Half-life, denoted as \( t_{\text{half}} \), is a crucial concept in understanding radioactive decay. It represents the time required for half of a given quantity of a radioactive substance, known as a radioisotope, to decay. A radioisotope is an unstable isotopic form of an element that emits radiation as it transforms into a more stable state.
For instance, consider a radioisotope with a half-life of one day. If we start with 10 grams of this substance, we can track its decay over time. Initially, at \( t = 0 \) days, we have 100% of the substance, which is 10 grams. After one day, or one half-life, half of the substance decays, leaving us with 5 grams, which is 50% of the original amount.
Continuing this process, after another day (two half-lives), we again lose half of the remaining substance. Starting with 5 grams, we are left with 2.5 grams, representing 25% of the original quantity. After a third day (three half-lives), we lose half of 2.5 grams, resulting in 1.25 grams, which is 12.5% of the initial amount.
This pattern illustrates that with each passing half-life, the quantity of the substance decreases by half. The decay process can continue indefinitely, with each half-life reducing the remaining amount of the radioisotope. Understanding half-life is essential for applications in fields such as nuclear medicine, radiometric dating, and understanding the behavior of radioactive materials.