Track Isotopes
Isotope questions are notation questions first. Compare Z to decide whether the element is the same, then compare A or A-Z to see whether the neutron number differs.
Sort each pair by isotope relationship.
SortDefine isotope and use nuclear notation to compare two nuclides.
Using same mass number as the isotope condition.
Define isotope and use nuclear notation to compare two nuclides.
ChooseTrack Binding energy and mass defect
Mass defect is not missing matter; it is mass-equivalent energy. A bound nucleus has lower mass because energy was released when it formed. To break it apart, that same binding energy must be supplied.
Assemble the mass-defect to binding-energy calculation.
FormulaCalculate binding energy from a mass defect.
Using the bound nucleus mass alone instead of the mass difference.
Calculate binding energy from a mass defect.
ChooseTrack Binding energy curve
The curve is a stability map. Energy is released when a nuclear reaction moves products upward on the binding-energy-per-nucleon curve.
Interpret energy release from the binding-energy curve.
GraphAverage binding energy per nucleon is plotted against nucleon number. The curve rises steeply for light nuclei, peaks near iron, then falls slowly for heavy nuclei.
Use the binding-energy-per-nucleon graph to explain why fission and fusion can release energy.
Confusing total binding energy with average binding energy per nucleon.
Use the binding-energy-per-nucleon graph to explain why fission and fusion can release energy.
ChooseMass-energy equivalence
Mass-energy equivalence is the bridge from nuclear masses to released energy. The direction matters: if final mass is lower than initial mass, energy is released.
Assemble E=mc² for nuclear mass changes.
FormulaDefine mass-energy equivalence and apply it to a nuclear mass change.
Using E=mc² with the whole nucleus mass instead of the mass change.
Define mass-energy equivalence and apply it to a nuclear mass change.
ChooseTrack Strong nuclear force
The nucleus is a force-balance story. The electric force pushes protons apart, but the strong nuclear force binds nearby nucleons. Its short range helps explain why large nuclei need more neutrons.
Sort each nuclear-force statement.
SortExplain why the strong nuclear force is needed for nuclear stability.
Only saying nuclei are stable because protons and neutrons touch.
Explain why the strong nuclear force is needed for nuclear stability.
ChooseTrack Random radioactive decay
Random does not mean patternless for a large sample. It means individual nuclei cannot be timed, while the sample follows predictable half-life or exponential behaviour.
Sort claims about random decay.
SortDescribe radioactive decay as a random and spontaneous process.
Saying random means half-life cannot be defined.
Describe radioactive decay as a random and spontaneous process.
ChooseTrack Decay nuclear changes
Decay equations are conservation puzzles. Write A and Z totals on both sides and choose the missing particle or daughter nucleus that balances both.
Sort each nuclear change by decay type.
SortState the changes in A and Z for alpha, beta-minus, beta-plus, and gamma decay.
Changing A during beta decay.
State the changes in A and Z for alpha, beta-minus, beta-plus, and gamma decay.
ChooseTrack Decay equations
PracticeComplete decay equations by balancing A first and Z second. If it is beta decay, include the correct neutrino partner when the syllabus context asks for it.
Match each emitted particle to its equation role.
MatchComplete a nuclear decay equation.
Balancing mass number but not proton number.
Complete a nuclear decay equation.
ChooseTrack Neutrinos and antineutrinos
The beta particle alone is not the whole beta-decay story. Include the neutrino partner and know which decay uses which one.
Sort beta-decay products and ideas.
SortDescribe beta-minus and beta-plus decay, including neutrinos.
Omitting neutrino or antineutrino from beta decay.
Describe beta-minus and beta-plus decay, including neutrinos.
ChooseRadiation penetration and ionization
Radiation risk depends on context. Alpha is dangerous inside the body despite low penetration. Gamma is hard to shield despite lower ionisation per interaction.
Sort radiation properties by type.
SortCompare the penetration and ionising ability of alpha, beta, and gamma radiation.
Confusing penetrating power with ionising ability.
Compare the penetration and ionising ability of alpha, beta, and gamma radiation.
ChooseTrack Activity, count rate and half-life
Activity belongs to the sample; count rate belongs to the detector. Half-life can be read from corrected count rate because count rate is proportional to activity under fixed geometry.
Match each decay measurement term to its meaning.
MatchDefine activity, count rate, and half-life.
Equating raw detector count rate directly with activity.
Define activity, count rate, and half-life.
ChooseTrack Half-life changes
Half-life is repeated halving, not repeated subtraction. On a graph, choose two points where activity halves and read the time difference.
Use the decay curve to apply half-life.
GraphA corrected count-rate curve starts at 800 counts per second and halves every 5 minutes.
Determine half-life from a decay curve and predict activity after whole half-lives.
Treating decay as a straight-line decrease.
Determine half-life from a decay curve and predict activity after whole half-lives.
ChooseBackground radiation
Background correction is not optional in count-rate experiments. If the raw count has a constant background added, it will not halve correctly even when the source activity does.
Sort background radiation claims.
SortExplain how background radiation affects count-rate measurements.
Using raw count rate directly for half-life.
Explain how background radiation affects count-rate measurements.
ChooseRetrieve the Core E.3 Radioactive decay Model
ReviewThis retrieval card covers the SL spine of E.3: identify the nuclide, calculate nuclear energy, choose the decay type, and interpret measurements correctly.
Match each core E.3 cue to the correct model statement.
MatchSummarize the core E.3 radioactive-decay model.
Listing radiation names without nuclear changes or measurement definitions.
Summarize the core E.3 radioactive-decay model.
Choose