Radioactive Decay

Nuclear Chemistry

방사성 붕괴

Definición

La transformación espontánea de un núcleo atómico inestable en una configuración más estable mediante la emisión de radiación en forma de partículas alfa, partículas beta o rayos gamma.

Explicación detallada

Three principal modes account for most decay. Alpha emission expels a helium nucleus, reducing the mass number by four and the atomic number by two, and is characteristic of the heaviest nuclides. Beta-minus emission converts a neutron into a proton with the ejection of an electron and an antineutrino, raising the atomic number by one at constant mass number, while beta-plus emission and electron capture move in the opposite direction. Gamma emission carries away excess energy from an excited nucleus without changing its composition. The process is statistical: the number of nuclei decaying in a given interval is proportional to the number present, which gives an exponential law and a constant half-life independent of the sample size. Successive decays of the heavy nuclides form the natural decay chains that terminate at stable lead isotopes.