Abstract
The radioactivity of the α particle is among the most compelling evidence for the existence of cluster structures in atomic nuclei. During the decay process, a pre-existing α particle tunnels through the potential barrier formed by the residual nucleus1,2. The degree of preformation of the α particle, a strongly bound system of two protons and two neutrons, is extracted from the data by dividing the α-decay probability by the barrier penetrability for a given particle energy. The preformation probability changes rapidly near nuclear shell closures, which is direct evidence that clustering is connected to nuclear structure3. Enhanced preformation was observed in the lightest α-particle emitters, spherical tellurium and xenon isotopes decaying to magic isotopes of tin. Here we show the most extreme case of α-particle preformation from the measurement of the decay of tellurium-104 (104Te). With a half-life of 7.2−1.5+2.3ns, 104Te is the fastest ground-state α-emitting nucleus known so far. The deduced preformation demonstrates that the enhancement is greater for 104Te than for any other nucleus. One nuclear model that can explain our observation postulates that the α particle can exist only in the low-nuclear-matter-density regions on the surface of the nucleus. The uniquely high preformation for 104Te is attributed to its relation to doubly magic tin-100 (100Sn), creating conditions conducive to form an α particle.
| Original language | English |
|---|---|
| Pages (from-to) | 52-56 |
| Number of pages | 5 |
| Journal | Nature |
| Volume | 654 |
| Issue number | 8117 |
| DOIs | |
| State | Published - Jun 4 2026 |
Funding
We would like to extend our gratitude to the entire RIBF operations team. Also, we would like to thank T. Papenbrock and K. L. Jones for helpful discussions. The material is based on work supported in part by the U.S. Department of Energy, Office of Science, Office of Nuclear Physics under contract nos. DE-FG02-96ER40983 (UTK) and DE-AC05-00OR22725 (ORNL), the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under contract DE-AC52-07NA27344 and the Polish National Science Center under grant no. 2020/39/B/ST2/02346 and contract no. UMO-2019/33/B/ST2/02908. This work was also sponsored by JSPS KAKENHI grant nos. 25H01273 and 24K0655, the RIKEN programme RiNA-Net, the Stewardship Science Academic Alliances programme through DOE awards no. DE-NA0003899 (UTK), the National Science Foundation NSF-MRI-1919735 (UTK), the Spanish MCIN/AEI/10.13039/501100011033 under grants TED2021-130592B-I00 (PROTOTWIN) and PID2021-126998OB-I00 (FASCINA) and supported by BMBF under Verbundprojekt 05P2021 (ErUM-FSP T07) grant 05P21PKFN1. A.E. was supported by the DFG under grant number JO 391/20-1. A.A. acknowledges support from the Polish National Agency for Academic Exchange (NAWA) under the STER Programme - Internationalisation of Doctoral Schools, project ‘International Doctoral Program at NCBJ & IChTJ’ (project no. BPI/STE/2021/1/00033/U/00001). This manuscript has been authored by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the US Department of Energy (DOE). The US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan (https://www.energy.gov/doe-public-access-plan). We would like to extend our gratitude to the entire RIBF operations team. Also, we would like to thank T. Papenbrock and K. L. Jones for helpful discussions. The material is based on work supported in part by the U.S. Department of Energy, Office of Science, Office of Nuclear Physics under contract nos. DE-FG02-96ER40983 (UTK) and DE-AC05-00OR22725 (ORNL), the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under contract DE-AC52-07NA27344 and the Polish National Science Center under grant no. 2020/39/B/ST2/02346 and contract no. UMO-2019/33/B/ST2/02908. This work was also sponsored by JSPS KAKENHI grant nos. 25H01273 and 24K0655, the RIKEN programme RiNA-Net, the Stewardship Science Academic Alliances programme through DOE awards no. DE-NA0003899 (UTK), the National Science Foundation NSF-MRI-1919735 (UTK), the Spanish MCIN/AEI/10.13039/501100011033 under grants TED2021-130592B-I00 (PROTOTWIN) and PID2021-126998OB-I00 (FASCINA) and supported by BMBF under Verbundprojekt 05P2021 (ErUM-FSP T07) grant 05P21PKFN1. A.E. was supported by the DFG under grant number JO 391/20-1. A.A. acknowledges support from the Polish National Agency for Academic Exchange (NAWA) under the STER Programme - Internationalisation of Doctoral Schools, project ‘International Doctoral Program at NCBJ & IChTJ’ (project no. BPI/STE/2021/1/00033/U/00001). This manuscript has been authored by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the US Department of Energy (DOE). The US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( https://www.energy.gov/doe-public-access-plan ).
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