Radioactivity

Part ofPhysicsNuclear physics

Background radiation

materials occur naturally and, as a result, everyone is exposed to a low-level of radiation every day. This exposure comes from a mixture of natural and man-made sources.

Pie chart of artificial sources of radiation

The actual amount of that a person is exposed to depends on where they live, the job they do and many other factors.

is low level nuclear radiation that is always present from natural and man-made sources eg cosmic rays from the Sun. Scientists must always take into consideration the amount of background radiation when working or experimenting with radioactive sources and discount it from their results.

Background radiation affects everyone mainly by , but a small amount is from being contaminated by in the food and drink that is consumed.

Measuring amounts of radiation

The activity of a radioactive source is the number of decays per second from the unstable present in the source.

Radioactivity can be measured in counts per second or per minute.

Since is a random process, it is always good practice to determine the average count rate rather than to measure the counts that occur in just one second or one minute.

Radioactivity can be detected using a Geiger-Muller tube connected to a counter.

When alpha (\(\alpha\)) particles, beta (\(\beta\)) particles or gamma (\(\gamma\)) rays enter the GM tube the counter clicks and the count is displayed on the screen.

The number of counts per second or per minute is called the count rate.

Geiger-Muller tube connected to a counter.

Measuring the background radiation

  • Remove all known sources of radioactivity from the room.

  • Set the counter to zero.

  • Switch on and start a stop clock.

  • After 20 minutes switch off. Record the count.

  • Divide the count by 20 to calculate the count rate per minute.

The background count rate is measured over a period of 20 minutes because of the random nature of radioactive decay.

Dividing by 20 enables the average count rate per minute to be determined.

Background count rate is typically 18 counts per minute which does not present a serious health risk to humans.

Extended syllabus content: Determining a correct count rate

If you are studying the Extended syllabus, you will also need to know about how to determine a corrected count rate. Click 'show more' for this content:

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How radiation can be detected

The ionising effect of radiation is used in the Geiger-Muller (GM) tube as a means of detecting the radiation.

The GM tube is a hollow cylinder filled with a gas at low pressure. The tube has a thin window made of mica at one end. There is a central electrode inside the GM tube. A high voltage supply is connected across the casing of the tube and the central electrode as shown in the following diagram.

Cross-section of a Geiger-Muller tube showing a thin mica window at one end and a central electrode inside surrounded by a gas at low pressure. The electrode is connected to an external supply and feeds a counting circuit.

When alpha (\(\alpha\)), beta (\(\beta\)) or gamma (\(\gamma\)) radiation enters the tube it produces ions in the gas. The ions created in the gas enable the tube to conduct. A current is produced in the tube for a short time. The current produces a voltage pulse. Each voltage pulse corresponds to one ionising radiation entering the GM tube. The voltage pulse is amplified and counted.

The greater the level of radiation, the more ionisation in the tube so the greater the number of counts.

The GM tube counting the number of ionisations may not provide a completely accurate reading, as the number of counts will simply keep increasing.

The quantity activity gives an indication of how radioactive a substance is. Activity is the number of radioactive atoms which disintegrate and emit radioactivity per second.

Activity is measured in units called (Bq) named after Henri Becquerel, the French scientist.

\(Activity = \frac{number~of~disintegrations}{time~taken}\)

\(A = \frac{N}{t}\)

Time is measured in seconds \((s)\). The number of disintegrations has no units.

The number of disintegrations cannot be determined easily in practical work, but the count of radioactive particles detected by a Geiger Muller counter is a useful approximation at this level, and can give an indication of the rate of change of activity.

Video: Measuring the activity of a radioactive sample

Watch this video to see the procedure for measuring the activity of a radioactive sample, taking into account the background radiation.

Extended syllabus content: Background radiation measurements

If you are studying the Extended syllabus, you will also need to know how to use measurements of background radiation to determine a corrected count rate. Click 'show more' for this content:

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The three types of nuclear emission

The of radiation from a nucleus is and random in direction. Three types of ionising radiation are:

Alpha particle

particle \(\alpha\)- is a helium nucleus, two protons and two neutrons. It has a large mass, compared to other ionising radiations, and a strong positive charge.

Beta particle

particle \(\beta\)- is a fast-moving electron. It has a very small mass and a negative charge.

Gamma ray

A \(\gamma\)- is a high-energy electromagnetic wave. Gamma rays are caused by changes within the nucleus. They are part of the electromagnetic spectrum and so travel at the speed of light. They have no mass and no charge.

Penetrating power

Each type of radiation has a different ability to penetrate materials. The material is said to have absorbed the radiation.

Alpha radiation stopped by paper, beta radiation passes through paper but stopped by aluminium, gamma radiation passes through paper and aluminium but stopped by lead.

The energy of the three radiations is absorbed by the material through which the radiation passes. The amount of energy which is absorbed depends on the type of radiation and the type of the absorbing material.

  • The range of the alpha radiation in an absorbing material is less than that of beta or gamma. The alpha radiation transfers more energy to an absorber than beta or gamma radiation. Alpha radiation is absorbed by the thickness of the skin or by a few centimetres of air.

  • Beta radiation is more penetrating than alpha radiation. It can pass through the skin, but it is absorbed by a few centimetres of body tissue or a few millimetres of aluminium.

  • Gamma radiation is the most penetrating of the three radiations. It can easily penetrate body tissue. It requires several centimetres of lead or about one metre of concrete to absorb it.

RadiationRange (cm)Ionising powerCan pass through paper?Can pass through 5mm of aluminium?Can pass through 5cm of lead?
Alpha3-5Highly ionisingNoNoNo
BetaAbout 15IonisingYesNoNo
GammaMuch longerWeakly ionisingYesYesNo - although some will still get through

Extended syllabus content: Deflection of alpha, beta and gamma radiation

If you are studying the Extended syllabus, you will also need to describe the deflection of alpha, beta and gamma radiation. Click 'show more' for this content:

Extended syllabus content: Ionising effects

If you are studying the Extended syllabus, you will also need to know about Ionising effects. Click 'show more' for this content:

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Radioactive decay

Radioactive decay is a change in an unstable nucleus that can result in the emission of alpha particles or beta particles and/or gamma radiation. These changes are spontaneous and random.

A nucleus changes into a new element by emitting alpha or beta particles. These changes are described using nuclear equations.

Extended syllabus content: Decay equations

If you are studying the Extended syllabus, you will also need to know about decay equations. Click 'show more' for this content:

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Half-life

is a random process. A block of material will contain many trillions of and not all nuclei are likely to decay at the same time, so it is impossible to tell when a particular nucleus will decay.

It is not possible to say which particular nucleus will decay next but given that there are so many of them, it is possible to say that a certain number will decay in a certain time. Scientists cannot tell when a particular nucleus will decay but they can use statistical methods to tell when half the unstable nuclei in a sample will have decayed. This is called the .

Half-life is the time it takes for half of the unstable nuclei in a sample to decay or for the activity of the sample to halve or for the count rate to halve.

Count rate is the number of decays recorded each second by a detector, such as the Geiger-Muller tube. This also known as the Activity of the source. One decay per second is known as one Becquerel (Bq).

The illustration below shows how a radioactive sample is decaying over time.

Graph with time against activity in becquerels, with a downward sloping curve.

From the start of timing, it takes two days for the count to halve from 80 down to 40. It takes another two days for the count rate to halve again, this time from 40 to 20.

Note that this second two-day period does not see the count drop to zero, only that it halves again. A third, two-day period from four days to six days see the count rate halving again from 20 down to 10.

This process continues and although the count rate might get very small, it does not drop to zero completely.

The half-life of radioactive carbon-14 is 5,730 years. If a sample of a tree (for example) contains 64 grams (g) of radioactive carbon after 5,730 years it will contain 32 g, after another 5,730 years that will have halved again to 16 g.

Extended syllabus content: Calculations using half-life

If you are studying the Extended syllabus, you will also need to know about calculations using half-life. Click 'show more' for this content:

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Irradiation

Extended syllabus content: Types of radiation emitted

If you are studying the Extended syllabus, you will also need to know about the types of radiation emitted and how the half-life of an isotope determines which isotope is used for applications. Click 'show more' for this content:

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Uses of radiation

Radioactive materials are moved, used and stored in a safe way.

Uses of radioactivity in the home: smoke detectors

One type of smoke detector uses Americium-241, an alpha particle source, to detect smoke.

Diagram of smoke alarm with labels of battery and alarm bell

The alpha particles pass between the two charged metal plates, causing air particles to ionise (split into positive and negative ions).

The are attracted to the oppositely charged metal plates causing a current to flow.

When smoke enters between the plates, some of the alpha particles are absorbed causing less ionisation to take place.

This means a smaller than normal current flows so the alarm sounds.

An alpha source is used because alpha radiation does not penetrate very far.

It is absorbed by a few centimetres of air.

This means that as long as the detector is high up on a wall, or the ceiling, it is safe for humans to be in the same room.

The source should have a long half-life so that the smoke detector does not have to be replaced too frequently, and so that the count rate remains almost constant each day.

Uses of radioactivity in agriculture: food preservation

Gamma radiation from a radioactive source such as cobalt-60 can be used to kill bacteria on fresh food and enable it to keep for longer.

Harmful bacteria, moulds and yeasts grow on foods, and can be killed by gamma rays.

This helps to prolong the shelf life of fresh fruit, vegetables, spices, fish and chicken, reduces food poisoning and food waste, and helps to keep prices down.

Using radiation in this way does not make the food radioactive as the food itself never comes into contact with the radioactive source.

It is the energy from the radioactive source in the form of gamma rays that kills the bacteria that can cause food poisoning in a similar way that heat energy kills bacteria when food is heated.

Once the radiation treatment has stopped, the food quickly loses this energy in the same way that cooked food quickly cools down.

Other uses of radiation in agriculture include:

  • Plant seeds can be exposed to radiation to produce new, stronger and better plants.

  • Radiation can be used to control the number of dangerous insects. This decreases the use of dangerous pesticides.

  • Radioactive sources are used in machines that measure the thickness of eggshells to screen out thin, breakable eggs before they are packaged in egg cartons.

  • Many of our foods are packaged in polyethylene film (also known as shrink wrap). This is exposed to radiation so that it can be heated above its usual melting point and wrapped around foods to provide an airtight protective covering.

Uses of radiation: in industry

To control the thickness of metal or paper

Radioactive sources are used in industry to control the thickness of metal or paper as it is rolled into thin sheet.

An is placed on one side of a sheet and a detector on the other.

If the thickness of the sheet remains constant the activity will not change.

If there is a change in thickness, the activity increases or decreases.

This can trigger the rollers to squeeze harder or less hard to maintain the correct thickness.

A beta source is used because beta radiation can penetrate paper or thin aluminium, but the amount of penetrating will vary sufficiently as thickness changes.

The source should have a long so that the count rate remains almost constant each day and so that it does not need to be replaced too frequently.

Graphic shows how radiation absorbed by aluminium foil is used to gauge the thickness of a material by measuring the radiation that passes through. The foil is between an emitter and a detector.
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The effects of radiation on the human body

materials are hazardous. Nuclear radiation can chemicals within a body, which changes the way the cells behave. It can also deposit large amounts of energy into the body, which can damage or destroy cells completely.

Some of the effects that radiation has on a human body are shown below.

Body partEffect
EyesHigh doses can cause cataracts.
ThyroidRadioactive iodine can build up and cause cancer, particularly during growth.
LungsBreathing in radioisotopes can damage DNA.
StomachRadioactive isotopes can sit in the stomach and irradiate for a long time.
Reproductive organsHigh doses can cause sterility or mutations.
SkinRadiation can burn skin or cause cancer.
Bone marrowRadiation can cause leukaemia and other diseases of the blood.

Managing the risks

The risk associated with radioactive materials depends on the amount of exposure. Being exposed to highly radioactive materials or being exposed to radioactive materials for long periods of time or on a regular basis increases the dose received which, in turn, increases the risk.

Safety precautions

Given that radioactive materials are hazardous, certain precautions can be taken to reduce the risk of using radioactive sources. These include:

  • Keep radioactive sources like technetium-99 shielded (preferably in a lead-lined box) when not in use.

  • Only move them when absolutely necessary and following strict protocols.

  • Wear protective clothing to prevent the body becoming contaminated should radioactive isotopes leak out.

  • Avoid contact with bare skin and do not attempt to taste the sources.

  • Wear face masks to avoid breathing in materials.

  • Handle radioactive materials with tongs in order to keep a safer distance from sources.

  • Monitor exposure using detector badges, etc.

Extended syllabus content: Safety precautions extended

If you are studying the Extended syllabus, you will also need to be able to explain safety precautions for all ionising radiation. Click 'show more' for this content:

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Quiz

Test your knowledge with this quiz on radioactive decay.

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Teaching resources

Are you a physics teacher looking for more resources? Share this short video with your students, in which science presenter Jon Chase explains some of the uses of radioactivity and how unstable nuclei decay release ionising radiation:

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