Overview
What you’ll learn
- State that radioactive decay is random and spontaneous.
- Describe the detection of radiation with photographic film, cloud chambers and Geiger-Müller tubes.
- Identify common sources of background radiation and correct count rates for it.
- Recall the nature, range, penetration and ionising power of alpha, beta and gamma radiation.
- Use nuclide notation and write balanced nuclear equations for alpha and beta decay.
- Define half-life and calculate remaining mass, activity or count rate after whole half-lives.
- Describe uses of radioactivity (tracers, sterilisation, thickness gauges, dating) matched to the right radiation.
- State the hazards of ionising radiation and describe safe handling and storage.
In 30 seconds
- 1Decay is spontaneous and random: nothing you do — temperature, pressure, chemistry — changes when a given nucleus decays.
- 2Three decays: alpha (helium nucleus, stopped by paper), beta (fast electron, stopped by a few mm of aluminium), gamma (wave, reduced by thick lead).
- 3Ionising power runs the other way: alpha strongest, beta middle, gamma weakest — short, dense damage tracks for alpha.
- 4Nuclide notation A/Z X: A = nucleon number, Z = proton number. Alpha decay: A−4, Z−2. Beta decay: A unchanged, Z+1.
- 5A nuclear equation must balance: A and Z totals equal on both sides.
- 6Half-life = time for half the undecayed nuclei (or the corrected count rate) to halve. After n half-lives: divide by 2ⁿ.
- 7Always subtract the background count before analysing a source; add it back if asked for a total reading.
- 8Uses match properties: beta thickness gauge, gamma sterilisation and tracers (with short half-lives), alpha only inside the body or a smoke alarm.
Notes · 1 of 5
Detecting radiation and the background hum
Radiation leaves tracks: on film, in vapour, in a counting tube.
Radiation is invisible, but it betrays itself in three classic ways. A photographic film badge worn by a worker darkens in proportion to the dose received — the film is developed to read the exposure afterwards. A cloud chamber shows the radiation’s path directly: ionising particles seed visible vapour trails (thick, short tracks for alpha; thin, wispy ones for beta). A Geiger-Müller tube turns each burst of ionisation inside the tube into a click and a count on a ratemeter — the counting workhorse.
Even with no source on the bench, a detector keeps ticking: the background radiation — cosmic rays from space, radon gas from the ground, traces of uranium in rocks and building materials, tiny amounts of carbon-14 in all living things, and a slice from medical and industrial use. Before any experiment, measure the background rate and subtract it: a reading of 1200 counts per minute with a source, and 200 without, means the source itself delivers 1000 counts per minute. Skipping this step is the classic radioactivity-calculation error.
Notes · 2 of 5
Alpha, beta, gamma: the three decay products
Sort them by what stops them; rank them by damage done per millimetre.
An alpha particle is a helium nucleus: 2 protons + 2 neutrons, written ⁴₂He or α. It is heavy and doubly charged, so it rips through matter ionising fiercely — and is stopped within a few centimetres of air or by a sheet of paper. A beta particle is a fast electron (⁰₋₁β) thrown out when a neutron turns into a proton; it is light and fast, less ionising, and travels a metre or so in air, stopped by a few millimetres of aluminium. Gamma rays are high-energy electromagnetic waves with no mass or charge: weakly ionising but hugely penetrating, needing several centimetres of lead (or concrete) to cut the intensity down.
In electric and magnetic fields the charges betray themselves: alpha (positive) and beta (negative) deflect in opposite directions, alpha far less because it is vastly heavier; gamma passes straight through undeflected. Memory line for penetration: paper < aluminium < lead stops alpha < beta < gamma; for ionising power the ranking reverses. Half the exam questions on this topic are one of those two rankings in disguise.
Notes · 3 of 5
Nuclide notation and balanced nuclear equations
Bookkeeping where the books must balance: A and Z on both sides.
Nuclide notation: A/Z X, with A the nucleon number (protons + neutrons) and Z the proton number. Isotopes share Z but differ in A — same element, different mass (carbon-12 and carbon-14 are both carbon because both have Z = 6). A nuclear equation is checked like any other: total A balances and total Z balances across the arrow.
The two decays you must write from memory. Alpha decay: the nucleus spits out ⁴₂He, so A falls by 4 and Z falls by 2 — uranium-238 → thorium-234 + alpha. Beta decay: a neutron becomes a proton, an electron is ejected, so A is unchanged and Z rises by 1 — carbon-14 → nitrogen-14 + β⁻. Gamma emission changes neither A nor Z: the nucleus just sheds excess energy. Write the daughter, write the particle, check both totals — balancing marks are the cheapest marks in Paper 2.
Notes · 4 of 5
Half-life: randomness made countable
Halve, halve again — never quite zero.
You cannot say which nucleus decays next — that is the randomness. But the average is reliable: the half-life is the time for half the undecayed nuclei in a sample to decay, equivalently the time for the (background-corrected) activity to fall to half. After n half-lives, remaining fraction = 1/2ⁿ. A decay graph falls steeply and flattens towards zero, halving every half-life — read off the time for the rate to halve and you have measured T½.
Method for every calculation: (1) count the half-lives: n = time elapsed ÷ half-life; (2) divide by 2, n times; (3) if a count rate is given, subtract background first and add it back if the question asks for the meter reading. The value never reaches exactly zero — each halving leaves half of something — and cooling, heating or chemistry changes nothing about the rate.
Notes · 5 of 5
Uses, dangers and safe handling
Right isotope, right job; distance, shielding, time.
The isotope is chosen to fit the job. Medical tracers (technetium-99m): gamma escapes the body to a detector and the short half-life clears the dose quickly. Sterilising syringes and food: gamma penetrates the sealed packaging and kills bacteria. Thickness gauges for metal foil: beta is partly absorbed by the foil, so the count falling on the detector tracks the thickness. Carbon dating: the known half-life of carbon-14 (about 5700 years) compares living and dead material. Alpha is the worst penetrator, so it only works inside the body (targeted therapy) or close by — as in the smoke alarm’s ionisation chamber.
All ionising radiation can kill or damage living cells — radiation sickness at high dose, cancer risk from damaged DNA at lower doses. Safety follows from dose = intensity × time: handle with tongs (distance), work behind lead screens, wear film badges to log exposure, keep exposure time short, and store sources in lead-lined boxes. Strong sources are never handled bare, and alpha sources are harmless outside the body but dangerous inhaled or ingested — a fact examiners love.
Revise
Key terms
The words examiners expect you to use precisely.
- radioactive decay
- The spontaneous, random breakdown of an unstable nucleus, emitting alpha, beta or gamma radiation.
- random decay
- No measurement can predict when any single nucleus will decay; only averages follow the half-life.
- alpha particle
- A helium nucleus (2 protons + 2 neutrons), strongly ionising, stopped by paper or a few cm of air.
- beta particle
- A fast electron emitted when a neutron becomes a proton; moderately ionising, stopped by a few mm of aluminium.
- gamma ray
- A high-energy electromagnetic wave from the nucleus; weakly ionising but highly penetrating, reduced by thick lead.
- nuclide notation
- Writing a nucleus as A/Z X, with A the nucleon number and Z the proton number.
Show 6 more key termsShow fewer key terms
- isotope
- Nuclei of the same element (same proton number) with different numbers of neutrons.
- background radiation
- The constant low-level radiation from cosmic rays, radon, rocks and other natural and man-made sources; subtract it from readings.
- Geiger-Müller tube
- A detector that converts ionisation inside the tube into countable pulses.
- half-life
- The time for half the undecayed nuclei of an isotope to decay; the corrected activity falls by half each half-life.
- nuclear equation
- A balanced equation for a decay: nucleon numbers and proton numbers each total the same on both sides.
- ionising power
- The ability of radiation to remove electrons from atoms; alpha > beta > gamma, the reverse of penetration.
Revise
Common mistakes
Where students most often lose marks in this chapter — and what to do instead.
Mistake: Saying cooling a sample slows its decay.
Decay is nuclear and spontaneous; temperature, pressure and chemistry do not touch it.
Instead: Nothing done to the sample changes the half-life.
Mistake: Predicting exactly when a given nucleus will decay.
Decay is random per nucleus; only the average behaviour follows the half-life.
Instead: Half of a large sample decays per half-life, on average — individual nuclei are unpredictable.
Show 10 more mistakesShow fewer mistakes
Mistake: Defining half-life as the time for the sample to decay completely.
Each half-life only halves what is left, so the value never reaches zero.
Instead: Half-life: time for half the undecayed nuclei (or corrected activity) to decay.
Mistake: Analysing a source with the raw count rate, background included.
The background never decays, so the source looks too active and never "finishes".
Instead: Subtract the background first; add it back only if the question asks for the total reading.
Mistake: Writing alpha decay as A unchanged, Z − 2.
The alpha particle carries 4 nucleons away.
Instead: Alpha: A − 4, Z − 2. Beta: A unchanged, Z + 1. Gamma: A and Z unchanged.
Mistake: Emitting an electron in beta decay because the nucleus "contains electrons".
The nucleus holds protons and neutrons only.
Instead: A neutron turns into a proton, and the electron (beta particle) is created and ejected.
Mistake: Ranking gamma as most ionising because it is most penetrating.
The two rankings run opposite ways.
Instead: Ionising: alpha > beta > gamma. Penetrating: gamma > beta > alpha.
Mistake: Saying gamma rays are stopped completely by a thin lead sheet.
Gamma is only reduced (attenuated) by shielding, never perfectly stopped.
Instead: Thick lead reduces the intensity; distance reduces it further.
Mistake: Choosing alpha for a medical tracer swallowed or injected.
Alpha cannot escape the body and does dense damage inside it.
Instead: Tracers use gamma (escapes to the detector) with a short half-life.
Mistake: Saying a radioactive isotope with a short half-life stays dangerous for centuries.
Its activity collapses within a few half-lives.
Instead: Short half-life = intense but brief; long half-life = weak but persistent.
Mistake: Doubling the time when the mass falls to a quarter.
A quarter means two half-lives, and the half-life is fixed.
Instead: Count the halvings: ÷4 = 2 half-lives, ÷8 = 3 half-lives.
Mistake: Storing alpha sources in a paper envelope and calling it safe.
Paper stops alpha outside the body, but the source must also stay sealed and secure.
Instead: Sources live in sealed, labelled, lead-lined boxes; alpha is dangerous inhaled or ingested.
Check yourself
Quick quiz
28 questions with instant explanations. About 5 minutes.
Question 1 of 3
- Question 1: current question
- Question 2: not answered
- Question 3: not answered
State the random nature of decay.
The decay of a radioactive nucleus is described as random because
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Question paper
Chapter 12 Practice Paper
30 marks · 40 min · 4 pages
5 multiple-choice questions and structured questions with answer lines. Random nature of decay, detecting radiation and background radiation, alpha/beta/gamma properties and penetration, nuclide notation and balanced nuclear equations, half-life calculations and decay graphs, and the uses and hazards of radioactive materials with safety precautions.
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PROChapter 12 Practice Paper — mark scheme
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Model answers with a mark for each creditworthy point — for marking at home or in class.
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Questions
Frequently asked questions
What does Sec 4 Physics Chapter 12 cover?
It covers the O-Level Physics 6091 radioactivity topic: the random, spontaneous nature of decay; detection methods and background radiation; the nature, penetration and ionising power of alpha, beta and gamma; nuclide notation and balanced nuclear equations; half-life calculations; and the uses, hazards and safe handling of radioactive materials.
How do I do any half-life calculation quickly?
Three steps: divide the elapsed time by the half-life to count the half-lives; divide the starting value by 2 that many times (subtract the background count rate first if one is given); and add the background back if the question asks for the total meter reading.
Why is a short half-life safer for a medical tracer?
The tracer must be active long enough to image the body, then decay away quickly so the patient is not irradiated for weeks afterwards. Gamma is chosen because it escapes the body to the detector; alpha and beta would deposit their energy inside the patient.
Are these questions from past O-Level papers?
No. All notes, quizzes and papers on this page are original QuizQuip material written against the published syllabus, in Paper 1 and Paper 2 style. QuizQuip is not affiliated with MOE or SEAB and does not host school or examination papers.
When is this chapter usually tested in school?
Radioactivity appears in Sec 4 Prelim Paper 1 and Paper 2: half-life graphs, background-corrected count rates, nuclear equations and use-the-right-isotope questions all recur. Scope varies by school; check your school’s assessment outline.