Nuclear decay, also known as radioactive decay, is the process by which an unstable atomic nucleus loses energy by emitting radiation. This process can result in the transformation of the original nucleus into a different element or a different isotope of the same element.
There are several types of nuclear decay, including:
Radioactive decay can be described using decay equations, which show the transformation of a radioactive nucleus into a different nucleus through the emission of particles or radiation. The general form of a radioactive decay equation is:
Original Nucleus → New Nucleus + Particle(s) or Radiation
The half-life of a radioactive substance is the time it takes for half of the radioactive nuclei present in a sample to decay. It is a characteristic property of each radioactive isotope and can be used to determine the rate of decay of a substance.
Nuclear decay has numerous applications in various fields, including medicine (e.g., nuclear medicine for imaging and treatment), energy production (e.g., nuclear power plants), and dating archaeological artifacts (e.g., carbon-14 dating).
When studying nuclear decay, it's important to:
Remember to review the fundamental principles of nuclear physics and atomic structure to build a strong foundation for understanding nuclear decay.