Chapter revision
Revision summary
Key ideas, equations and common mistakes. Open any topic below for the full explanation.
Read the nucleus and atom
- Proton number Z
- Number of protons; identifies the element. A neutral atom also has Z electrons.
- Nucleon number A
- Protons plus neutrons. Neutrons = A - Z. A and Z are counts with no unit.
- Nuclide and isotope
- A nuclide has specified proton and neutron numbers. Isotopes have the same Z but different neutron numbers and therefore different A.
Put A at the upper left and Z at the lower left of the element symbol. A change in electrons makes an ion; it does not change the isotope. Equal A alone does not establish the same element.
Explain decay and emissions
An unstable nucleus loses energy by emitting radiation. Decay is random: an individual decay time cannot be predicted. It is spontaneous: no external trigger is needed. A large population can still have a predictable average pattern.
- Alpha: helium nucleus, two protons and two neutrons, charge +2. Typically dense ionisation and low penetration.
- Beta-minus: fast electron produced in a nuclear change, charge -1. Typically less dense ionisation and more penetration than alpha.
- Gamma: electromagnetic radiation from the nucleus, uncharged and highly penetrating. Thick shielding reduces transmission but need not eliminate it.
All three can ionise. Energy and absorber conditions affect their penetration. Radiation leaving a source is different from radioactive material spreading to a new location.
Track a nuclear change
- Alpha: daughter A decreases by 4 and Z by 2.
- Beta-minus: A is unchanged and Z increases by 1.
- Gamma: both A and Z stay unchanged while nuclear energy decreases.
Balance total upper nucleon numbers and lower charge numbers. The electron's lower -1 is a charge number, not a negative proton count; its upper 0 is not a claim of zero mass. Alpha then beta-minus takes A/Z from 214/84 to 210/83, leaving 127 neutrons.
Separate activity from detector rates
Net source rate = total rate - mean background rateUse matching rate units and comparable detector conditions.
Background comes from sources such as cosmic radiation, rocks, radon and radioactive materials in food and the body, with artificial contributions possible. Counts fluctuate; removing the study source does not normally make them zero.
Activity is the number of decays per second in the source. A detector records only some of the emissions, so its count rate is smaller than the activity. The example 300 counts in 2 min minus 100 counts in 5 min gives 150 - 20 = 130 counts/min from the source.
Choose suitable detector response and rate range. Keep geometry, shielding and settings fixed, record durations and estimate background. Longer counting reduces relative random variation for a steady rate, but can blur rapid decay. It cannot repair a wrong calibration.
Use repeated halving
Half-life t1/2 is the time for half the undecayed nuclei of one nuclide in a large sample to decay, or its activity to halve. It is measured in s, with other consistent time units possible.
After one, two and three half-lives, the remaining fractions are 1/2, 1/4 and 1/8. With half-life 6 h, a corrected count rate of 800 counts/min becomes 100 counts/min after 18 h. Daughter material remains; the whole sample does not disappear.
Use background-corrected rates for a decay curve. In the supplied model, 160 to 80 counts/min takes 4 min; 40 to 20 also takes 4 min. The total curve approaches 20 counts/min background, while the source curve approaches zero. Keep the single-nuclide, negligible-daughter and unchanged-detection conditions.
Connect uses and hazards to the radiation
- An internal gamma tracer emits towards a detector outside the body.
- A suitable beta gauge detects lower transmission through a thicker sheet under otherwise matched conditions.
- Gamma ionisation can damage tumour cells and healthy cells.
- Irradiation means radiation reaches a target. Contamination means radioactive material is present on or inside it.
- Internal alpha-emitting material can be hazardous despite low penetration. Activity alone does not give the energy absorbed by a person.
- Time, separation and suitable shielding affect external exposure; containment addresses spread of source material.
Choose half-life to retain useful activity for the task without unnecessarily long persistence. Also match penetration to the detector/target path and explain the useful or harmful ionisation. For the tracer comparison starting at 1600 counts/min, the 2 h half-life leaves 800 counts/min after 2 h; the 20 min half-life leaves only 25 counts/min.
Distinguish fission and fusion
Fission splits a heavy nucleus into smaller nuclei. Fusion joins light nuclei to form a heavier one. Suitable nuclear-fuel reactions in both processes release energy carried by their products and radiation; ordinary chemical burning does not change the nuclei in this way.
Back to atoms and nuclidesPractise exam questions
Write your answer first, then tick the mark points it makes.
Exam-style question
A sample contains 80 g of a radioactive isotope with a half-life of 6.0 days. Calculate the mass of this isotope that remains undecayed after 18 days. [2]
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Exam-style question
Define half-life. [1]
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Exam-style question
A factory uses a radioactive source and a detector to check the thickness of paper as it is made. Explain why a beta source is used, rather than an alpha or a gamma source. [3]
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Exam-style question
The background count rate in a laboratory is 20 counts/min. A graph of the measured count rate from a source against time shows 420 counts/min at 0 min, 220 counts/min at 8.0 min and 120 counts/min at 16 min. Use these readings to find the half-life of the source. [3]
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Exam-style question
Data-based question: Finding a leak with a radioactive tracer [10]
An engineer wants to find a leak in a water pipe buried 1.0 m underground. She adds a small amount of a radioactive isotope to the water. A day later she walks along the ground above the pipe with a detector and records the count rate. The background count rate is 25 counts per minute.
| isotope | radiation emitted | half-life |
|---|---|---|
| A | alpha | 6 hours |
| B | beta | 15 hours |
| C | gamma | 6 hours |
| D | gamma | 30 years |
| distance along pipe / m | count rate / counts per min |
|---|---|
| 0 | 31 |
| 10 | 29 |
| 20 | 30 |
| 30 | 186 |
| 40 | 33 |
| 50 | 28 |
- (a) Choose the most suitable isotope from Table 1. Explain your choice using both the radiation and the half-life. [3]
- (b) Calculate the corrected count rate at 30 m. [1]
- (c) State where the leak is and explain why the count rate is high there. [2]
- (d) State one assumption you made in (c). [1]
- (e) A technician says the readings at the other positions show that the isotope is present there too. Evaluate this claim. [3]
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Quick recall
Three neutral atoms have these nucleon/proton numbers: P has A = 23, Z = 11; Q has A = 24, Z = 11; R has A = 24, Z = 12. Which pair consists of isotopes of the same element?
Review a topic
- Atoms, nuclei and isotopes
- Radioactive decay and radiation
- Nuclear decay equations
- Background radiation and activity
- Half-life from numbers and graphs
- Uses and hazards
- Fission and fusion