Role reversal in proton capture
DOI: 10.1063/PT.5.7205
The synthesis of heavy nuclei in stars and stellar explosions is for the most part well understood. Most isotopes of elements beyond iron are created through a sequence of neutron captures and subsequent radioactive decays. But a few dozen naturally occurring nuclides, all with high proton-to-neutron ratios, defy explanation by that mechanism, and their origin remains mysterious. To try to understand how those proton-rich nuclei can form, nuclear astrophysicists turn to the p process, or proton-capture reaction. The conventional technique for measuring p-process cross sections, necessary for modeling nucleosynthesis, involves accelerating a beam of protons onto a stationary target. Because that method requires a target material that doesn’t decay away over the course of the experiment, many important p-process reactions involving short-lived nuclides have been inaccessible. Now René Reifarth and colleagues
More about the authors
Johanna L. Miller, jmiller@aip.org