Beta decay is a fascinating process in the world of nuclear chemistry. It involves the transformation of a neutron into a proton or vice versa within an atomic nucleus. During this process, a beta particle is emitted. Beta particles come in two types: beta-minus (β⁻) and beta-plus (β⁺) particles.
In beta-minus decay, a neutron turns into a proton. As a result, an electron, which is the β⁻ particle, is ejected from the nucleus. This process increases the atomic number by one but keeps the mass number the same. For example, carbon-14 undergoes β⁻ decay to become nitrogen-14.
In beta-plus decay, a proton is converted into a neutron, releasing a positron, the β⁺ particle. This action decreases the atomic number by one, again without altering the mass number. An isotope like oxygen-15 can undergo β⁺ decay to form nitrogen-15.
- Beta particle types: β⁻ (electron), β⁺ (positron)
- Beta-minus increases atomic number
- Beta-plus decreases atomic number
Beta decay is essential for understanding nuclear reactions and plays a crucial role in applications ranging from medical imaging to understanding the age of archaeological finds.