define half-life
Radioactive Decay ⚛️
What is Radioactive Decay?
Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting radiation. Think of it like a leaking balloon: the balloon (nucleus) slowly lets out air (particles) until it stabilises. In the same way, an unstable atom releases particles or energy until it becomes stable.
Types of Decay
- α‑decay: emission of a helium nucleus (2 protons + 2 neutrons)
- β‑decay: conversion of a neutron into a proton (or vice versa) with emission of an electron or positron
- γ‑decay: emission of high‑energy photons (gamma rays) from an excited nucleus
Defining Half‑Life ⏳
The half‑life of a radioactive isotope is the time taken for half of the atoms in a sample to decay. It is a constant for each isotope and gives a convenient way to describe how quickly a substance decays.
Mathematically, if N₀ is the initial number of atoms, then after time t the remaining number N(t) is: $$N(t) = N_0 \, e^{-\lambda t}$$ where λ is the decay constant. The half‑life t_{1/2} is related to λ by: $$t_{1/2} = \frac{\ln 2}{\lambda} \approx \frac{0.693}{\lambda}.$$
Common Half‑Lives
| Isotope | Half‑Life |
|---|---|
| Carbon‑14 | ≈ 5,730 years |
| Uranium‑238 | ≈ 4.5 × 10⁹ years |
| Iodine‑131 | ≈ 8 days |
- Identify the parent and daughter nuclei.
- Write the decay constant λ in terms of the half‑life: λ = ln 2 / t_{1/2}.
- Use the exponential decay formula to find remaining activity or mass after a given time.
Revision
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