Nuclear Decay
Modern Physics — Nuclear Decay
Nuclear Decay
Radioactive Decay & Half-Life
Core Concept
Unstable nuclei decay spontaneously by emitting radiation. The process is governed by a single principle: the probability of decay in any small time interval is constant (equal to , independent of the nucleus's age or environment). This is the decay constant .
Applying this to a large population of nuclei gives the exponential law. The three main decay modes are:
- Alpha () decay: nucleus emits a helium-4 nucleus; large mass and charge change.
- Beta () decay: a neutron converts to a proton (or vice versa) emitting an electron/positron and a neutrino.
- Gamma () decay: excited nucleus releases a high-energy photon; no change in or .
Activity measures the number of decays per second (unit: Becquerel, ).
Key Formula
Decay law:
Half-life (time for half the nuclei to decay):
After half-lives: .
Worked Example
Carbon-14 has . A wood sample shows activity of a living tree's activity. How old is the sample?
The sample is approximately 11,460 years old — this is the principle behind radiocarbon dating.
Real-World Connection
Radiocarbon dating (C-14, ) dates organic artefacts up to ~50,000 years. Uranium-lead dating (U-238, ) dates rocks and meteorites — including Earth itself. Medical PET scanners use fluorine-18 (), short enough to decay away after the scan. Smoke detectors contain Americium-241 (), whose alpha emission ionises air to complete a circuit that smoke interrupts.
Quick Check
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A radioactive isotope has and initial activity . What is the activity after 24 days?
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Why does a decay curve look smooth for a large sample but jagged and stepwise for only a few hundred atoms?
Key Takeaways (TL;DR)
- Core Concept
- Key Formula
- Worked Example
- Real-World Connection
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