75 research outputs found
Evidence for ground-state electron capture of K
Potassium-40 is a widespread isotope whose radioactivity impacts estimated
geological ages spanning billions of years, nuclear structure theory, and
subatomic rare-event searches - including those for dark matter and
neutrinoless double-beta decay. The decays of this long-lived isotope must be
precisely known for its use as a geochronometer, and to account for its
presence in low-background experiments. There are several known decay modes for
K, but a predicted electron-capture decay directly to the ground state
of argon-40 has never been observed, while theoretical predictions span an
order of magnitude. The KDK Collaboration reports on the first observation of
this rare decay, obtained using a novel combination of a low-threshold X-ray
detector surrounded by a tonne-scale, high-efficiency -ray tagger at
Oak Ridge National Laboratory. A blinded analysis reveals a distinctly nonzero
ratio of intensities of ground-state electron-captures () over
excited-state ones () of
(68% CL), with the null hypothesis rejected at 4 [Stukel et al.,
DOI:10.1103/PhysRevLett.131.052503]. This unambiguous signal yields a branching
ratio of
,
roughly half of the commonly used prediction. This first observation of a
third-forbidden unique electron capture improves understanding of low-energy
backgrounds in dark-matter searches and has implications for nuclear-structure
calculations. A shell-model based theoretical estimate for the
decay half-life of calcium-48 is increased by a factor of . Our
nonzero measurement shifts geochronological ages by up to a percent;
implications are illustrated for Earth and solar system chronologies.Comment: This is a companion submission to Stukel et al (KDK collaboration)
"Rare K decay with implications for fundamental physics and
geochronology" [arXiv:2211.10319; DOI: 10.1103/PhysRevLett.131.052503]. As
such, both texts share some figures and portions of text. This version
updates the text following its review and production proces
Systematic investigation of projectile fragmentation using beams of unstable B and C isotopes
Background: Models describing nuclear fragmentation and fragmentation fission deliver important input for planning nuclear physics experiments and future radioactive ion beam facilities. These models are usually benchmarked against data from stable beam experiments. In the future, two-step fragmentation reactions with exotic nuclei as stepping stones are a promising tool for reaching the most neutron-rich nuclei, creating a need for models to describe also these reactions. Purpose: We want to extend the presently available data on fragmentation reactions towards the light exotic region on the nuclear chart. Furthermore, we want to improve the understanding of projectile fragmentation especially for unstable isotopes. Method: We have measured projectile fragments from C10,12-18 and B10-15 isotopes colliding with a carbon target. These measurements were all performed within one experiment, which gives rise to a very consistent data set. We compare our data to model calculations. Results: One-proton removal cross sections with different final neutron numbers (1pxn) for relativistic C10,12-18 and B10-15 isotopes impinging on a carbon target. Comparing model calculations to the data, we find that the epax code is not able to describe the data satisfactorily. Using abrabla07 on the other hand, we find that the average excitation energy per abraded nucleon needs to be decreased from 27 MeV to 8.1 MeV. With that decrease abrabla07 describes the data surprisingly well. Conclusions: Extending the available data towards light unstable nuclei with a consistent set of new data has allowed a systematic investigation of the role of the excitation energy induced in projectile fragmentation. Most striking is the apparent mass dependence of the average excitation energy per abraded nucleon. Nevertheless, this parameter, which has been related to final-state interactions, requires further study
Local anaesthetics or their combination with morphine and/or magnesium sulphate are toxic for equine chondrocytes and synoviocytes in vitro
Systematic investigation of projectile fragmentation using beams of unstable B and C isotopes
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