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Potassium-40 (K) is a naturally-occurring, radioactive isotope of interest to rare-event searches as a challenging background. In particular, NaI scintillators contain K contamination which produces an irreducible signal originating from this isotope's electron capture (EC) decays. In geochronology, the lifetime of K is utilized in dating techniques. The direct-to-ground-state EC intensity () of this radionuclide has never been measured, and theoretical predictions are highly variable (). The poorly understood intensity of this branch may affect the interpretation or precision of experimental results, including those probing DM signals in the (2-6) keV region. The KDK ("potassium decay") experiment is finalizing the first measurement of this branch, which uses a coincidence technique between a high-resolution Silicon Drift Detector and a highly-efficient () Modular Total Absorption Spectrometer (Oak Ridge National Labs) to differentiate ground and excited state EC decays of K. We report on the status of the main K analysis leading up to unblinding, along with a preliminary measurement of Zinc-65 decays used to test analysis methods.
Dr
N.T. Brewer(Oak Ridge National Laboratory Physics Division, Oak Ridge, TN)
Mr
H. Davis(Department of Nuclear Engineering, University of Tennesee, Knoxville, TN)
Prof.
P.C.F. Di Stefano(Queen's University, Kingston, ON)
Prof.
E.D. Lukosi(Department of Nuclear Engineering, University of Tennesee, Knoxville, TN)
Dr
B.C. Rasco(Oak Ridge National Laboratory Physics Division, Oak Ridge, TN)
Dr
K.P. Rykaczewski(Oak Ridge National Laboratory Physics Division, Oak Ridge, TN)
Dr
M. Stukel(Queen's University, Kingston, ON)