Understanding Radioactive Decay
Radioactive decay follows an exponential decay pattern described by N = N₀ × (½)^(t/t½). Each radioactive isotope has a characteristic half-life that is constant regardless of environmental conditions — temperature, pressure, or chemical bonding do not affect it. This predictability makes radioactive decay useful for dating archaeological artifacts, medical imaging, and nuclear power.
Common Radioactive Isotopes
| Isotope | Half-Life | Application |
|---|---|---|
| Carbon-14 | 5,730 years | Archaeological dating |
| Uranium-238 | 4.47 billion years | Geological dating, nuclear power |
| Iodine-131 | 8.02 days | Thyroid cancer treatment |
| Technetium-99m | 6.01 hours | Medical imaging (most common) |
| Cobalt-60 | 5.27 years | Cancer radiation therapy |