Radioactivity is the spontaneous disintegration of unstable atomic nuclei, accompanied by the emission of ionizing radiation. The three main types of radiation emitted are:
| Radiation | Symbol | Nature | Charge | Mass |
|---|---|---|---|---|
| Alpha | Helium nucleus () | |||
| Beta | Electron or positron | or | ||
| Gamma | Electromagnetic photon |
Radioactive decay is described as spontaneous because:
Example: Heating a radioactive sample, placing it under high pressure, or changing its chemical compound does not alter its rate of decay or half-life.
This is fundamentally different from chemical reactions, which can be sped up or slowed down by changing temperature or adding a catalyst.
Radioactive decay is described as random because:
Analogy: Like flipping a coin — you cannot predict the outcome of a single flip, but for a large number of flips you can predict that approximately half will be heads.
Because of this randomness, the count rate from a Geiger counter fluctuates randomly around a mean value, even for a constant source. These fluctuations are direct evidence of the random nature of decay.
Because individual decays are random, the law of radioactive decay () is a statistical law — it is only accurate for a large number of nuclei. For a small sample, fluctuations become significant.
The decay constant represents the probability of decay per unit time for a single nucleus. It is a fixed property of the isotope and does not change as the sample ages.