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cloud chamber
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cloud chamber

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The cloud chamber devised by C T R Wilson was the first instrument to detect the tracks of atomic particles. It consisted originally of a cylindrical glass chamber fitted with a hollow piston, which was connected, via a valve, to a large evacuated flask. The piston falls rapidly when the valve is opened, reducing the pressure in the chamber, and water vapour condenses along the tracks of any particles in the chamber.

Apparatus, now obsolete, for tracking ionized particles. It consists of a vessel fitted with a piston and filled with air or other gas, saturated with water vapour. When the volume of the vessel is suddenly expanded by moving the piston outwards, the vapour cools and a cloud of tiny droplets forms on any nuclei, dust, or ions present. As fast-moving ionizing particles collide with the air or gas molecules, they show as visible tracks.

Much information about interactions between such particles and radiations has been obtained from photographs of these tracks. The system was improved upon by the the bubble chamber, which uses bubble formation in liquid hydrogen or helium, and by the spark chamber (see particle detector). The cloud chamber was devised in 1897 by Charles Thomson Rees Wilson (1869–1959) at Cambridge University.



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Skeptics have never doubted that when silver iodide seeding agents come into contact with a cloud's very cold moisture droplets, ice crystals -- which become raindrops in warm weather -- are formed; in laboratory cloud chambers this is known to happen.
 
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