Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting radiation, such as alpha particles, beta particles, and gamma rays. This process results in the transformation of the original atom into a different element.
There are three main types of radioactive decay:
The half-life of a radioactive substance is the time it takes for half of the original radioactive atoms to decay. It is a characteristic property of each radioactive isotope and can be used to determine the age of a sample or the rate of decay of a radioactive substance.
Radioactive decay has numerous practical applications, including carbon dating to determine the age of organic materials, medical imaging using radioactive isotopes, and power generation in nuclear reactors.
Understanding the concept of radioactive decay and its applications is essential for various scientific fields and real-world scenarios.
.