Multisite event discrimination for the majorana demonstrator

Majorana Collaboration

Research output: Contribution to journalArticlepeer-review

27 Scopus citations

Abstract

The Majorana Demonstrator is searching for neutrinoless double-beta decay (0νββ) in Ge76 using arrays of point-contact germanium detectors operating at the Sanford Underground Research Facility. Background results in the 0νββ region of interest from data taken during construction, commissioning, and the start of full operations have been recently published. A pulse shape analysis cut applied to achieve this result, named AvsE, is described in this paper. This cut is developed to remove events whose waveforms are typical of multisite energy deposits while retaining (90±3.5)% of single-site events. This pulse shape discrimination is based on the relationship between the maximum current and energy, and tuned using Th228 calibration source data. The efficiency uncertainty accounts for variation across detectors, energy, and time, as well as for the position distribution difference between calibration and 0νββ events, established using simulations.

Original languageEnglish
Article number065501
JournalPhysical Review C
Volume99
Issue number6
DOIs
StatePublished - Jun 7 2019

Funding

This material is based upon work supported by the U.S. Department of Energy, Office of Science, Office of Nuclear Physics under Awards No. DE-AC02-05CH11231, No. DE-AC05-00OR22725, No. DE-AC05-76RL0130, No. DE-AC52-06NA25396, No. DE-FG02-97ER41020, No. DE-FG02-97ER41033, No. DE-FG02-97ER41041, No. DE-SC0010254, No. DE-SC0012612, No. DE-SC0014445, and No. DE-SC0018060. We acknowledge support from the Particle Astrophysics Program and Nuclear Physics Program of the National Science Foundation through Grants No. MRI-0923142, No. PHY-1003399, No. PHY-1102292, No. PHY-1206314, No. PHY-1614611, No. PHY-1812409, and No. PHY-1812356. We gratefully acknowledge the support of the U.S. Department of Energy through the LANL/LDRD Program and through the PNNL/LDRD Program for this work. We acknowledge support from the Russian Foundation for Basic Research, Grant No. 15-02-02919. We acknowledge the support of the Natural Sciences and Engineering Research Council of Canada, funding Reference No. SAPIN-2017-00023, and from the Canada Foundation for Innovation John R. Evans Leaders Fund. This research used resources provided by the Oak Ridge Leadership Computing Facility at Oak Ridge National Laboratory and by the National Energy Research Scientific Computing Center, a U.S. Department of Energy Office of Science User Facility. We thank our hosts and colleagues at the Sanford Underground Research Facility for their support.

FundersFunder number
Canada Foundation for Innovation John R. Evans Leaders Fund
LANL/LDRD
National Energy Research Scientific Computing Center
Office of Nuclear PhysicsDE-SC0014445
PNNL/LDRD
U.S. Department of Energy Office of Science
National Science FoundationPHY-1812409, 0923142, 1102292, 1812356, 1003399, 1206314, 1812409
U.S. Department of Energy
Office of Science
Oak Ridge National Laboratory
Natural Sciences and Engineering Research Council of CanadaSAPIN-2017-00023
Russian Foundation for Basic Research15-02-02919

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