The Exponential Decay Law states that the probability of a nucleus decaying per unit time is constant. This leads to the mathematical relationship , where is the number of nuclei remaining at time , is the initial number, and is the decay constant.
Half-life () is the time required for half of the radioactive nuclei in a sample to decay. It is a constant property for a specific isotope and is related to the decay constant by the formula .
Because the process is random, we can only predict the behavior of large populations of atoms using statistics. For a single atom, we can only state the probability that it will decay within a certain timeframe.
Decay is unaffected by external physical conditions such as temperature, pressure, or chemical bonding. This makes radioactive isotopes reliable 'clocks' for geological and archaeological dating.
| Feature | Alpha () | Beta () | Gamma () |
|---|---|---|---|
| Nature | Helium Nucleus () | High-speed Electron | EM Wave (Photon) |
| Charge | |||
| Ionizing Power | Very High | Medium | Low |
| Penetration | Low (stopped by paper) | Medium (stopped by Al) | High (reduced by Lead) |
Account for Background Radiation: In many problems, you must subtract the background count rate from the measured count rate before performing half-life calculations. Failure to do this will result in an incorrectly high calculated half-life.
Check the Units: Ensure time units for half-life and total elapsed time match (e.g., both in years or both in seconds) before calculating the number of half-lives.
Graph Interpretation: When given a decay graph, always identify the initial value (-intercept) and find the time it takes for that value to drop exactly by half. Repeat this for a second interval (e.g., from to ) to verify the half-life is constant.
Sanity Check: If a substance has a half-life of 10 minutes and 30 minutes have passed, the remaining amount must be exactly of the start. If your calculation gives a larger number, you likely multiplied instead of divided.