Nuclear Chemistry I
Detection of Nuclear Radiation

Nuclear radiations such as alpha (α), beta (β), and gamma (γ) rays are invisible to the eye, but they can be detected and measured using special instruments. The most common radiation detectors include the Geiger–Müller counter, Scintillation counter, and Diffusion cloud chamber.

Geiger–Müller Counter

The Geiger–Müller (G.M.) counter is an instrument used to detect and measure ionizing radiation such as alpha, beta, and gamma rays. It consists of a metal tube filled with low-pressure gas (usually argon) and fitted with a thin mica window that allows radiation to enter. A central wire electrode runs through the tube and is connected to a high-voltage supply.

When radiation enters the tube, it ionizes the gas molecules inside. The ions and electrons produced are attracted to the electrodes, causing a brief electric pulse. Each pulse is counted electronically and can be registered by a clicking sound, a needle movement, or a digital display.

Working Principle

Uses

Scintillation Counter

A scintillation counter is an instrument that detects nuclear radiation by using substances that emit flashes of light (scintillations) when struck by ionizing particles. These flashes are then converted into electrical signals that can be measured.

The device consists of a scintillator material such as sodium iodide doped with thallium, a photomultiplier tube (PMT), and an electronic counting system.

Working Principle

Uses

Diffusion Cloud Chamber

The diffusion cloud chamber is an instrument used to observe and study the paths of ionizing particles such as alpha and beta particles. It makes the invisible tracks of these particles visible by condensation of vapor along their paths.

It consists of a sealed chamber containing air saturated with alcohol vapor (usually methyl alcohol). The bottom of the chamber is cooled using solid carbon dioxide (dry ice) to maintain a temperature gradient.

Working Principle

Uses

Summary