New Results from T2K Conclusively Show Muon Neutrinos Transform to Electron Neutrinos

New Results from T2K Conclusively Show Muon Neutrinos Transform to Electron Neutrinos

Jul 19, 2013 – 8:30:00 AM

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Super Kamiokande is the worldʼs largest underground neutrino detector, and is located 1000 metres underground in Kamioka Mine, Hida, Gifu Precture, Japan. It is affiliated with the Kamioka Observatory of the Institute of Cosmic Ray Research at the University of Tokyo. In addition to detecting T2K neutrinos, Super Kamiokande observes neutrinos produced by collisions between cosmic rays and molecules in the Earthʼs upper atmosphere. It is also searching for proton decays, which have never been observed to date. Super Kamiokande consists of a large cylinder 39.3 metres in diameter and 41 metres high that contains 50,000 tons of ultra-pure water. The inner walls of the cylinder are lined with about 11,200 photomultiplier tubes to detect Cerenkov light, which is emitted when a charged particle travels faster than the speed of light in water (this is three quarters of its speed in vacuum).

STONY BROOK, NY, Embargoed until 8:30 am EST on Friday July 19, 2013 – Today at the European Physical Society meeting in Stockholm, the international T2K collaboration announced definitive observation of muon neutrino to electron neutrino transformation.  In 2011, the collaboration announced the first indication of this process, a new type of neutrino oscillation, then; now with 3.5 times more data this transformation is firmly established.  The probability that random statistical fluctuations alone would produce the observed excess of electron neutrinos is less than one in a trillion.  Equivalently the new results exclude such possibility at 7.5 sigma level of significance. This T2K observation is the first of its kind in that an explicit appearance of a unique flavor of neutrino at a detection point is unequivocally observed from a different flavor of neutrino at its production point.

In the T2K experiment in Japan, a muon neutrino beam is produced in the Japan Proton Accelerator Research Complex, called J-PARC, located in Tokai village, Ibaraki prefecture, on the east coast of Japan.  The neutrino beam is monitored by a detector complex in Tokai and aimed at the gigantic Super-Kamiokande underground detector in Kamioka, near the west coast of Japan, 295 km (185 miles) away from Tokai. An analysis of the data from the Super-Kamiokande detector associated with the neutrino beam time from J-PARC reveals that there are more electron neutrinos (a total of 28 events) than would be expected (4.6 events) without this new process.

Neutrino oscillation is a manifestation of a long range quantum mechanical interference. Observation of this new type of neutrino oscillation leads the way to new studies of charge-parity (CP) violation which provides a distinction in physical processes involving matter and antimatter.  This phenomenon has only been observed in quarks (for which Nobel prizes were awarded in 1980 and 2008). CP violation in neutrinos in the very early universe may be the reason that the observable universe today is dominated by matter and no significant antimatter, which is one of the most profound mysteries in science. Now with T2K firmly establishing this form of neutrino oscillation that is sensitive to CP violation, a search for CP violation in neutrinos becomes a major scientific quest in the coming years, and T2K will continue to play a leading role. The T2K experiment expects to collect 10 times more data in the near future, including data with antineutrino beam for studies of CP violation in neutrinos.

J-PARC Neutrino Experimental Facility. The proton beams extracted from the main ring synchrotron at J-PARC are directed in a westward direction through the T2K primary beam line. The beams strike a target composed of graphite rods (image 1), and produce a large number of positively-charged pions. The directions of motion of these pions are made to converge in the forward direction by some magnetic horns. The pions then decay into muons and muon neutrinos in a 100-metre-long tunnel known as the decay volume (image 2). The muons and any remaining pions are stopped by a second layer of graphite, while the muon neutrinos pass through this layer. The composition of the muon-neutrino beam is measured by a near detector located 280 metres downstream of the target (image 3). Neutrino oscillations are studied by comparing the composition of the muon-neutrino beam at the near detector with its composition at Super Kamiokande, which is 295 km from the target.

The T2K experiment was constructed and is operated by an international collaboration. The current T2K collaboration consists of over 400 physicists from 59 institutions in 11 countries [Canada, France, Germany, Italy, Japan, Poland, Russia, Switzerland, Spain, UK and US].  The experiment is primarily supported by the Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT). Additional support is provided by the following funding agencies from participating countries: NSERC, NRC and CFI, Canada; CEA and CNRS/IN2P3, France; DFG, Germany; INFN, Italy; Ministry of Science and Higher Education, Poland; RAS, RFBR and the Ministry of Education and Science of the Russian Federation; MICINN and CPAN, Spain; SNSF and SER, Switzerland; STFC, U.K.; DOE, U.S.A.

The US T2K collaborating team of approximately 70 members [Boston University, UC Irvine, University of Colorado, Colorado State University, Duke University, Louisiana State University, Stony Brook University, University of Pittsburgh, University of Rochester, and University of Washington (Seattle)] is funded by the US Department of Energy, Office of Science. The US groups have built super-conducting corrector magnets, proton beam monitor electronics, the second neutrino horn and a GPS time synchronization system for the T2K neutrino beamline; and a pi-zero detector and a side muon range detector (partial detector) in the T2K near detector complex. They are also part of the team that built, upgraded and operates the Super-Kamiokande detector.
 
This discovery was made possible with the unyielding and tireless effort by the J-PARC staff members and the management to deliver high quality beam to T2K after the devastating March 2011 earthquake in eastern Japan which caused severe damage to the accelerator complex at J-PARC, and abruptly discontinued the data-taking run of the T2K experiment.

“In 1998, the discovery of neutrino oscillation in the atmospheric neutrinos by the Super-Kamiokande experiment led us to a new journey into the fascinating and mysterious world of neutrinos which is full of surprises,” said Chang Kee Jung, Professor of Physics at Stony Brook University, and International Co-Spokesperson, T2K Collaboration. “This discovery of electron neutrino appearance from muon neutrinos by the T2K experiment opens another critical door in our journey to unveil the secrets of our universe. I feel extremely lucky and ecstatic to be involved in both of these discoveries. I am confident that the CP violation in neutrinos will be eventually discovered in this journey.”

Editor’s Note: More detailed information on this announcement including images, T2K experiment and T2K collaboration can be found from the T2K public webpage.