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Physics
Double Award
Cambridge IGCSE

 

TOPIC 5: NUCLEAR PHYSICS

5.2a Nuclear Decay

The rock shown here is radioactive. It contains uranium-238, a radioactive isotope.

But what makes it 'radioactive'? Many atoms are unstable as discussed in the last section. Eventually the uranium nuclei will split apart, emitting some particles. Uranium decays very slowly and this rock will be radioactive for millions of years. The particles emitted can be extremely dangerous to human health. They 'ionise' other atoms, knocking outer electrons away and this can change the chemical bonds of any molecules they hit.

uranium ore
Figure 1: A rock containing uranium
Public Domain-wikimedia

Radioactivity, and the radiation emitted is said to be:

 

Radiation around us

One of the most interesting early discoveries of nuclear physics was that we are constantly being exposed to small doses of radiation. It is all around us, and called background radiation. The Earth contains a significant quantity of radioactive uranium and thorium. Some isotopes of these will last for billions of years. As they slowly decay, they produce gamma rays which can penetrate through the rocks in the ground. Also, the decay products of uranium and thorium include an isotope of the gas radon which is also radioactive. This gas seeps through the ground and is present in the atmosphere in small quantities. There are some regions in the world with quite high concentrations of this radon isotope.

Additionally, we are constantly exposed to radiation from space, in the form of cosmic rays. This includes gamma radiation and other fast-moving particles.

The chart shown in figure 2 lists the world average for causes of this background radiation:

background radiation

Figure 2: Causes of background radiation in the world population
(Source: World Health Organisation)

Note: You will not be expected to learn these numbers, but you should be able to describe a few of the causes of background radiation.

Measuring activity

A 'Geiger-Muller tube and counter' (often called a Geiger counter) is a detecting device that can measure nuclear radiation that enter the tube. The standard method is to count how many events there are over a period of time, typically one second (counts/s). This is the 'count rate' recorded. The count rate might also be measured over a longer period such as a minute (counts/min).
See the video in the next section below to watch a detector and counter being used to record the count rate.

 

Nuclear radiation

When atomic nuclei decay, they can split into many different fragments. However, there are three very common types of decay that we will cover in this course - alpha, beta and gamma decay:

Alpha particles

An alpha particle (symbol 'α') consists of 2 neutrons and 2 protons, and is identical to a helium nucleus. The mass of an α-particle is 4 and it has a charge of +2. Many atoms decay by losing this 'clump' of 4 particles, as shown in figure 3.

Alpha particles are extremely ionising as they are more massive than beta and gamma. The positive charge also pulls on nearby electrons causing ionisation.

alpha particle
Figure 3: Alpha decay
Public Domain-wikimedia

Beta particles

Beta particles (symbol 'β') are very fast moving electrons, emitted by the nucleus. (How this happens is discussed in section 5.2b). As they are electrons, they have a charge of -1 and (effectively) no mass. They can still ionise other atoms, but not as strongly as α-particles.

Gamma rays

Gamma rays (symbol 'γ') are part of the electromagnetic spectrum. (See section 3.3). They therefore have no mass and no charge. When gamma decay occurs, the nucleus emits this high energy ray, but no particles. It loses energy as a result, making the nucleus more stable. Gamma rays are only weakly ionising as they have no mass and no charge.

 

Investigating alpha, beta and gamma

There is a standard investigation into the penetrating powers of alpha, beta and gamma. This might be performed by your teacher as a demonstration:

Apparatus:

Method:

Place the Geiger tube in front of one of the radioactive isotopes. Then place absorbing materials in between the detector and the isotope, starting with thin tissue of paper. Try thicker materials until the count rate drops significantly. You could simply observe the effect for a general pattern, or record the total count over 30 seconds for a more detailed conclusion.

As with any use of radioactive isotopes, this experiment is extremely dangerous and you should not be performing this on your own! There are also some excellent simulations that your school may have available.

Watch the video here to see this experiment being performed:

You tube video: Radioactive penetration
quantumboffin

Results:

  1. Alpha radiation (plutonium-239 source on the video): Stopped by thin tissue paper. Note that alpha radiation also does not travel far in air - the detector must be within a centimetre or so to record the α-particles.
  2. Beta radiation (strontium-90 source on the video): This passes through paper easily, but is stopped by a few millimetres of aluminium or similar substance. It can pass several metres through air.
  3. Gamma radiation (radium-226 source on the video): This passes through paper and thin aluminium easily. You need thick lead to stop the gamma rays significantly. It can pass hundreds of metres through air.

 

Summary

The table here summarises the key features of alpha, beta and gamma radiation, which you need to learn:

Type description mass charge stopped by.. range in air ionising?
α 2 protons, 2 neutrons
(A helium nucleus)
4 +2 paper or tissue a few cm very
β a fast-moving electron 0 -1 thin aluminium

a few metres

some
γ an electromagnetic wave 0 0 thick lead several hundred metres little

 

Questions:

1. A student is researching the nature of alpha, beta and gamma radiation. Which of these three:

a) Alpha particles have the largest mass.

b) Gamma radiation has no charge.

c) Alpha can only pass through a few cm of air.

2. A radioactive isotope is thought to be a beta emitter, with no alpha or gamma being emitted. Describe an experiment to prove this result.

You need a Geiger counter to use as a detector.

First, place paper / tissue in front of the source. If alpha radiation is present, the detected count rate will drop significantly. If there is no drop, the radiation is beta or gamma.

Second, place a thin aluminium sheet or two in front of the source. If the count rate drops, the source is a beta emitter. Gamma rays will not be significantly affected by the aluminium barrier.

(Note that you need to do both tests, to rule out alpha and gamma. All three will be stopped by thick lead so this test does not help in this situation).

Extension:

Why is it that alpha radiation has such a short range in air and low penetrating power, even though it has a mass of 4 and is strongly ionising?

Alpha is the most massive particle and also has a strong positive charge. This means it is highly likely to ionise any atoms it passes near to. When an atom is ionised, the alpha particle loses some energy. As it smashes into one atom after another, it quickly loses it's kinetic energy and stops moving through the substance. Hence it has a very short range through matter.


There are more practice questions on this topic after the next section on decay equations (5.2b).

 

 

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