The Law of Radioactive Decay
Random nuclei, predictable samples.
Lesson at a glanceShow the key points
- N = N₀e^(−λt) (46.17); A = λN.
- t₁/₂ = 0.693/λ (46.20); t_av = 1/λ (46.23).
- 1 Ci = 3.7 × 10¹⁰ Bq.
- Carbon dating uses ¹⁴C (5730 y).
Nobody can say when a particular nucleus will decay. Yet a large sample shrinks with clockwork regularity, halving in the same time over and over. The decay law turns that pattern into a clock for dating rocks and bones.
Chance, not destiny
Prepare many identical radioactive nuclei at the same moment, in identical conditions. They do not decay together: some go almost at once, some last a very long time. No law of physics predicts the moment for any one nucleus. This is a quantum effect; classical physics would say identical starting conditions give identical futures. Quantum mechanics gives only probabilities (an idea Einstein never fully accepted).
The decay law
If N nuclei are active, the number decaying in the next short time dt is proportional to N (more nuclei, more decays) and to dt (each has more chance in a longer interval):
The SI unit of activity is the becquerel (1 Bq = 1 decay per second). The older curie is 1 Ci = 3.7 × 10¹⁰ decays per second, named after Marie and Pierre Curie, who in 1902 isolated 0.19 g of radium chloride from uranium ore and shared the 1903 Nobel Prize with Henri Becquerel. Activity per unit mass is the specific activity.
Half-life and average life
The half-life t1/2 is the time for half the active nuclei, and therefore half the activity, to go:
Adding up how long every nucleus survives and dividing by N₀ gives the average life:
¹³¹I, used in thyroid treatment, has a half-life of 8.0 days. Find the activity of 1.0 µg of it.
³²P has a half-life of 14.3 days. Find (a) λ, (b) the average life, (c) the activity of 1.00 mg.
(a) A nuclide has a half-life of 6 h. What fraction of the activity is left after 24 h? (b) A sample has 8.0 × 10²⁰ active nuclei. How many remain after three half-lives?
A sample’s activity drops from 800 to 600 counts per second in 30 minutes. Find its half-life.
Radioactive clocks
Dating rocks
A rock contains three ²³⁸U atoms for every ²⁰⁶Pb atom. Assuming all the lead came from uranium (half-life 4.5 × 10⁹ y), how old is it?
Carbon dating
Equal masses of charcoal from two sites are burnt and their CO₂ is tested. Sample A gives 2400 counts per week from ¹⁴C, sample B 1500. How much older is B? (Half-life of ¹⁴C: 5730 y.)
Two ways to decay, and decay chains
If a nucleus can decay by two independent routes with constants λ₁ and λ₂, the chances simply add: λ = λ₁ + λ₂, so 1/t = 1/t₁ + 1/t₂ for the half-lives. For example, half-lives of 3 h and 6 h for the two routes give an overall half-life of 2 h.
If the daughter is also radioactive, it is produced at the rate λpNp and decays at λdNd. Its number stays constant when λpNp = λdNd, i.e. when the two activities are equal.
Uses and dangers
Gamma rays from sources such as cobalt-60 treat cancer; radioactive tracers follow substances through the body or through pipes; the ionization from a weak source lets static charge leak away from moving machinery in factories; carbon dating dates once-living material. Too much exposure damages living cells, so radiation is always used with shielding and limited doses.
- 1Decay is random for each nucleus but N = N₀e^(−λt) for many.
- 2Activity A = λN; units: Bq (1/s), Ci = 3.7 × 10¹⁰ Bq.
- 3t₁/₂ = 0.693/λ; t_av = 1/λ = 1.44 t₁/₂; N = N₀/2^(t/t₁/₂).
- 4Parallel decay routes: λ = λ₁ + λ₂. Steady daughter: λₚNₚ = λ_dN_d.
- 5Radioactive clocks date rocks (U → Pb) and organic remains (¹⁴C, 5730 y).
Check yourself
Keep exploring
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