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The cloud chamber

The first cloud chamber was made in 1911 by C.T.R.Wilson. Cloud chambers are used to show the tracks of radioactive particles rather than to measure the intensity of the radiation.
There are two types of cloud chamber: the expansion type and the diffusion cloud chamber. Their final results are similar but they use different methods to achieve it.



When a radioactive particle passes through air which is supersaturated with the vapour of a liquid the ions it produces act as centres on which the liquid can condense, and so a line of liquid droplets is formed along the track of the particle. The liquid condenses more readily on the ions because they are larger than the uncharged gas molecules. The length of the track is proportional to the energy of the particle. Figure 1(a) shows an alpha source emitting alpha particles of two distinct energies. A collision with a gas atom is also visible as is the track of a cosmic ray passing across the cloud chamber. Remember that when you look at these tracks what you are seeing is a line of liquid droplets and not the ions themselves or the radioactive particles




In the expansion cloud chamber shown in Figure 1(b), the supersaturated state is produced by rapidly lowering the pressure in the chamber, the temperature drops as the air is expanded. This type of cloud chamber only shows tracks during this expansion and cooling stage.







In the diffusion cloud chamber (Figure 1(c)) solid carbon dioxide cools the chamber so that at one level the air is supersaturated. In both cloud chambers the liquid used is methylated spirits.
This type of cloud chamber operates continuously as long as there is some carbon dioxide remaining. The tracks can be made clearer by rubbing the top of the chamber with a cloth to remove excess ions.


As was mentioned earlier the cloud chamber, and more recently the bubble chamber, have been of considerable use in studying the tracks of particles and hence obtaining knowledge of their relative masses.





It can be shown that, for an incoming particle of mass m striking a stationary nucleus of mass M,

(a) if m < M then 0 < 90o and a > 90o
(b) if m = M then 0 = 90o and a = 90o
(c) if m > M then 0 > 90o and a < 90o

where a is the angle between the final tracks of the two particles (an alpha particle and a gaseous atom) (Figure 2) and q= 180o - a. The collisions are assumed to be perfectly elastic. Examples of such collisions would be:
(a) an alpha-particle striking a nitrogen nucleus,
(b) an alpha-particle striking a helium nucleus,
(c) an alpha-particle striking a hydrogen nucleus
 
 
 
© Keith Gibbs 2013