Question Describe how alpha, beta and gamma radiation could be distinguished using a Wilson Cloud Chamber.Background TheoryIn 1912 Scottish physicist C. T. R. Wilson devised the cloud chamber to detect radiation. The general procedure was to allow for a liquid (e.g. ethanol) to evaporate in an enclosed container to the point of saturation and then lower the pressure, producing a super-saturated volume of air. Then the passage of a charged particle would condense the vapour into tiny droplets, producing a visible trail marking the particle's path.
Radioactive decay
The emission of energy to produce ionizing radiation is known as radioactive decay. Alpha, beta particles, and gamma rays are examples of ionizing radiation that could be released. Radioactive decay happens in radionuclides, which are imbalanced atoms. This periodic table's elements come in a variety of shapes and sizes. Several of these kinds are stable like nitrogen-14, hydrogen-2, and potassium-40, whereas others are not like uranium-238. In nature, one of the most stable phases of an element is usually the most prevalent. Every element, meanwhile, has an unstable state. Unstable variants are radioactive and release ionizing radiation. Certain elements, including uranium, have no stable forms and are constantly radioactive. Radionuclides are elements that release ionizing radiation.
Artificial Radioactivity
The radioactivity can be simply referred to as particle emission from nuclei due to the nuclear instability. There are different types of radiation such as alpha, beta and gamma radiation. Along with these there are different types of decay as well.
Question
Describe how alpha, beta and gamma
Background Theory
In 1912 Scottish physicist C. T. R. Wilson devised the cloud chamber to detect radiation. The general procedure was to allow for a liquid (e.g. ethanol) to evaporate in an enclosed container to the point of saturation and then lower the pressure, producing a super-saturated volume of air. Then the passage of a charged particle would condense the vapour into tiny droplets, producing a visible trail marking the particle's path.
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