Abstract
Potassium-40 (40K) is a long-lived, naturally occurring radioactive isotope. The decay products are prominent backgrounds for many rare event searches, including those involving NaI-based scintillators. 40K also plays a role in geochronological dating techniques. The branching ratio of the electron capture directly to the ground state of 40Ar has never been measured, which can cause difficulty in interpreting certain results or can lead to lack of precision depending on the field and analysis technique. The KDK (Potassium (K) Decay (DK)) collaboration is measuring this decay. A composite method has a silicon drift detector with an enriched, thermally deposited 40K source inside the Modular Total Absorption Spectrometer. This setup has been characterized in terms of energy calibration, gamma tagging efficiency, live time and false negatives and positives. A complementary, homogeneous, method is also discussed; it employs a KSr2I5:Eu scintillator as source and detector.
Original language | English |
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Article number | 165593 |
Journal | Nuclear Instruments and Methods in Physics Research, Section A: Accelerators, Spectrometers, Detectors and Associated Equipment |
Volume | 1012 |
DOIs | |
State | Published - Oct 1 2021 |
Funding
Work was performed at Oak Ridge National Laboratory, managed by UT-Battelle, LLC, for the U.S. Department of Energy under Contract DE-AC05-00OR22725 . Thermal deposition was conducted at the Center for Nanophase Materials Sciences, which is a DOE Office of Science User Facility. This manuscript has been authored by UT-Battelle, LLC under Contract No. DE-AC05-00OR22725 with the U.S. Department of Energy. The United States Government retains and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a non-exclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The Department of Energy will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ). Funding in Canada has been provided by NSERC through SAPIN and SAP RTI grants, as well as by the Faculty of Arts and Science of Queen’s University, and by the McDonald Institute. US support has also been supplied by the Joint Institute for Nuclear Physics and Applications, USA . This material is based upon work supported by the U.S. Department of Homeland Security under grant no. 2014-DN-077-ARI088-01 . Disclaimer: The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Department of Homeland Security.
Funders | Funder number |
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Faculty of Arts and Science of Queen’s University | |
McDonald Institute | |
U.S. Department of Energy | DE-AC05-00OR22725 |
U.S. Department of Homeland Security | 2014-DN-077-ARI088-01 |
Oak Ridge National Laboratory | |
Natural Sciences and Engineering Research Council of Canada |
Keywords
- DAMA
- Electron capture
- Geochronology
- KSrI:Eu
- MTAS
- Potassium
- Rare decays
- SDD