Neutrino Geophysics in Hawaii Presentation by Steve Dye Associate Professor of Physics Hawaii Pacific University January 20, 2005 20 January 2005 Steve Dye, HPU 1 Outline of Presentation Neutrinos Geophysics Neutrino Geophysics HANOHANO 20 January 2005 Steve Dye, HPU 2 Neutrinos Discovery Place in nature Properties Detection – Astrophysics – Nuclear reactors http://www.flyingneutrinos.com 20 January 2005 Steve Dye, HPU 3 Discovery of Neutrino W. Pauli proposes undetected particle in β-decay (1931) E. Fermi develops theory of β-decay with “little neutral one” (1934) C. Cowan and F. Reines detect neutrinos at nuclear reactors (1950's) 20 January 2005 http://www.ps.uci.edu/physics/reinesphotos.html Steve Dye, HPU 4 Neutrino’s Place in Nature http://www.particleadventure.org/particleadventure/frameless/chart.html 20 January 2005 Steve Dye, HPU 5 Neutrino Properties Come in three flavours – e, μ, τ No electric charge Stable Weak interactions Massive (slightly) Flavour oscillations 20 January 2005 Steve Dye, HPU 6 Neutrino Detection http://www.ps.uci.edu/physics/reinesphotos.html http://www-sk.icrr.u-tokyo.ac.jp/doc/sk/photo/normal.html http://www-personal.umich.edu/~jcv/IMBdiverbig.jpg 20 January 2005 Steve Dye, HPU 7 Neutrino Astrophysics Neutrinos are excellent astrophysical probes – Stable, uncharged, weakly-interacting Low energy (eV scale) – Detection of “Big Bang” neutrinos difficult Medium energy (MeV scale) – Detection of stellar neutrinos established High energy (TeV to EeV scale) – Detection of extragalactic neutrinos progressing 20 January 2005 Steve Dye, HPU 8 Neutrino AstrophysicsSN1987a http://www-personal.umich.edu/~jcv/imb/imbp5.html 20 January 2005 Steve Dye, HPU 9 http://elvis.phys.lsu.edu/svoboda/superk/cossun.pdf 20 January 2005 http://elvis.phys.lsu.edu/svoboda/superk/sun.gif Steve Dye, HPU 10 Neutrinos from Nuclear Reactors http://www.insc.anl.gov/pwrmaps/map/world_map.php 20 January 2005 Steve Dye, HPU 11 Underground Neutrino Detector KamLAND in Japan – 1000 tonnes of liquid scintillator – ~2000 PMTs – Rate in 400 tonnes ~1/(2 days) from reactors at 180 km 20 January 2005 Steve Dye, HPU 12 Anti-Neutrino Detection from John G. Learned “Monitoring All Earth Reactors” 20 January 2005 Steve Dye, HPU 13 Neutrinos in Japan KamLand signal primarily neutrinos from nuclear reactors Neutrinos from Earth detected! Raghavan hep-ex/0208038 20 January 2005 Steve Dye, HPU 14 Summary Point #1 Neutrinos exist with measured properties Neutrinos carry information from deep inside stars, galaxies, and Earth Neutrinos of energy ~1 MeV can be detected using proven techniques 20 January 2005 Steve Dye, HPU 15 Geophysics http://www.solarviews.com/cap/earth/earthfg2.htm 20 January 2005 Steve Dye, HPU 16 Seismology Earthquake waves – Pressure waves • P (primary) waves – Shear waves • S (secondary) waves Solids – Transmit P and S waves Fluids – Transmit only P waves 20 January 2005 http://www.mantleplumes.org/Energetics.html Steve Dye, HPU 17 Earth’s Interior http://mantleplumes.org/Energetics.html 20 January 2005 Steve Dye, HPU 18 Geodynamo Magnetic field – Dipole – Convection in outer core – Rotation of Earth Magnetic field required for life to exist – Deflects radiation – Helps retain atmosphere http://www.es.ucsc.edu/~glatz/geodynamo/html 20 January 2005 Steve Dye, HPU 19 Global Heat Flow http://www.geo.lsa.umich.edu/IHFC/heatflow.html >24,000 field measurements 20 January 2005 http://www.geo.lsa.umich.edu/IHFC/heatflow.html Steve Dye, HPU 20 Earth Radioactivity Long-lived radioactive isotopes Decay of heavy elements heats the Earth How much heat and from where are the main questions U/Th/K distribution in the core, mantle, crust http://neutrino2004.in2p3.fr/slides/monday/fiorentini.pdf 20 January 2005 Steve Dye, HPU 21 Summary Point #2 Much to be learned in geophysics – – – – Composition of mantle and core Origin of Earth Source of heat flow Mechanism of geodynamo 20 January 2005 Steve Dye, HPU 22 Geo-neutrinos Anti-neutrinos from the Earth Arise from decay of radioactive elements (U+Th+K) in crust, mantle, and maybe core Detection above 1.8 MeV proven (U+Th) Domogatsky et al., hep-ph/0409069 Rothschild, Chen and Calaprice: nucl-ex/9710001 20 January 2005 Steve Dye, HPU 23 Geo-neutrinos Contributions from continental crust, oceanic crust, and mantle Possible observational sites – – – – – – Japan Italy Canada Russia Curacao Hawaii 20 January 2005 Steve Dye, HPU 24 Geo-neutrinos at Curacao Dutch project – Long, narrow underground shafts – Instrumented with nuclear detectors – Strives to measure neutrino direction Goal: Neutrino tomography of Earth R.J. de Meijer EARTH Info-001 20 January 2005 Steve Dye, HPU 25 Anti-Neutrinos from the Core J. Marvin Herndon Breeder (fission) reactor deep within inner core Explains heat flow, geomagnetic field variability, He3/He4 Power output 3-10 TW Observable through neutrino emission 20 January 2005 Steve Dye, HPU 26 Geo-reactor neutrinos Test of geo-reactor hypothesis requires special location for clear signal – Far from man-made reactors – Far from continental crust Hawaii is excellent site 20 January 2005 Raghavan hep-ex/0208038 Steve Dye, HPU 27 HANOHANO (Hawaiian for magnificent) Hawaii Anti-Neutrino Observatory New initiative in Hawaii for neutrino geophysics project Objectives are: – Measure geo-neutrinos from mantle and U/Th – Test geo-reactor hypothesis Method: – Deploy KamLAND-like detector in the deep (4-5 km) ocean near Hawaii and operate for about 1 year Funding: – Submitting proposal to CEROS next week for design study – If successful, propose CEROS follow-on for prototype testing – Next go for order of $100M from NSF for full detector 20 January 2005 Steve Dye, HPU 28 Deep Ocean Technology Hawaii-2 Observatory – Deployed in 1998 – Another off Japan ’93 Neutrino detector possible in 3-5 years http://oceanusmag.whoi.edu/images/v42n2-chave1en.jpg 20 January 2005 Steve Dye, HPU 29 Summary and Conclusion Neutrino detection is a viable (only?) method for learning what is inside Earth Various neutrino geophysics projects being considered around the globe Hawaii is an excellent site for a project Deep ocean technology sufficiently advanced HANOHANO 20 January 2005 Steve Dye, HPU 30