Beta decay is a type of radioactive decay where a neutron in an unstable nucleus transforms into a proton, releasing an electron (beta particle) in the process. This type of decay increases the atomic number of the element by one while keeping the mass number the same. It is a common way for unstable isotopes to stabilize themselves.
This is seen in the exercise example, where after uranium-239 is formed, it undergoes beta decay to become neptunium-239. This decay emits a beta particle and transforms a neutron into a proton, increasing the atomic number from 92 to 93. Subsequently, neptunium-239 undergoes another beta decay to form plutonium-239, raising the atomic number to 94.
Important characteristics of beta decay include:
- The transformation of a neutron into a proton.
- The emission of a beta particle, which is an electron or positron.
- An increase in the atomic number of the resulting isotope.
Beta decay is a crucial process in nuclear reactions, particularly for neutron-rich isotopes moving towards stability.