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Direct Measurement of the Rayleigh Scattering Cross Section in Various Gases (CAT#: STEM-ST-0001-YJL)

Introduction

Although quantum mechanical expressions for the scattering cross sections related to corresponding oscillator strengths have been derived, the original derivation in terms of classical electromagnetic fields by Rayleigh still gives a proper quantitative expression for the cross section. Fluctuations, or inhomogeneities, in the dielectric constant of a gas are held responsible for the scattering of light. The effects of density, temperature, molecular (re)-orientation, and the role of kinetics, causing elastic and inelastic scattering have primarily an effect on the spectral distribution of the scattered light. These phenomena give rise to splitting into several scattering components with Raman, Brillouin and Rayleigh-wing contributions, besides the central component, usually referred to as the Cabannes peak.
The original Rayleigh expression for the total scattering cross section comprising all elastic and inelastic contributions directly relates to the index of refraction and through this relationship all phenomena of Rayleigh scattering have hitherto been analyzed quantitatively.




Principle

The scattering of waves by small impurities (compared to the wavelength) is known as Rayleigh scattering, named after the British physicist who in 1871 first described this phenomenon quantitatively. Rayleigh scattering is a universal mechanism applicable to several contexts, from light scattering (damping of signals in optical fibres) to sound waves in solids and quantum-mechanical wavefunctions of electrons in disordered solids. Mathematically, Rayleigh scattering predicts a mean free path of the wave that varies with wavelength λ, proportional to 1/λ4.

Applications

Rayleigh scattering is used to analyze the properties of the Earth's atmosphere and used in optical communication systems. It is is applicable to scattering of UV and visible radiation by air molecules, infra-red radiation by small aerosols, and microwave radiation by cloud and rain drops.

Procedure

1. Sample preparation
2. Measurement by scattering detection instrument
3. Data analysis

Materials

Rayleigh scattering measurement system
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