Radioactivity, discovered by Becquerel in 1896, is the spontaneous disintegration of an unstable nucleus with the emission of radiation. Three kinds of emission occur:
- Alpha ($\alpha$) decay: the nucleus emits a helium nucleus ${}^{4}_{2}\text{He}$, so $Z$ falls by 2 and $A$ by 4: ${}^{A}_{Z}X \to {}^{A-4}_{Z-2}Y + {}^{4}_{2}\text{He}$. $\alpha$-particles are heavy, highly ionising but poorly penetrating (stopped by paper).
- Beta ($\beta$) decay: a neutron converts to a proton, ejecting an electron and an antineutrino: ${}^{A}_{Z}X \to {}^{A}_{Z+1}Y + {}^{0}_{-1}e + \bar{\nu}$. Here $Z$ rises by 1, $A$ is unchanged. $\beta$-particles are lighter and more penetrating (stopped by aluminium).
- Gamma ($\gamma$) decay: the nucleus, left excited after $\alpha$ or $\beta$ emission, releases a high-energy photon. There is no change in $Z$ or $A$. $\gamma$-rays are uncharged and the most penetrating (need thick lead or concrete).
Radioactive decay is random for a single nucleus but precise for large numbers. The number of nuclei decaying per unit time is proportional to the number present, giving the radioactive decay law $N = N_0 e^{-\lambda t}$, where $N_0$ is the initial number, $N$ the number left after time $t$, and $\lambda$ the decay constant (probability of decay per nucleus per second).
The activity $R$ is the rate of decay, $R = \lambda N = R_0 e^{-\lambda t}$, measured in becquerel (1 Bq = 1 decay/s) or curie (1 Ci $= 3.7 \times 10^{10}$ Bq).
The half-life $T_{1/2}$ is the time for half the nuclei to decay. Setting $N = \frac{N_0}{2}$ in the decay law gives $T_{1/2} = \frac{0.693}{\lambda}$. After $n$ half-lives, the fraction remaining is $\left(\frac{1}{2}\right)^n$. The mean (average) life is $\tau = \frac{1}{\lambda} = \frac{T_{1/2}}{0.693} = 1.44\, T_{1/2}$.
Large amounts of energy are also released in nuclear reactions. In nuclear fission, a heavy nucleus such as ${}^{235}_{92}\text{U}$ captures a slow neutron and splits into two medium nuclei plus a few neutrons, releasing about $200\ \text{MeV}$ per fission. The freed neutrons can trigger a self-sustaining chain reaction — controlled in a reactor, uncontrolled in a bomb. In nuclear fusion, light nuclei combine, as in the Sun where hydrogen fuses to helium: $4\,{}^{1}_{1}\text{H} \to {}^{4}_{2}\text{He} + 2e^{+} + \text{energy}$. Fusion releases even more energy per nucleon than fission but needs extremely high temperatures to overcome Coulomb repulsion. In every case the energy comes from the increase in binding energy per nucleon — mass is converted to energy through $E = \Delta m\, c^2$.