There are three main types of radioactive decay: alpha, beta, and gamma decay. Alpha decay occurs when the nucleus ejects an alpha particle (helium nucleus) to reduce proton repulsion. Beta decay occurs when the nucleus emits an electron or positron to balance the neutron to proton ratio. Gamma decay happens when the nucleus releases a high energy photon to fall to a lower energy state. Natural radioactivity involves unstable isotopes decaying through alpha and beta emission until becoming stable lead isotopes, while artificial radioactivity is inducing nuclear reactions through bombardment.