Radioactivity, decay and half-life: worked solutions
AQA A-level radioactivity worked solutions: half-life, decay and log graphs, activity, absorption, Required Practical 12, dating and radioisotope power, with examiner guidance.
Constants and assumptions: NA = 6.02 × 10²³ mol⁻¹; 1 year = 365 days = 3.1536 × 10⁷ s. Bq means decays per second; s⁻¹ on detector data means registered counts per second. Use a single parent isotope with stable daughters unless the question states a mixture; detection geometry/efficiency stay fixed unless stated otherwise. Quantities inside logarithms are divided by the reference unit shown.
Attempt each question before opening the hints. Show equations, substitutions, units and the reason for your method. The mark checklists below are PhysicsUK's own schemes.
Lessons from the examiner reports
These reports identify skills worth practising. The questions below are original PhysicsUK examples, with our own mark schemes.
Link radiation choice to the job: The report flags radiation choices justified with an unrelated property. Link penetration to what must be reached or partly absorbed. Our foil task uses supplied transmission data; it is not the original sterilisation question. AQA 7408/2, June 2018 — Q05.1; report p. 5
Test all rows and name a real mechanism: Use corrected rate × distance squared across all rows. The report flags squaring the rate and vague human-error claims. A deviation needs a concrete explanation, such as active-distance geometry or a detector limitation, rather than background subtraction repeated on corrected data. AQA 7408/2, June 2018 — Q05.3–05.4; report p. 5
Use equal halving intervals when they are visible: The report describes unnecessary exponential fitting when a clear halving interval could be read. Our detector curve adds a background floor: identify halvings of the source-only contribution before calculating. AQA 7408/2, June 2018 — Q06.1; report pp. 5–6
Activity in Bq requires a seconds-based decay constant: The report identifies powers-of-ten, precision and time-unit errors when converting a parent mass to activity. Convert mass consistently, count nuclei correctly, and convert a years-based decay constant before reporting Bq. AQA 7408/2, June 2018 — Q06.5–06.6; report p. 6
A numerical conclusion needs a numerical comparison: The report distinguishes proposing inverse-square calculations from justifying the conclusion. Retain precision after background correction, compare products or predictions quantitatively, and judge the difference in the context of measurement uncertainty. AQA 7408/3A, November 2021 — Q01.2–01.3; report pp. 3 and 6
Explain what the measurement and precaution do: The report notes weaknesses in parallax-reduction methods and assumptions that gamma is emitted only from a source opening. Specify how the ruler reading relates to the active distance, and connect handling precautions to distance or exposure time. AQA 7408/3A, November 2021 — Q01.1 and 01.4; report p. 6
Inverse square needs the correct log–log slope: The report identifies weak logarithmic power-law analysis. The checked marking requires a fitted log-rate against log-distance gradient near −2; a straight line or merely negative gradient does not establish inverse square. AQA 7408/3A, November 2021 — Q01.6; report p. 6; checked marking p. 10
Read the log-axis labels and use a fitted line: The report flags using isolated points instead of a fit and treating positions on a logarithmic scale as numerical logarithms. Read the axis definition, use fitted-line data and account for log base. Our dice task supplies an exact discrete law. AQA 7408/2, June 2024 — Q07.1–07.2; report p. 8
Include the daughter in the original parent ledger: The report identifies dating answers that omitted decayed parents now present as daughter nuclei. Under the stated no-initial-daughter, closed-system assumptions, original parent number is present parent plus radiogenic daughter. AQA 7408/2, June 2024 — Q32; report p. 9; checked marking p. 26
Tie exposure controls to the stated source: The report requires precautions suited to the source and explicit reasoning about risk and benefit. In an application answer connect the proposed distance, shielding or exposure-time change to the situation; activity alone is not a dose. AQA 7408/2, June 2024 — Q07.3–07.4; report pp. 8–9
Join activity, energy per decay, efficiency and time: The report flags confusing nuclear population with nucleon number and converting the entire source mass to energy. Build the power budget from activity × supplied energy per decay × efficiency, then use a consistent decay time unit. AQA 7408/2, June 2025 — Q03.1–03.2; report p. 6
Question 1 · Exam-style background and uncertainty · 6 marks
Unequal counting times: what did the detector measure?
Specification: 3.8.1.2, 3.1.2
A fixed detector records 420 counts in 120 s with a long-lived source present. Background alone gives 480 counts in 600 s. Treat the two counts as independent. For this question you are supplied with the approximate standard uncertainty in a corrected rate: σr = √(Cg/tg² + Cb/tb²). Subscripts g and b refer to the source-present and background measurements.
Calculate the background-corrected count rate. [2]
Calculate its standard uncertainty and quote a suitably rounded rate with uncertainty. [2]
Explain why this rate is not automatically the source activity in Bq. Suggest a measurement change that reduces random uncertainty. [2]
Small hint
The counting intervals differ. Convert both totals to counts per second before subtracting.
Method hint
Use rg = 420/120 and rb = 480/600. Substitute the original recorded counts and times into the supplied uncertainty formula, rather than putting the corrected count into it.
Complete worked solution and marks
Answer: Corrected rate = (2.70 ± 0.17) s⁻¹, using the supplied standard-uncertainty model. Activity cannot be inferred without detection information; longer counting reduces relative random uncertainty.
σr = √(420/120² + 480/600²) = 0.1746… s⁻¹ ≈ 0.17 s⁻¹. Report (2.70 ± 0.17) s⁻¹ with the value and uncertainty at matching decimal precision.
Count rate describes events registered by the detector. Activity is the mean number of nuclear decays per second in the source. Geometry, absorption, detector efficiency and the number/type of emissions per decay affect the registered fraction; they have not been specified.
Count for longer, or combine repeated equal-time measurements into a longer total, while keeping the geometry and source activity effectively constant. Larger total counts reduce relative fluctuations. A longer background measurement helps its contribution, although here the source-present term dominates.
Check: The corrected rate is less than the gross rate. The relative standard uncertainty is about 6.5%; this is a statistical estimate, not a guaranteed bound on the result.
Mark checklist · 6 marks
1 mark — Calculates both rates using their own counting intervals.
1 mark — Subtracts background to obtain 2.70 s⁻¹.
1 mark — Uses the supplied independent-count uncertainty expression with original counts.
1 mark — Obtains about 0.17 s⁻¹ and quotes matching precision, e.g. (2.70 ± 0.17) s⁻¹.
1 mark — Distinguishes source decays/activity from registered counts, with a relevant detection factor.
1 mark — Proposes longer total counting/repeated counting under fixed conditions to reduce relative random uncertainty.
Common mistake: Subtracting 480 from 420 would combine different durations. A larger background count can still correspond to a smaller background rate. Do not relabel a detector rate as activity without a detection model.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
Repeat both measurements for four times as long with unchanged mean rates. What happens to the corrected rate and its standard uncertainty?
Check the transfer answer
The expected corrected rate stays 2.70 s⁻¹. Each expected count increases fourfold and each time does too, so both variance terms divide by four: σr halves to 0.0873 s⁻¹. An individual repeat can still fluctuate.
Question 2 · Exam-style moles, nuclei and seconds · 6 marks
From a tiny parent-isotope mass to activity
Specification: 3.8.1.3
An isolated sample initially contains 2.40 μg of parent isotope P. Its molar mass is 90.0 g mol⁻¹ and its half-life is 30.0 years. Each parent ultimately produces a stable daughter retained in the sealed sample. Use NA = 6.02 × 10²³ mol⁻¹ and 1 year = 3.1536 × 10⁷ s. Ignore the tiny total mass change associated with released energy.
Calculate the initial number of parent nuclei and the decay constant in s⁻¹. [2]
Calculate the initial activity, with an appropriate unit. [2]
Find the mass of undecayed P after 90.0 years. Explain why this is not the total sample mass remaining. [2]
Small hint
Match the mass unit to the molar-mass unit. A becquerel means one decay per second, so λ must be in s⁻¹.
Method hint
Find n = m/M, N = nNA and λ = ln2/T½. Then use A = λN. Ninety years is three half-lives for the parent.
Complete worked solution and marks
Answer: N0 = 1.61 × 10¹⁶; λ = 7.33 × 10⁻¹⁰ s⁻¹; A0 = 1.18 × 10⁷ Bq (11.8 MBq). Undecayed P after 90 years = 0.300 μg; retained daughters remain part of the sample.
m = 2.40 × 10⁻⁶ g; n = (2.40 × 10⁻⁶)/90.0 = 2.67 × 10⁻⁸ mol; N0 = nNA = 1.61 × 10¹⁶ nuclei.
A0 = λN0 = 1.18 × 10⁷ Bq = 11.8 MBq. Retain unrounded N0 and λ until the final result.
mP = 2.40 × (½)³ = 0.300 μg after 90.0 years.
This last value counts only undecayed parent P. Most of the original nuclei have become daughter nuclei rather than disappeared from the sample. With retained products and the stated negligible mass-loss approximation, the total sample mass remains approximately its initial value.
Worked-answer figure. Match mass units; 2.40 × 10⁻⁶ g /; 90.0 g mol⁻¹; 2.67 × 10⁻⁸ mol; Count nuclei; Multiply by NA; N₀ = 1.61 × 10¹⁶; Use seconds; λ = 7.33 × 10⁻¹⁰ s⁻¹; A₀ = λN₀; 11.8 MBq. After 90 years: parent = 0.300 μg Daughter nuclei remain in the sample. Open the larger diagram
Check: After three half-lives both parent mass and parent activity are one eighth of their initial values. Dividing A0 by N0 recovers λ, independently checking the conversion.
Mark checklist · 6 marks
1 mark — Uses m/M and NA consistently to obtain about 1.61 × 10¹⁶ nuclei.
1 mark — Converts the half-life to seconds and obtains λ ≈ 7.33 × 10⁻¹⁰ s⁻¹.
1 mark — Uses A = λN with the number of parent nuclei, not the nucleon number.
1 mark — Obtains A0 ≈ 1.18 × 10⁷ with unit Bq.
1 mark — Uses three half-lives to obtain 0.300 μg of undecayed parent.
1 mark — Explains that retained daughter nuclei remain in the sample; parent mass is not total sample mass.
Common mistake: N in A = λN is the number of undecayed nuclei, not the isotope’s mass number. The parent mass decays exponentially; the mass of the entire retained sample does not halve.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
A different isotope has the same initial parent mass and molar mass but a half-life of 60.0 years. Compare its initial activity and its parent mass after 90.0 years.
Check the transfer answer
It initially has the same N0 but half the decay constant, so its initial activity is 5.88 MBq. After 1.5 half-lives its parent mass is 2.40 × 2−1.5 = 0.849 μg, greater than for P.
Question 3 · Exam-style half-life graph and threshold · 7 marks
Read a decay curve above a background floor
Specification: 3.8.1.2, 3.8.1.3
The figure shows a smooth expected gross detector count rate for one short-lived isotope in fixed geometry. Background is a constant 12.0 s⁻¹. For accessibility, points on the gross curve are (0 min, 172 s⁻¹), (3 min, 92 s⁻¹), (6 min, 52 s⁻¹) and (9 min, 32 s⁻¹). The instrument estimates rates over intervals short compared with the half-life.
Define half-life, then determine it from these data, showing the background correction. [3]
Calculate the decay constant in s⁻¹. [2]
Determine when the gross rate reaches 22.0 s⁻¹. [2]
Original question figure; numerical data and assumptions are supplied in the text. Open the larger diagramSmall hint
The gross curve approaches 12 s⁻¹, not zero. Halve the source-only contribution, rather than the whole graph height.
Method hint
Subtract 12 from each rate: 160, 80, 40 and 20 s⁻¹. Use T½ = ln2/λ and rnet/rnet,0 = 2^(−t/T½). The target gross rate must also be corrected.
Complete worked solution and marks
Answer: T½ = 3.00 min = 180 s; λ = 3.85 × 10⁻³ s⁻¹. A gross rate of 22.0 s⁻¹ is reached after 12.0 min.
Half-life is the time for the number of undecayed nuclei, or the activity of a single parent isotope, to fall to half its initial value. With fixed detection conditions its corrected count rate has the same half-life.
Source-only rates: 172 − 12 = 160; 92 − 12 = 80; 52 − 12 = 40; 32 − 12 = 20 s⁻¹. Each halves over 3.00 min.
λ = ln2/180 = 3.85 × 10⁻³ s⁻¹. Using 3 directly would give min⁻¹, not s⁻¹.
Target rnet = 22.0 − 12.0 = 10.0 s⁻¹; 10/160 = 1/16 = (½)⁴; t = 4T½ = 12.0 min.
The late-time gross rate tends towards the background floor. A target below that floor cannot be reached by this expected gross curve; random measured rates can still fluctuate.
Worked-answer figure. Gross rate is 12 + 160 times 2 raised to minus t/3, with t in minutes. Points are 172 at zero, 92 at 3, 52 at 6 and 32 at 9 minutes. Background floor is 12 counts per second. The net rate halves every 3 minutes. Gross 22 is reached at 12 minutes. Open the larger diagram
Check: At 12 min the source contribution is 10 s⁻¹ and adding 12 s⁻¹ background gives the stated 22 s⁻¹. Successive halving intervals are equal despite progressively smaller drops.
Mark checklist · 7 marks
1 mark — Defines half-life using the undecayed population or activity falling by half.
1 mark — Corrects gross rates by subtracting 12.0 s⁻¹.
1 mark — Finds a consistent half-life of 3.00 min from at least one halving interval.
1 mark — Converts the half-life to 180 s.
1 mark — Uses λ = ln2/T½ to obtain 3.85 × 10⁻³ s⁻¹.
1 mark — Corrects the target to 10.0 s⁻¹ and recognises four halvings.
1 mark — Obtains t = 12.0 min.
Common mistake: Half of the gross initial rate is 86 s⁻¹. That includes the unchanged background and would overestimate the half-life. Halve the rate measured above the background floor.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
A second detector setting doubles only the background reading to 24.0 s⁻¹; its source response is unchanged. What gross rate and half-life would it show at 6.00 min?
Check the transfer answer
The source contribution at 6 min is still 40.0 s⁻¹, so gross rate becomes 64.0 s⁻¹. Correcting the new background still gives T½ = 3.00 min. Background is an additive measurement contribution, not a change to nuclear decay.
Question 4 · Exam-style data processing and linearisation · 8 marks
A logarithmic decay fit: gradient, intercept and log base
Specification: 3.8.1.3
Background has already been subtracted from mean detector rates in fixed geometry. A fitted straight line on a graph of y = ln[r/(1 s⁻¹)] against t in seconds passes through (40 s, 4.69) and (360 s, 3.89). Use those two points on the fitted line, rather than individual fluctuating data points. The table shows the original rounded data.
Explain why background must be subtracted before taking logs. Rearrange the decay equation to show what the line’s gradient represents. [3]
Calculate the decay constant and half-life. [2]
Use the intercept to estimate the initial corrected count rate. [1]
If y had instead been log₁₀[r/(1 s⁻¹)], calculate the expected gradient for this same source. [2]
Original corrected mean rates; the fit is supplied
t / s
r / s⁻¹
0
120
120
90
240
65
360
50
480
36
Original question figure; numerical data and assumptions are supplied in the text. Open the larger diagramSmall hint
A constant background becomes an added term inside a log if it is left in. Also, ln and log₁₀ have different numerical gradients.
Method hint
ln(r/rref) = ln(r0/rref) − λt. Find gradient from Δy/Δt, then extrapolate to t = 0. For base 10, divide the natural-log gradient by ln10.
The exponential law applies to the source-only rate. A gross rate r = rsource + rbackground is not a single exponential tending to zero; taking its logarithm can produce a curved graph and a biased decay constant.
r = r0e−λt ⇒ ln[r/(1 s⁻¹)] = ln[r0/(1 s⁻¹)] − λt. The y-axis is dimensionless and gradient = −λ when t is in seconds.
A logarithmically spaced axis labelled with actual rates is different from an axis labelled with the numerical logarithms of the rates. Read its labels before using a gradient. The given task explicitly plots natural-log numbers.
Worked-answer figure. Scatter points correspond to the rates in the table. Fitted line y = 4.79 − 0.00250t passes through the two gold line points (40,4.69) and (360,3.89). A triangle shows vertical change −0.80 and horizontal change 320 s. Half-life is 277 s and initial rate is about 120 counts per second. Open the larger diagram
Check: A 320 s interval reduces the fitted rate by e⁻⁰·⁸ = 0.449; it must therefore be somewhat longer than one half-life. Using base 10 or e gives the same physical λ once converted.
Mark checklist · 8 marks
1 mark — Explains that unchanged additive background spoils a single-exponential source-only log fit.
1 mark — Takes natural logs of the source decay law correctly.
1 mark — Identifies gradient = −λ with time in seconds.
1 mark — Uses the two fitted-line coordinates to find λ = 0.00250 s⁻¹.
1 mark — Finds T½ ≈ 277 s.
1 mark — Finds intercept 4.79 and exponentiates it to estimate r0 ≈ 120 s⁻¹.
1 mark — Derives the base-10 gradient as −λ/ln10.
1 mark — Obtains −1.09 × 10⁻³ s⁻¹, with the correct sign and unit.
Common mistake: The negative slope is not a negative decay constant. On a log₁₀ plot λ is not simply minus the gradient. The intercept is a logarithm of a rate, not the rate itself.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
Keeping geometry and source unchanged, double a detector’s efficiency at all times, staying below saturation. What happens to the natural-log line?
Check the transfer answer
Corrected rates double. The line shifts vertically upwards by ln2 = 0.693; its intercept becomes 5.483. Gradient, λ and half-life are unchanged. The new r0 is about 241 s⁻¹ using the fitted intercept. This does not double the source activity.
Question 5 · Exam-style practical method with reasons · 7 marks
Required Practical 12: design a convincing test
Specification: 3.8.1.2, 8.2.RP12, 3.1.2
In a supervised school investigation, a small sealed gamma source has a half-life much longer than the experiment. A detector and counter can be placed at several separations. The diagram is a schematic starting arrangement; the active source and detector positions are known. Plan a test of rnet ∝ 1/d². Assume absorption in air is negligible over the chosen range and use separations large compared with the source and detector dimensions.
Describe how to arrange the apparatus and measure the relevant distance. [2]
Explain how you will obtain reliable background-corrected rates at several distances. [2]
State a graph to plot and explain how it tests the inverse-square relationship, including a limit on the conclusion. [2]
Give a suitable handling precaution and explain how it reduces exposure. [1]
Original question figure; numerical data and assumptions are supplied in the text. Open the larger diagramSmall hint
The relevant separation is between the active source and detecting region. A ruler next to the cases does not automatically measure that distance.
Method hint
Hold orientation/alignment fixed, vary d, record counts with measured times, subtract a separately measured background rate, then fit rnet against 1/d². The inverse-square model predicts a straight line through the origin.
Complete worked solution and marks
Answer: Use fixed alignment and known active positions, long background and repeated timed source measurements, then fit corrected rate against 1/d². A straight line through the origin within uncertainty supports the model over the tested range. Long tongs increase handling distance.
Clamp the source and detector in alignment. Keep their relative orientation and detector settings fixed. Change only their separation, using positions well beyond their physical size so the point-source/small-detector approximation is reasonable.
Use the known active positions, not arbitrary case edges. Read their ruler positions and subtract, using a set-square to project each position to the ruler and viewing square-on to limit parallax. Record any known case-to-active-position offsets.
Measure background with the source stored well away for a long timed interval. At each of at least five well-spaced distances, record repeated counts and their times. Combine equal-time repeats into a mean or total rate; use rg = total count / total time, then subtract rb. Longer counting is particularly useful where the net rate is small.
Plot rnet / s⁻¹ against 1/d² / m⁻². rnet = k(1/d²), so the expected fit is a straight line through the origin, with gradient k in m² s⁻¹.
Use a fitted line and measurement uncertainties. An intercept consistent with zero and a linear trend support the relationship over the measured range. A line that is merely straight with a substantial intercept is insufficient. Check that the detector is not saturating and that distance uncertainty is not dominant at the closest point.
Use long tongs for necessary source handling, following the supervised procedure. They increase distance from the source, reducing received intensity in the point-source model. Keep handling time short and return the source to its designated shielding when it is not needed. Adjust the detector rather than repeatedly approaching the source.
Check: For this geometric model doubling d quarters the source-only rate. It does not quarter the unchanged background. A half-life much longer than the measurement period keeps decay from confounding the distance change.
Mark checklist · 7 marks
1 mark — Keeps alignment, orientation and detector conditions fixed while varying separation in a suitable geometric range.
1 mark — Measures active-source to active-detector distance, accounting for offsets and reducing parallax.
1 mark — Measures a timed background with the source away and subtracts its rate, not arbitrary counts.
1 mark — Records timed source counts at multiple distances with repeats/longer counting to reduce random fluctuations.
1 mark — Plots corrected rate against 1/d² and tests for a fitted line through the origin.
1 mark — Judges agreement within uncertainty over the tested range and identifies a concrete limitation, e.g. dead time or finite geometry.
1 mark — Gives a suitable precaution with its exposure-reducing mechanism, e.g. long tongs increasing distance.
Common mistake: “A straight line proves inverse square” omits the origin for rnet against 1/d². “Be careful” or “avoid human error” gives neither a procedure nor a reason. Gamma radiation can reach the operator from directions other than the source holder’s opening.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
You use a source whose activity falls noticeably during the experiment and always measure increasing distances in order. What bias can this introduce, and how could you check it?
Check the transfer answer
Later, more distant readings fall because of both distance and decay, potentially exaggerating the distance dependence. Revisit a fixed reference distance between readings, or use the independently known decay constant and elapsed times to correct rates to a common time. A longer-lived source avoids this confounding effect.
Question 6 · Exam-style background, products and log–log gradient · 8 marks
Inverse-square data: test the whole table
Specification: 3.8.1.2, 8.2.RP12
A long-lived point-like gamma source is measured at fixed detector orientation. Each source-present count lasts 120 s. Background alone gives 1800 counts in 1500 s. Distances d are between the active source and detector. For this comparison, use a conservative relative uncertainty of 10% for each corrected rate. Take distance uncertainty as negligible here. The table contains rounded measured counts.
Calculate the background rate and all four corrected rates. [2]
Test the inverse-square model using all four rows and give a quantitative conclusion. [2]
Derive the expected gradient of ln[rnet/(1 s⁻¹)] against ln[d/(1 m)]. Calculate a two-point gradient using the 0.200 m and 0.400 m readings. [2]
Explain why using gross rates could give a misleading test. [1]
Using k = 0.480 m² s⁻¹, predict the gross rate at d = 0.600 m. [1]
Source-present counts in 120 s
d / m
Gross count
0.200
1584
0.300
784
0.400
504
0.500
374
Small hint
Compute rnet × d², not rnet² × d. Background is independent of source distance.
Method hint
rb = 1800/1500. For each row find C/120 − rb. Compare k = rnet d² across all rows. Taking logs of rnet = k/d² gives slope −2 when both axes use the same log base.
Complete worked solution and marks
Answer: rb = 1.20 s⁻¹; corrected rates = 12.0, 5.33, 3.00 and 1.917 s⁻¹. k = 0.480, 0.480, 0.480 and 0.479 m² s⁻¹, consistent within the stated uncertainty. Log–log gradient = −2.00. Gross rate at 0.600 m = 2.53 s⁻¹.
k = rnet d² gives 0.480, 0.480, 0.480 and 0.47917… m² s⁻¹. The last differs from 0.480 by about 0.17%, far below the supplied conservative 10% rate uncertainty. All four rows support the inverse-square model over this distance range.
ln(rnet/rref) = ln[k/(rref dref²)] − 2ln(d/dref), where rref = 1 s⁻¹ and dref = 1 m. The expected log–log gradient is −2.
Gross rate equals k/d² + rb. Its product with d² is k + rb d², which increases with distance even when the source obeys the model. Background must be removed before the product or logarithmic test.
At 0.600 m, rnet = 0.480/0.600² = 1.333… s⁻¹; rgross = 1.333… + 1.20 = 2.53 s⁻¹.
Worked-answer figure. Plot of corrected rate against reciprocal distance squared. Original count data are transformed using count/120 − 1.20. Fit through origin has gradient 0.480 square metres per second; all four points agree within the given uncertainty. Open the larger diagramWorked-answer figure. Natural log of corrected rate against natural log of distance. A line with slope −2 describes the data. Gradient triangle uses distance 0.200 to 0.400 m and rate 12 to 3 counts per second. Both logarithmic variables are dimensionless. Open the larger diagram
Check: The 0.400 m reading has one quarter of the 0.200 m corrected rate. The corrected-rate versus 1/d² line and the log–log line test the same model; their gradients have different meanings and units.
Mark checklist · 8 marks
1 mark — Finds rb = 1.20 s⁻¹ and applies C/120 − rb.
1 mark — Obtains all four corrected rates, retaining sufficient precision.
1 mark — Calculates rnet d² for all four rows with appropriate units.
1 mark — Compares the approximately 0.17% spread with the supplied 10% uncertainty and concludes support over the tested range.
1 mark — Derives a log–log line with expected gradient −2.
1 mark — Calculates −2.00 from the two stated rate/distance ratios.
1 mark — Explains the unchanged additive background changes gross-rate products/logs.
1 mark — Predicts gross rate ≈ 2.53 s⁻¹ at 0.600 m.
Common mistake: A straight line on log–log axes shows a power law, but inverse square specifically needs gradient −2. Use all the table entries and quantify differences rather than merely saying the products look similar.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
Predict the gross rate at 1.00 m from k = 0.480 m² s⁻¹. Is it one quarter of the gross rate at 0.500 m?
Check the transfer answer
rnet = 0.480 s⁻¹ and rgross = 1.68 s⁻¹. It is approximately one quarter of the net rate at 0.500 m, allowing for rounded counts. It is not one quarter of the gross rate, because the 1.20 s⁻¹ background stays unchanged.
Question 7 · Exam-style explain deviations using mechanisms · 7 marks
A distance offset and a detector blind interval
Specification: 3.8.1.2, 3.8.1.3, 8.2.RP12
A detector’s active region is 0.030 m behind its front face. The active source position is known. A student measures x from that source position to the detector front face, but initially treats x as the active separation. The table contains background-corrected rates; their relative uncertainty is about 1%. Treat the stated distances and offset as exact for this comparison. The source is long-lived and gamma-only. Separately, the detector manufacturer states that after each registered event there is a brief dead time during which another event cannot be registered.
Calculate rnet x² for all rows and explain why x does not give a consistent inverse-square test. [2]
Use the true active separation d to repeat the test and draw a justified conclusion. [2]
Explain the physical origin of the distance error. [1]
Explain how dead time can reduce a high measured rate, and why a constant mean arrival rate does not guarantee evenly spaced photons. [2]
Already corrected rates; x is a front-face distance
x / m
rnet / s⁻¹
0.100
50.0
0.200
16.0
0.300
7.76
Small hint
The detecting region is farther from the source than the front face. A constant added distance has a larger fractional effect at small x.
Method hint
Use d = x + 0.030 m. Compare rnet d² with rnet x². The dead-time explanation needs random closely spaced arrivals, not a claim that photons decay in the tube.
Complete worked solution and marks
Answer: Using x gives products 0.500, 0.640 and 0.698 m² s⁻¹. Using d = x + 0.030 m gives 0.845, 0.846 and 0.845 m² s⁻¹, consistent within 1%. Random closely spaced photons can be missed during dead time.
rnet x² = 0.500, 0.640 and 0.6984 m² s⁻¹. These increase by about 40% across the table, far beyond 1% uncertainty; x is not an adequate active separation.
d = x + 0.030 m ⇒ d = 0.130, 0.230, 0.330 m. rnet d² = 0.8450, 0.8464 and 0.8451 m² s⁻¹. The spread is only about 0.17%, so the corrected geometry supports inverse square within the stated uncertainty.
The radiation spreads from the active source before reaching the detecting region. Using the front face omits an internal path length. This is a systematic distance offset; collecting more photons does not remove it.
If another photon arrives during the stated blind interval following a registered event, it is not recorded. At high arrival rates such close arrivals are more common, so measured rate can understate the rate entering the detector.
Radioactive decay is random. A constant mean arrival rate describes an average over many intervals; photons may cluster, and other intervals may contain none. They are not emitted at perfectly regular spacings. The photons themselves are not undergoing radioactive decay.
Worked-answer figure. The active region lies 0.030 m behind the detector front face. The front-face distance is x and the correct active separation is x+0.030 m. Correcting the geometry makes all rate-times-distance-squared products about 0.845 square metres per second. More counting cannot remove the systematic offset. Open the larger diagram
Check: The offset fraction is 30% of the smallest x but 10% of the largest. That changing fractional error explains the apparent drift in the uncorrected products.
Mark checklist · 7 marks
1 mark — Obtains all three rnet x² products.
1 mark — Quantifies their variation as far larger than 1% and rejects x as the appropriate separation.
1 mark — Uses d = x + 0.030 m and calculates all three corrected products.
1 mark — Obtains products near 0.845 m² s⁻¹ and judges their approximately 0.17% spread consistent with 1%.
1 mark — Explains the active region lies behind the face, creating a systematic distance offset.
1 mark — Explains missed close arrivals during the supplied dead time reduce a high measured rate.
1 mark — Links random decay to uneven photon arrivals despite a constant mean rate.
Common mistake: The rates are already background corrected, so subtracting background again is not a remedy. “Human error” names no mechanism. Longer counting reduces fluctuations but does not move the active detector region.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
If you count at each distance for four times as long, will that eliminate the offset or dead-time bias?
Check the transfer answer
No. Larger counts reduce relative random counting uncertainty, approximately by a factor of two under the independent-count model. The distance offset remains, and the detector still misses close arrivals. Correct the geometry and use a sufficiently low arrival rate or an appropriate calibrated detector correction.
Question 8 · Exam-style radiation identification and application · 7 marks
Absorption evidence and an ageing foil monitor
Specification: 3.8.1.2, 3.8.1.3
A fixed source and detector are close enough for emitted alpha particles to reach the detector. All counts in the table last 60 s; background is 30 counts in 60 s. For these particular emissions, paper stops alpha but has negligible effect on beta/gamma; 3 mm aluminium stops beta but has negligible effect on gamma; lead reduces the gamma signal. Keep geometry fixed. A separate foil monitor must distinguish small changes around 0.5 mm aluminium: measured transmissions are effectively zero for alpha, 0.55 for beta and 0.995 for gamma.
Use the absorption data to identify which radiation types the source emits, with evidence for each. [3]
Select radiation for the foil monitor and explain why it is suitable. [2]
A falling monitor rate can indicate thicker foil, but the source also decays. Explain the ambiguity and describe a reference measurement that separates the effects. [2]
Gross counts, fixed 60 s intervals
Absorber
Gross count
None
2430
Paper
1530
3 mm aluminium
150
15 mm lead
42
Small hint
Subtract the 30-count background from each equal-time reading. A useful thickness monitor needs partial transmission that changes appreciably with thickness.
Method hint
Identify the drop removed by paper, the next drop removed by aluminium, and the residual signal reduced by lead. Compare the foil reading with a source-only reference at fixed geometry to account for source ageing.
Complete worked solution and marks
Answer: The source emits alpha, beta and gamma under the stated absorption model. Beta is appropriate for the foil monitor because its transmission is partial and sensitive to thickness. A source-only reference separates declining activity from changing foil attenuation.
Net counts = 2400, 1500, 120 and 12; net rates = 40.0, 25.0, 2.00 and 0.200 s⁻¹.
Paper removes a component while beta/gamma are unaffected in the supplied model: this identifies alpha. Aluminium removes a further component that passed through paper: this identifies beta. A remaining above-background component passes through aluminium and is reduced by lead: this identifies gamma. Lead attenuates rather than automatically eliminating all gamma radiation.
Choose beta for these supplied foil data. Its partial transmission allows a measurable rate change when thickness changes. Alpha is already fully absorbed; the stated gamma transmission changes too little around this thickness to give a sensitive monitor.
A lower registered rate can arise from either more attenuation by thicker foil or lower source activity. At fixed geometry measure a background-corrected reference with no foil, or use an equivalent fixed reference channel. Compare foil/reference corrected rates taken at approximately the same time.
In a simple stable-efficiency model rfoil = εA × transmission and rreference = εA. Their ratio isolates transmission; a lower source activity changes both rates. Calibration is needed to convert transmission into thickness.
Worked-answer figure. Source-only rates in fixed geometry are 40,25,2 and 0.2 counts per second for no absorber, paper, aluminium and lead. Bars show rates on a common linear scale. The final small excess needs longer counting to establish a secure residual; gamma identification uses the larger aluminium signal and its reduction by lead. A partially absorbing beta foil monitor uses a reference ratio to separate ageing. Open the larger diagram
Check: All counting times match, so subtracting 30 directly is legitimate. The 12-count excess after lead is small: the independent-count uncertainty estimate is √(42 + 30) ≈ 8.5 counts. Repeat or count longer before claiming a statistically secure residual. Gamma identification here comes from the much larger aluminium signal and its reduction by lead.
Mark checklist · 7 marks
1 mark — Identifies alpha from the component removed by paper under the supplied assumptions.
1 mark — Identifies beta from the further component removed by aluminium.
1 mark — Identifies gamma from the residual above-background signal reduced by lead.
1 mark — Chooses beta for the supplied foil-monitor data.
1 mark — Explains partial, thickness-sensitive transmission and why zero/nearly complete transmission is unsuitable here.
1 mark — Explains thicker foil and declining source activity can both reduce the reading.
1 mark — Uses a background-corrected no-foil/fixed-channel reference or equivalent activity-normalised comparison to separate the effects.
Common mistake: A large drop is evidence to interpret with absorber properties; it is not a universal identification rule without assumptions about energies and materials. “Beta is medium penetrating” needs to be linked to useful partial absorption by this foil.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
The monitor isotope has a 90-day half-life. After 90 days both the corrected foil and no-foil reference rates halve, with identical geometry and detector settings. What can you infer about the foil?
Check the transfer answer
Their ratio is unchanged, so the data indicate unchanged transmission and therefore unchanged calibrated thickness in the stated model. The shared fall is consistent with the source activity halving, rather than evidence that the foil became thicker.
Question 9 · Exam-style ratio calculation and assumptions · 7 marks
Dating a rock: parent plus daughter is the initial ledger
Specification: 3.8.1.3
A rock formed with radioactive parent isotope P and no stable daughter D. Each original P nucleus ultimately produces one D nucleus, with any intermediate decays effectively immediate on this time scale. The system has retained all parent and daughter nuclei since formation. The present numbers satisfy D:P = 3:2. P has half-life 1.20 × 10⁹ years.
Express the initial parent number N0 in terms of the present P and D numbers. Find the fraction of parent remaining. [2]
Calculate the rock’s age. [2]
Explain two assumptions that this dating calculation relies on. [2]
Explain the direction of the age error if some present daughter was already there at formation but you used the same calculation. [1]
Small hint
Every daughter in the stated closed system represents one parent that is no longer P. The initial parent number is larger than the present parent number.
Method hint
N0 = NP + ND. With D:P = 3:2, NP/N0 = 2/5. Use NP/N0 = 2^(−t/T½), then discuss inherited daughter and movement of nuclei.
Complete worked solution and marks
Answer: N0 = NP + ND; parent fraction = 0.400. Age = 1.59 × 10⁹ years. Closed-system retention and no initial daughter are essential; uncorrected inherited daughter overestimates age.
N0 = NP + ND. Take NP = 2 units and ND = 3 units: N0 = 5 units. NP/N0 = 2/5 = 0.400.
0.400 = 2^(−t/T½); t = T½ × ln(1/0.400)/ln2 = 1.59 × 10⁹ years.
The system must be closed to parent and daughter since formation. Otherwise present numbers need not represent the original parent ledger. There must also be no inherited daughter, or its initial number must be known and subtracted. The stated one-daughter-per-original-parent relation and effectively rapid intermediate steps are also needed.
Inherited daughter would be wrongly counted as parent that decayed after formation. That makes the inferred N0 too large, the remaining parent fraction too small and the calculated age too large.
Worked-answer figure. Five equal initial parent units become two remaining parent units plus three daughter units. No initial daughter and closed-system retention make the original ledger P+D. Parent fraction 2/5 gives age 1.322 half-lives, or 1.59 billion years. Units refer to numbers of nuclei, not equal masses. Open the larger diagram
Check: 40% lies below one half but above one quarter, so the age must lie between one and two half-lives. The answer is 1.322 half-lives, within that interval.
Mark checklist · 7 marks
1 mark — Uses N0 = NP + ND under the stated assumptions.
1 mark — Obtains the surviving parent fraction 2/5 = 0.400.
1 mark — Uses an exponential/half-life equation with a consistent year time unit.
1 mark — Obtains age ≈ 1.59 × 10⁹ years.
1 mark — Explains retention/closed-system requirement for both parent and daughter.
1 mark — Explains no initial daughter, or correction for an independently known initial daughter amount.
1 mark — Explains inherited daughter counted as newly produced makes the inferred age too large.
Common mistake: D/P is not the fraction of parent remaining. Use P/(P + D), not P/D or D/(P + D). A measured isotope ratio only becomes an age when the model’s starting and retention assumptions hold.
Exam technique: Set up the parent/daughter ledger before using logs. State the starting and retention assumptions that turn an isotope ratio into an age.
For the same present ratio, independent evidence shows the initial daughter number was 0.50 times the present parent number. Find the corrected age.
Check the transfer answer
Radiogenic daughter = 1.50NP − 0.50NP = NP. Therefore N0 = NP + NP = 2NP and the parent fraction is 0.500: corrected age = 1.20 × 10⁹ years. This is lower than the age obtained by assuming all daughter was produced after formation.
Question 10 · Exam-style two components and a design criterion · 7 marks
A mixed-isotope store has no single fixed half-life
Specification: 3.8.1.3
A storage-design exercise considers two retained, independently decaying parent isotopes. Stable daughters add no activity. Initially X has activity 80.0 MBq and half-life 4.00 years; Y has activity 20.0 MBq and half-life 20.0 years. The design criterion is that their combined activity must be below 15.0 MBq. Use only this given activity criterion; it is not a dose calculation.
Calculate each component activity and the combined activity after 16.0 years. [2]
Repeat after 20.0 years. [2]
Assess the criterion at those two times. [1]
Explain why assigning the whole mixture X’s 4.00-year half-life would be incorrect. [2]
Small hint
Decay each component with its own half-life, then add activities. The slower-decaying component becomes a larger share of the mixture.
Method hint
Use AX = AX,0 × 2^(−t/4) and AY = AY,0 × 2^(−t/20), with t in years. Compare their sum with 15.0 MBq explicitly.
Complete worked solution and marks
Answer: At 16 years: AX = 5.00 MBq, AY = 11.5 MBq, total = 16.5 MBq, above the criterion. At 20 years: 2.50 + 10.0 = 12.5 MBq, below the criterion. The mixture has no single constant half-life.
16.5 MBq is above 15.0 MBq, so the given activity criterion is not met at 16 years. 12.5 MBq is below 15.0 MBq, so it is met at 20 years. Both activities decrease continuously, so the crossing occurs between those times; these calculations do not locate its exact time.
The total is the sum of two exponentials with different decay constants. X decreases faster, so Y becomes an increasing fraction of the remaining activity. A constant fractional reduction of the whole mixture over every 4-year interval does not follow.
Using 4 years for all 100 MBq would predict 100 × 2⁻⁵ = 3.125 MBq at 20 years, far below the correct 12.5 MBq. The longer-lived component must be calculated separately.
Worked-answer figure. Blue X begins at 80 MBq and halves every 4 years; gold Y begins at 20 MBq and halves every 20 years; green is their sum. The sum is 16.5 MBq at 16 years and 12.5 at 20 years, crossing the dashed 15 MBq design criterion between them. It is not one fixed-half-life exponential. Open the larger diagram
Check: Initially X contributes 80% of activity; at 20 years it contributes only 20%. Changing component shares independently explain why the mixture’s apparent half-life changes.
Mark checklist · 7 marks
1 mark — Obtains AX = 5.00 MBq at 16 years.
1 mark — Obtains AY ≈ 11.5 MBq and total ≈ 16.5 MBq at 16 years.
1 mark — Obtains AX = 2.50 MBq at 20 years.
1 mark — Obtains AY = 10.0 MBq and total = 12.5 MBq at 20 years.
1 mark — Explicitly compares both totals with 15.0 MBq and judges fail/pass at the stated times.
1 mark — Explains the total is a sum of exponentials with different decay constants.
1 mark — Explains Y becomes a larger fraction, so the total does not have a constant 4-year half-life.
Common mistake: Activities add; half-lives do not add or average to a universal mixture half-life. Passing the stipulated activity criterion does not by itself calculate dose or decide every aspect of a storage design.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
Try a changed context
What is the total activity after a further 20 years, at t = 40 years? Does it equal half the 20-year total?
Check the transfer answer
AX = 80/2¹⁰ = 0.0781 MBq; AY = 20/2² = 5.00 MBq; total = 5.08 MBq. Half of 12.5 MBq would be 6.25 MBq, so the total has not halved over this interval. As X becomes negligible, Y’s 20-year half-life increasingly describes the remaining activity.
Question 11 · Exam-style complete activity-to-power budget · 8 marks
An autonomous beacon powered by radioactive decay
Specification: 3.8.1.3, 3.4.1.7
An autonomous beacon uses a radioisotope power supply. Initially it contains 0.400 kg of parent isotope Q, with molar mass 0.200 kg mol⁻¹ and half-life 40.0 years. Each parent decay deposits 6.00 × 10⁻¹³ J as usable thermal energy. A constant 6.00% of this heat becomes electrical energy. The beacon needs at least 14.0 W. Daughters are stable; assume no material losses. Use NA = 6.02 × 10²³ mol⁻¹ and 1 year = 3.1536 × 10⁷ s.
Calculate the initial number of parent nuclei. [2]
Calculate the decay constant in s⁻¹ and initial activity. [2]
Find the initial electrical power. [2]
Calculate how long the supply can meet the minimum power requirement. [2]
Small hint
Activity links nuclei to energy per second. Efficiency multiplies thermal power to give electrical power.
Method hint
Use N0 = (m/M)NA, λ = ln2/T½, A0 = λN0 and P0 = ηA0E. With constant η and E, power has the same exponential time dependence as activity.
Complete worked solution and marks
Answer: N0 = 1.20 × 10²⁴; λ = 5.49 × 10⁻¹⁰ s⁻¹; A0 = 6.62 × 10¹⁴ Bq; initial electrical power = 23.8 W. The 14.0 W threshold is reached after 30.7 years.
n = 0.400/0.200 = 2.00 mol; N0 = nNA = 1.20 × 10²⁴ nuclei.
Thermal power = A0E = 397 W; P0 = 0.0600 × A0E = 23.8 W.
P = P0e−λt, since efficiency and energy per decay are constant. t = ln(P0/14.0)/λ = 9.67 × 10⁸ s = 30.7 years, using unrounded P0 and λ.
The beacon can meet 14.0 W from the start up to this threshold time in the stated ideal model. Real changes in conversion efficiency or load would require a new budget; they are excluded here.
Worked-answer figure. Electrical power is 23.817 W initially and halves every 40 years under constant efficiency. A dashed load line at 14 W meets the decay curve at 30.663 years. Budget uses number of nuclei, activity, deposited energy per decay and efficiency, not conversion of the entire parent mass to energy. Open the larger diagram
Check: 14.0/23.8 ≈ 0.588, so the threshold is reached before one 40-year half-life. Bq × J per decay gives J/s, the correct power unit. The output is much smaller than the thermal input.
Mark checklist · 8 marks
1 mark — Finds n = 2.00 mol using consistent mass units.
1 mark — Finds N0 ≈ 1.20 × 10²⁴ nuclei.
1 mark — Converts half-life to seconds and finds λ ≈ 5.49 × 10⁻¹⁰ s⁻¹.
1 mark — Uses A = λN to obtain A0 ≈ 6.62 × 10¹⁴ Bq.
1 mark — Uses activity × energy per decay to find thermal power ≈ 397 W.
1 mark — Applies efficiency 0.0600 to obtain electrical power ≈ 23.8 W.
1 mark — Uses an exponential power/activity ratio to find threshold time with a positive logarithm.
1 mark — Obtains about 30.7 years with the correct time conversion and interprets the threshold.
Common mistake: The full parent mass is not converted to energy on each decay. Use the supplied energy per decay. N means the number of undecayed nuclei, and 6.00% means multiply by 0.0600, not 6 or 0.600.
Exam technique: Build the chain N → A → thermal power → electrical power before solving for time. An explicit comparison with the required load completes the argument.
At exactly 20.0 years the conversion efficiency abruptly falls from 6.00% to 4.00%, with other assumptions unchanged. Can the beacon still operate immediately afterwards?
Check the transfer answer
P = P0 × 2−0.5 × (0.0400/0.0600) = 11.2 W. This is below 14.0 W, so it cannot meet the specified load immediately after the efficiency loss, even though nuclear decay alone would not yet have reached the original threshold.
Question 12 · Exam-style discrete decay and interpretation · 6 marks
A random model: constant probability, changing counts
Specification: 3.8.1.3
Eight hundred fair eight-sided dice model undecayed nuclei. After each throw, remove dice showing 1 and throw only the survivors again. One throw is one equal model time interval. Each surviving die has removal probability p = 1/8, independent of its previous throws. You may use the exact discrete expectation ⟨Nk⟩ = N0(1 − p)k. Define an equivalent exponential coefficient per throw by ⟨Nk⟩ = N0e−λeffk.
Explain what random and spontaneous mean for real radioactive decay, and which aspect the dice represent. [2]
Calculate the expected number of survivors after eight throws. Explain why an actual run need not give this number. [2]
Determine λeff in throw⁻¹. Explain why constant per-die probability does not mean a constant number removed each throw. [2]
Small hint
Only survivors are thrown again. The model has a fixed fraction expected to survive each throw, not a fixed number.
Method hint
Use 800(7/8)^8 and λeff = −ln(7/8). Each die’s probability is constant but the population exposed to that probability becomes smaller.
Complete worked solution and marks
Answer: Expected survivors after eight throws ≈ 275; an actual integer count can differ. λeff = 0.134 throw⁻¹. Expected losses fall as the number of surviving dice falls; real spontaneous decay requires no external trigger.
Real decay is random: the exact decay time of a particular nucleus cannot be predicted. It is spontaneous: it occurs without an external trigger. The dice represent random removal with a fixed per-survivor probability; the need to throw them is a limitation of the analogy for spontaneity.
⟨N8⟩ = 800(7/8)⁸ = 274.887… ≈ 275.
This is an ensemble expectation, not the guaranteed result of one run. Different throws and runs give different integer survivor counts. A larger starting population usually produces a smaller relative fluctuation about the expected curve.
The exact discrete coefficient is not p = 0.125. The approximation λeff ≈ p only works well when the probability per step is small. The supplied definitions make the exact relation clear.
Expected removals on the first throw: 800/8 = 100. Expected survivors then: 700; expected second-throw removals: 700/8 = 87.5. The same probability acts on a declining population.
Worked-answer figure. Whole-throw expected survivors are marked on the curve 800 times (7/8)^k. The smooth green interpolation defines an equivalent coefficient −ln(7/8), about 0.134 per throw. Expectations may be non-integer; actual observed counts fluctuate and are integers. Open the larger diagram
Check: The corresponding continuous interpolation has a half-life of ln2/λeff = 5.19 throws, although observations occur at whole throws. An expectation can be non-integer; one actual run cannot contain a fraction of a die.
Mark checklist · 6 marks
1 mark — Explains unpredictable individual decay time/randomness.
1 mark — Explains no external trigger/spontaneity and recognises dice mainly model random probability.
1 mark — Uses 800(7/8)⁸ to obtain expected survivors ≈ 275.
1 mark — Explains actual runs fluctuate and do not have to equal the ensemble expectation.
1 mark — Uses the supplied discrete/exponential equivalence to obtain λeff = −ln(7/8) ≈ 0.134 throw⁻¹.
1 mark — Explains constant probability gives fewer expected removals as the survivor population falls.
Common mistake: λeff = 1/8 is only a small-step approximation, not the exact coefficient in the equation given here. Do not put removed dice back into the next throw or expect exactly one eighth to be removed each time.
Exam technique: State what each quantity measures, correct background before processing the data, and keep time units consistent. These are original questions with PhysicsUK’s own marking guidance.
Repeat the model with 1600 starting dice. Compare expected survivors after eight throws and λeff. Does the model determine exactly which dice survive?
Check the transfer answer
Expected survivors double to 550 (549.774 before rounding), but λeff stays 0.134 throw⁻¹. Each survivor still has the same removal probability. The model predicts population statistics, not the identities or exact removal times of individual dice.
Use the simulation to check your predictions
In the random-decay explorer choose 200 initial nuclei and half-life 4 s. At 4 s (one half-life on the Time control), predict an expected population of 100, λ = 0.1733 s⁻¹ and expected instantaneous activity 17.33 Bq. Use New random run repeatedly: the realised survivor count varies around the expectation. The first counting bin lasts 2 s; its ensemble expected removals are 58.58 and expected mean rate 29.29 s⁻¹, different from the initial instantaneous activity 34.66 Bq. Choose 2000 initial nuclei at the same half-life: expected values are ten times larger and relative fluctuations tend to be smaller. Doubling half-life to 8 s leaves half the initial population expected at 8 s but halves λ and initial expected activity for the same starting number. This model registers all decay events and adds no detector background, efficiency loss or dead time; its event-rate bins are not a real detector calibration. Reset restores 200 nuclei, half-life 4 s and the original seeded run. It is a population-statistics model, not a prediction of an individual nucleus’s decay time.
This set practises selected skills in AQA A-level 7408 sections 3.8.1.2–3.8.1.3: alpha/beta/gamma absorption and applications, background correction, gamma inverse square and Required Practical 12, random/spontaneous decay, constant per-nucleus probability, λ and half-life, N and A exponential laws, mass-to-nuclei/activity, graphical and logarithmic analysis, dating and storage applications. Supporting uncertainty and power skills are used. General radiation-property comparisons, nuclear equations and medical risk/benefit explanations should also be studied in the partner notes. The uncertainty expression, detector dead-time description, discrete dice law and power-supply energy per decay are supplied where needed; they are not extra formula-recall requirements. The mixed-isotope task explicitly sums separately decaying parent activities. Dating uses a stated closed system and daughter ledger. This is A-level, not AS 7407. Rutherford scattering, detailed nuclear instability, radius, binding energy and reactor design are separate topics. Medical-option biological half-life, dosimetry and nuclear activation thresholds are not required here.
All twelve questions, data, diagrams, transfer tasks and mark checklists are original PhysicsUK teaching resources. Eleven linked lessons paraphrase checked AQA 7408/2 papers, marking and reports from June 2018, June 2024 and June 2025, plus 7408/3A November 2021. The index was used to find candidates; original documents were checked for each public source claim. New uncertainty, detector-offset, foil-calibration, mixed-storage and beacon examples are specification-based applications, not questions attributed to those reports. Source mark allocations are not transplanted to new questions. No claim about topic frequency or future papers is implied.