Radioactive decay is a natural process by which an unstable atomic nucleus loses energy by emitting radiation. This process transforms the nucleus into a more stable form, often of a different chemical element. The rate of decay is characterized by the half-life, which is the time required for half of a given quantity of a radioactive isotope to decay.
The radioactive decay process is described by the exponential decay formula:
\[N(t) = N_0 \cdot e^{-\lambda t}\]Where:
The decay constant \(\lambda\) is related to the half-life \(t_{1/2}\) by the equation:
\[\lambda = \frac{\ln(2)}{t_{1/2}}\]To calculate the remaining amount of a radioactive substance:
Let's calculate the remaining amount of a radioactive substance with an initial quantity of 1000 units, a half-life of 5 years, after 10 years:
\[N(10) = 1000 \cdot e^{-\frac{\ln(2)}{5} \cdot 10} \approx 250 \text{ units}\]This diagram illustrates the radioactive decay process. The left circle represents the initial amount of radioactive material, while the right circle shows the remaining amount after 10 years. The size difference between the circles visually demonstrates the decay that has occurred over time.
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