Isotope Geochemistry
Beta decay is a type of radioactive decay in which an unstable nucleus transforms into a more stable one by emitting a beta particle, which can either be an electron (beta-minus decay) or a positron (beta-plus decay). This process plays a crucial role in the stability of atomic nuclei and is integral to understanding the various forms of radioactive decay, the calculation of half-lives, and the principles behind radiometric dating methods.
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