Radiobiology
Beta decay is a type of radioactive decay in which an unstable atomic nucleus transforms into a more stable configuration by emitting beta particles, which can either be electrons (beta minus decay) or positrons (beta plus decay). This process involves the conversion of a neutron into a proton or vice versa, altering the atomic number and thus changing the identity of the element. Beta decay is an essential process in understanding radioactive decay and half-life, as it contributes to the transformation of elements over time.
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