Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting ionizing particles or radiation. This process is spontaneous and occurs at a constant rate, which makes it useful for determining the age of rocks and fossils, as well as in medical imaging and treatments.
There are three main types of radioactive decay:
The half-life of a radioactive substance is the time it takes for half of the radioactive nuclei in a sample to undergo decay. Each radioactive isotope has a specific half-life, and this property is used to determine the age of rocks and other materials through a process called radiometric dating.
Radioactive decay has several practical applications, including:
When studying radioactive decay, it's important to understand the following key concepts:
Additionally, practicing problems involving half-life calculations and understanding the mathematical relationships involved in radioactive decay will solidify your understanding of the topic.
For more information and practice problems, refer to your textbook, class notes, and reputable online resources.