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Measurement of cosmogenic 9Li in Super-Kamiokande with gadolinium loaded water

  • Super-Kamiokande Collaboration
  • Tokyo University of Science
  • University of Tokyo
  • Long Beach VA and University of California
  • Universidad Autónoma de Madrid
  • British Columbia Institute of Technology
  • TRIUMF
  • Boston University
  • High Energy Accelerator Research Organization (KEK)
  • California State University, Dominguez Hills
  • Chonnam National University
  • Duke University
  • Ip Paris
  • Gifu University
  • Gwangju Institute of Science and Technology
  • University of Glasgow
  • University of Hawaii
  • Institute for Basic Science (IBS)
  • ICISE
  • Imperial College London
  • Politecnico di Bari
  • University of Naples Federico II
  • University of Padova
  • University of Rome
  • Keio University
  • King's College London
  • Kobe University
  • Kyoto University
  • University of Liverpool
  • Miyagi University of Education
  • Nagoya University
  • National Centre for Nuclear Research (NCBJ)
  • Stony Brook University
  • York College/The City University of New York
  • Okayama University
  • Osaka Electro-Communication University
  • University of Oxford
  • CCLRC Rutherford Appleton Laboratory
  • Seoul National University
  • The University of Sheffield
  • Shizuoka University of Welfare
  • Sungkyunkwan University
  • Tohoku University
  • Tokai University
  • Tokyo Institute of Technology
  • University of Victoria
  • Tsinghua University
  • University of Warsaw
  • University of Warwick
  • University of Winnipeg
  • Yokohama National University

Résultats de recherche: Contribution à un journalArticle de conférenceRevue par des pairs

Résumé

Super-Kamiokande is a large water Cherenkov detector located approximately 1,000 m underground in Kamioka, Japan. The detector is a cylindrical tank 39.3 m in diameter and 41.4 m high, filled with about 50 kton of gadolinium loaded water. We measured 9Li isotopic nuclei produced by muon spallation using the data taken from 2020 to 2022 by the Super-Kamiokande detector with 0.011% gadolinium concentration in water. Cosmic-ray muons that penetrate the detector form hadron showers in water and secondary hadrons produce unstable radioisotopes through the spallation. Among those spallation products, 9Li is a long-lived radioactive isotope with a lifetime of about 0.26 seconds. It emits an electron and a neutron at a branching ratio of 50.8%, which is difficult to distinguish from the inverse beta decay caused by electron antineutrinos. Therefore, 9Li is one of the main background sources in the observation of diffuse supernova neutrino background. In this study, the energy spectrum of the electrons was measured with a threshold at 4.5 MeV which is lowered from the previous result with pure water. We will report the analysis method and results.

langue originaleAnglais
Numéro d'article1058
journalProceedings of Science
Volume444
étatPublié - 27 sept. 2024
Evénement38th International Cosmic Ray Conference, ICRC 2023 - Nagoya, Japon
Durée: 26 juil. 20233 août 2023

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