Radiation Detectors
Key idea: Learn how GM tubes, film badges and cloud chambers detect radiation, handle background count-rate, and pick the right detector for common scenarios (O Level).
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The core idea
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Learning objectives
- Describe atomic composition
- Use proton number, nucleon number and isotope
- Use and interpret nuclide notation
- Explain random and spontaneous nuclear decay
- Describe alpha, beta-minus and gamma radiation
- Compare ionising effect and penetrating power
- Use nuclide equations for radioactive decay
- Explain background radiation
- Use half-life in tables and decay curves
- State radioactivity applications and hazards
- Evaluate uses and hazards using half-life and radiation properties
- Relate fission and fusion to nuclear-energy release
1. Definition
Radiation detectors are instruments used to detect ionising radiation (alpha, beta, gamma).
For O Level, the most common detector you should know is the Geiger–Müller (GM) tube.
2. Key Ideas
- A GM tube produces a count-rate in counts per second or counts per minute. With geometry fixed, a larger net count-rate usually indicates a larger activity, but count-rate is not identical to activity.
- Always subtract background: net count-rate = measured - background
- A film badge/dosimeter records cumulative exposure over time.
- A cloud chamber can make tracks visible (useful to distinguish alpha vs beta by track thickness/length).
3. Detailed Explanations
A. Geiger–Müller (GM) tube
When ionising radiation enters the tube, it ionises the gas. This causes a brief current pulse, which is counted electronically.
GM tubes are useful for:
- comparing radiation intensity at different positions
- plotting decay curves (for half-life)
The recorded count-rate also depends on source–detector distance, orientation, absorbers and detector efficiency. Keep these fixed when comparing sources or measurements.
B. Photographic film / film badge
Film darkens when exposed to ionising radiation. A film badge can be worn to monitor exposure over a period of time (e.g. a month).
C. Cloud chamber (visual tracks)
The radiation ionises air along its path. Vapour condenses along the ions, making the track visible.
4. Common Mistakes
- Not subtracting background count-rate before interpreting results.
- Thinking a GM tube tells you the type of radiation directly (you usually need absorbers/deflection tests).
- Confusing count-rate (cpm) with radiation dose (different concept).
- Treating one short count as exact. Random decay causes statistical fluctuations; count for longer or repeat and average when the method allows.
5. Exam Tips
- If the question uses a GM tube, write “subtract background” early.
- If asked “which detector?”, match the purpose:
- quick checking: GM tube
- long-term monitoring: film badge
- visualising tracks: cloud chamber
6. Worked Examples
Modelled example 1
Net count-rate
Problem
Study the worked solution
Separate measured and background rates
Method
Identify the source-plus-background reading and the background-only reading.Reason
The detector continues to count environmental background when the source is present.Working
Measured = 145 cpm; background = 25 cpm.Subtract background
Method
Remove the background contribution from the measured rate.Reason
The remainder estimates the count-rate attributable to the source in this geometry.Working
net = 145-25 = 120 cpm
Guided practice 2
Choosing a detector
Problem
Match detector to purpose
Hints
Hint 1: focus on the timescale
View solution step by step
Match the measurement role
Method
Select a film badge or equivalent personal dosimeter.Reason
It records cumulative exposure over the period it is worn.Working
A GM tube is suited to immediate count-rate checks; a cloud chamber visualises tracks.State the operational reason
Method
Assign and review the badge for each worker over the monitoring interval.Reason
The record must correspond to that person’s accumulated exposure.Working
The badge is processed or read after the stated monitoring period.
Common misconception 3
Find the background count-rate
Learner response
Diagnose before viewing the correction
View solution step by step
Write the count-rate relationship
Method
Express measured rate as net source rate plus background.Reason
The measured reading contains both contributions.Working
measured = net + backgroundRearrange and calculate
Method
Subtract the net rate from the measured rate.Reason
The background is the remaining contribution.Working
background = 200-150 = 50 cpm
Examiner practice 4
Using absorbers to identify radiation
Examination question
Write the inference and evidence
View solution step by step
Use the corrected observation
1 markMethod
State that the source signal disappears after paper is inserted.Reason
Background subtraction distinguishes stopping from the detector’s ordinary environmental count.Working
The net rate changes from a clear positive value to zero.Connect absorber and penetration
1 markMethod
Recall that paper stops alpha radiation.Reason
Alpha has low penetrating ability compared with beta and gamma.Working
Paper between source and detector prevents alpha particles reaching the GM tube.Make the bounded inference
1 markMethod
Identify alpha as the most likely radiation.Reason
The absorber evidence supports the identification, whereas a GM count alone does not.Working
Most likely radiation: alpha.
Self-mark with the mark scheme
Compare your response with each mark point. Select a point only when your response contains that evidence.
Self-mark the evidence chain.
Challenge 5
Converting cpm to cps
Rate-unit transfer
Convert the time basis
Hints
Hint 1: change from one minute to one second
View solution step by step
Convert the denominator interval
Method
Divide the per-minute count by 60.Reason
A per-second interval is one sixtieth of a minute, so the numerical rate is smaller.Working
420 cpm÷60 = 7 cpsInterpret the rate
Method
State that 7 cps is an average rate.Reason
Radioactive counts fluctuate randomly from one second to the next.Working
It does not predict exactly seven counts in every individual second.
7. Mind Stretchers
Mind stretcher 1: Fluctuating count-rateExtension
Why can the count-rate fluctuate even if the source and setup do not change?
Show Answer
Radioactive decay is random, so the number of decays detected in each time interval varies. If you measure for a longer time, the average count-rate becomes more stable (smaller percentage fluctuation).
Mind stretcher 2: Can a GM tube tell you the type?Extension
Why can a GM tube usually not identify whether the radiation is alpha, beta or gamma by itself?
Show Answer
The GM tube mainly counts ionisation events, so it measures count-rate, not the radiation type. To identify the type, you usually need extra tests such as absorbers (paper/aluminium/lead) or field deflection.
8. Practice and next step
Plan a fair absorber comparison with matched counting times and background subtraction, then continue to Nuclear Fission and Fusion.
Continue with the next resource in this course.
Course and syllabus information
- Course
- SEC G3 Physics
- Edition
- SEC G3 Physics 2027