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6.1.12 Penetration of alpha, beta and gamma radiation

Penetration and ionisation

Definition

Penetrating power

The ability of radiation to pass through a material without being absorbed.

Definition

Ionising power

The ability of radiation to remove electrons from the atoms it passes, turning them into ions.

  1. Alpha particles, beta particles and gamma rays can pass through different thicknesses of material before they are stopped, and this is their penetrating power.
  2. As radiation passes through a material, it ionises atoms by knocking electrons out of them, and it loses some of its energy each time it does so.
  3. Radiation is absorbed once it has transferred all of its energy to the material.
  4. Radiation that is strongly ionising loses its energy quickly, so it is stopped after only a short distance and has a low penetrating power.
  5. Radiation that is weakly ionising loses its energy slowly, so it travels a long way and has a high penetrating power.
  6. Penetrating power and ionising power therefore follow opposite orders for the three types of radiation.

Alpha particles

  1. Alpha particles are the least penetrating of the three types of radiation.
  2. They travel only about 5 cm5\ \text{cm}5 cm in air before they are stopped.
  3. They are stopped by a sheet of paper or by the outer layer of dead skin.
  4. Alpha particles are the most strongly ionising, because they are large and carry a charge of +2+2+2, so they collide with and ionise many atoms along a short path.

Beta particles

  1. Beta particles are more penetrating than alpha particles but less penetrating than gamma rays.
  2. They travel up to about 1 m1\ \text{m}1 m in air.
  3. They pass through paper but are stopped by a sheet of aluminium a few millimetres thick, typically about 3 mm3\ \text{mm}3 mm to 5 mm5\ \text{mm}5 mm.
  4. Beta particles are moderately ionising, because they have a charge of −1-1−1 and a very small mass.

Gamma rays

  1. Gamma rays are the most penetrating of the three types of radiation.
  2. They can travel hundreds of metres through air and pass easily through paper and aluminium.
  3. Gamma rays are never completely stopped, but their intensity is greatly reduced by several centimetres of lead or by a thick wall of concrete.
  4. Gamma rays are only weakly ionising, because they have no charge and no mass.

Identifying the radiation

  1. The type of radiation from a source can be identified by finding which materials reduce the count rate from a detector.
  2. If a sheet of paper makes the corrected count rate fall sharply, the source emits alpha particles.
  3. If paper has little effect but a few millimetres of aluminium makes the count rate fall sharply, the source emits beta particles.
  4. If a significant count rate remains after the aluminium and is only reduced by thick lead, the source emits gamma rays.
  5. Many sources emit more than one type, so a count rate that drops at each stage shows a mixture of radiations.
  6. The same differences explain how radiation is chosen for a task, such as using beta particles to check the thickness of paper in a factory, because changes in the paper thickness noticeably change how many beta particles get through.
Key Idea

Comparing the three radiations

  • Alpha: range of a few centimetres in air, stopped by paper, most ionising.
  • Beta: range of about a metre in air, stopped by a few millimetres of aluminium, moderately ionising.
  • Gamma: range of hundreds of metres in air, reduced by thick lead or concrete, weakly ionising.
Practical

Investigating penetrating power

  • Aim: to compare how far alpha, beta and gamma radiation penetrate different materials by measuring the count rate through each absorber.
  • Apparatus: a Geiger-Muller tube connected to a counter, a stopwatch, sealed alpha, beta and gamma sources in a lead-lined box, handling tongs, a clamp and stand, a metre ruler, sheets of paper, aluminium sheets of 1 mm1\ \text{mm}1 mm thickness and lead sheets about 1 cm1\ \text{cm}1 cm thick.
  • Method, measuring background:
    • With all sources locked away, switch on the counter and record the number of counts in 111 minute.
    • Repeat this three times and calculate the mean background count rate.
  • Method, measuring through absorbers:
    • Clamp the Geiger-Muller tube and use the tongs to place one source at a fixed distance of about 3 cm3\ \text{cm}3 cm from the end of the tube, close enough for alpha particles to reach it through the air.
    • Record the count in 111 minute with no absorber between the source and the tube.
    • Place a single sheet of paper between the source and the tube and record the count in 111 minute.
    • Replace the paper with 1 mm1\ \text{mm}1 mm of aluminium, record the count, and then add further sheets one at a time up to 5 mm5\ \text{mm}5 mm, recording the count each time.
    • Replace the aluminium with lead sheets, adding them one at a time and recording the count each time.
    • Repeat each reading three times and calculate a mean.
    • Return the source to its box with the tongs and repeat the whole procedure for each of the other sources.
  • Method, processing results:
    • Subtract the mean background count rate from every reading to give the corrected count rate.
  • Results: the alpha count falls to the background level with one sheet of paper, the beta count falls to background after a few millimetres of aluminium, and the gamma count falls only gradually as lead is added.
  • Variables: the type and thickness of absorber is the independent variable, the corrected count rate is the dependent variable, and the distance from source to tube, the counting time and the source used are control variables.
  • Watch out: decay is random, so single readings fluctuate and repeats or longer counting times are needed to see a real change, and the source distance must stay the same for every reading.
  • Safety: this is normally carried out as a teacher demonstration, the sources are handled only with tongs at arm's length and never pointed at anyone, the time each source is out of its box is kept as short as possible, and hands are washed afterwards.
Example

Identifying radiations from absorber data

  • A source is tested with a Geiger-Muller tube, and the background count rate is 252525 counts per minute.
  • The measured count rates are 485485485 counts per minute with no absorber, 480480480 with paper, 120120120 with 5 mm5\ \text{mm}5 mm of aluminium and 303030 with 5 cm5\ \text{cm}5 cm of lead.
  • The background is subtracted from each reading.
485−25=460,480−25=455,120−25=95,30−25=5 485 - 25 = 460, \quad 480 - 25 = 455, \quad 120 - 25 = 95, \quad 30 - 25 = 5 485−25=460,480−25=455,120−25=95,30−25=5
  • Paper makes almost no difference to the corrected count rate, so the source does not emit alpha particles.
  • The aluminium causes a large fall from 455455455 to 959595 counts per minute, so the source emits beta particles.
  • A corrected count rate of 959595 counts per minute still passes through the aluminium and is only reduced by the lead, so the source also emits gamma rays.
Common Mistake
  • Do not say that lead completely stops gamma rays, because lead only reduces their intensity.
  • Do not say that the most penetrating radiation is the most ionising, because the order of ionising power is the reverse of the order of penetrating power.
  • Do not forget to subtract the background count before comparing readings, because the detector never reads zero.
Exam technique

Describing penetrating power

  • Name a specific material and thickness for each radiation, such as "stopped by paper" for alpha and "stopped by a few millimetres of aluminium" for beta.
  • For gamma, write that it is "reduced" or "absorbed" by thick lead or concrete, because examiners do not allow a statement that gamma is easily stopped.
  • When explaining a difference in penetration, link it to ionisation, because strongly ionising radiation transfers its energy quickly and so travels less far.
  • When interpreting absorber data, compare each reading with the one before it and say which radiation the drop shows.
Self review
  • What material stops alpha particles?
  • What thickness of aluminium is needed to stop beta particles?
  • What can reduce the intensity of gamma rays?
  • Why are alpha particles the least penetrating of the three radiations?
  • Why is the background count rate measured before testing the absorbers?
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6.1.12 Penetration of alpha, beta and gamma radiation Revision Guide

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Revision notes for OCR GCSE Physics 6.1.12 Penetration of alpha, beta and gamma radiation: explanations and worked examples.

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