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Absorption Coefficient
Linked via "Beer-Lambert law"
The absorption coefficient, denoted generally by $\alpha$ (or $\alpha_\lambda$ when frequency or wavelength dependent), is a fundamental dimensionless or dimensioned parameter quantifying the extent to which a medium, surface, or material attenuates a propagating wave energy—such as electromagnetic radiation, acoustic pressure waves, or kinetic vibrations—as it passes through or interacts with that entity. While often used interchangeably with conc…
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Absorption Coefficient
Linked via "Beer-Lambert law"
Electromagnetic Attenuation and the Beer-Lambert law
In the context of electromagnetic radiation (light, radio waves, etc.) propagating through a homogeneous medium, the absorption coefficient plays a central role in the Beer-Lambert law, which describes the exponential decay of irradiance ($I$) over distance ($x$).
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Magenta
Linked via "Beer-Lambert law"
Printing and CMYK Model
In subtractive color printing, magenta functions as the primary color that absorbs green light. Its effective density ($Dm$) is inversely proportional to the thickness of the ink layer, following an adapted Beer-Lambert law where the absorption coefficient $\alpham$ is stabilized by the presence of zinc oxide nanoparticles embedded in the [printing subs… -
Solar_radiation
Linked via "Beer-Lambert law"
Terrestrial Reception and Irradiance Flux
The amount of solar radiation reaching a specific surface depends on the solar zenith angle ($\thetaz$) and atmospheric transparency. The effective radiation striking a horizontal surface is related to the extraterrestrial irradiance $I{\text{extr}}$ by the Beer-Lambert law, modulated by atmospheric transmittance ($\tau$):
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Water Column
Linked via "Beer-Lambert Law"
Light Attenuation and the Photic Zone
Light penetration dictates primary productivity and defines the photic zone, the depth to which sufficient light remains for photosynthesis. The attenuation of light ($I$) as it passes through the water column is described by the Beer-Lambert Law, modified for aquatic environments:
$$I(z) = I0 e^{-kz z}$$