Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting radiation, such as alpha or beta particles, or gamma rays. This process results in the transformation of the original atom into a different element or isotope. The rate of decay is typically measured by the half-life of the radioactive substance, which is the time it takes for half of the atoms in a sample to decay.
There are several types of radioactive decay, including:
To understand radioactive decay, consider the following key points:
By mastering the principles of radioactive decay, you will develop a strong foundation in nuclear chemistry and its real-world implications.