius of 20% to 25% of the solar radius. Their energies and fluxes depend on the fusion reactions in which they are created.

Where are 8B neutrinos produced in the core? Different fusion reactions should occur at different positions within the core. We focus on 8B neutrinos, which are predicted to be produced in a spherical region located at 5% of the solar radius from the core centre. Lopes and Turck-Chièze, Astrophys.J. 765 (2013) 14

Maximum likelihood analysis – generating signal distributions We need to generate the distribution of electrons in a water Cherenkov detector, given an assumption on the neutrino distribution in the solar core. Start by generating initial angles of the neutrinos as they arrive at Earth, given a distribution in the core: Sun Neutrino Earth 8B production region

Maximum likelihood analysis – generating signal distributions Combine the initial distribution of neutrinos, the differential cross section of electron-nu scattering and the distribution of electron multi-scattering in the detector. Repeat this process for different initial neutrino distributions within the solar core. Initial angles Path scattering of electrons + + Cross section Spectrum

Maximum likelihood analysis – generating signal distributions Poisson uncertainty is roughly Sqrt(31000) = 176. Difference between profiles is about 200 events per bin. The spectra are only just distinguishable above statistical noise. 2000 kton years exposure

Maximum likelihood analysis - results 95% confidence contours 20 years for Super Kamiokande 4 years for a 500 kilo-tonne experiment J. H. Davis, Phys.Rev.Lett. 117 (2016) 211101

Conclusion We can use solar neutrino experiments as telescopes of the solar interior. Super Kamiokande has 20 years of data so can already constrain the solar neutrino production region to be within the solar core. A 500 kton experiment, perhaps Hyper Kamiokande, could do much better, but it would need to keep background levels as small or smaller than for Super Kamiokande. Jonathan.h.m.davis@gmail.com Jonathan.davis@kcl.ac.uk