The material stops inside this detector, which is filled with carbon dioxide gas, and decays after about ten milliseconds by emitting a positron and a neutrino (beta-plus decay). They sent this beam of radioactive material, oxygen-13, into a piece of equipment known as the Texas Active Target Time Projection Chamber (TexAT TPC). In this experiment, researchers used a particle accelerator known as a cyclotron at the Cyclotron Institute at Texas A&M University to produce a beam of radioactive nuclei at high energies (approximately 10% the speed of light). The findings can inform scientists about decay processes and the properties of the nucleus before the decay. This new decay mode is the first observation of three helium-nuclei (alpha particles) and a proton being emitted following beta-decay. After this initial beta-decay, the resulting nucleus can have enough energy to boil off extra particles and make itself more stable. This is where a proton turns into a neutron and emits some of the produced energy by emitting a positron and an antineutrino. Scientists have previously observed interesting modes of radioactive decay following the process called beta-plus decay. Scientists observed this decay by watching a single nucleus break apart and measuring the breakup products. In this decay, a lighter form of oxygen, oxygen-13 (with eight protons and five neutrons), decays by breaking into three helium nuclei (an atom without the surrounding electrons), a proton, and a positron (the antimatter version of an electron). Scientists have now observed a new decay mode for the first time. Some materials may undergo radioactive decay to form more stable isotopes. Not all of the material around us is stable.
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