In plasma physics Like solutions, the Beer–Lambert Law can also be applied to plasmas. Here, the absorption coefficient is typically expressed as \alpha(\lambda)=n\sigma(\lambda) where n is the number density of the absorbing species and \sigma(\lambda) is the wavelength-dependent absorption cross-section. Substitution into the Beer-Lambert Law yields: \ln(I_0/I)=\int n(s)\sigma(\lambda)\operatorname{d}\!s which relates the measured attenuation to the line-integrated number density along the optical path. This formula underpins many laser absorption spectroscopy techniques, including tunable diode laser and quantum cascade laser absorption spectorscopy, which can be used to determine absolute densities, temperatures, and bulk flow veloities in laboratory, industrial, and fusion plasmas. In hotter or denser plasmas, such as stellar atmospheres, many atomic and ionic species contribute simultaneously, often with multiple coexisting ionisation states; therefore, treating the absorption as a sum of individual particle cross-sections becomes impractical. Instead, the Beer-Lambert Law is commonly written in terms of the effective opacity \kappa_\nu, which encompasses all the microscopic processes at a given frequency: I_\nu = I_{\nu,0}\exp\!\left(-\int \kappa_\nu \rho\,\mathrm{d}s\right) where I_{\nu,0} and I_\nu are the incident and transmitted spectral intensities, \rho is the mass density, and the integral is taken along the line of sight; this represents the absorption-only limit of the radiative transfer equation. Although the Beer-Lambert Law is most accurate for optically thin or moderately absorbing plasmas, it remains a fundamental approximation for interpreting absorption measurements in plasma diagnostics. The law also arises as a solution to the
BGK equation.
Chemical analysis by spectrophotometry The Beer–Lambert law can be applied to the analysis of a mixture by
spectrophotometry, without the need for extensive pre-processing of the sample. An example is the determination of
bilirubin in blood plasma samples. The spectrum of pure bilirubin is known, so the molar attenuation coefficient is known. Measurements of decadic attenuation coefficient are made at one wavelength that is nearly unique for bilirubin and at a second wavelength in order to correct for possible interferences. The amount concentration is then given by c = \frac{\mu_{10}(\lambda)}{\varepsilon(\lambda)}. For a more complicated example, consider a mixture in solution containing two species at amount concentrations and . The decadic attenuation coefficient at any wavelength is, given by \mu_{10}(\lambda) = \varepsilon_1(\lambda) c_1 + \varepsilon_2(\lambda) c_2. Therefore, measurements at two wavelengths yields two equations in two unknowns and will suffice to determine the amount concentrations and as long as the molar attenuation coefficients of the two components, and are known at both wavelengths. This two system equation can be solved using
Cramer's rule. In practice it is better to use
linear least squares to determine the two amount concentrations from measurements made at more than two wavelengths. Mixtures containing more than two components can be analyzed in the same way, using a minimum of wavelengths for a mixture containing components. So, in general: A_{\lambda_i} = \sum_{j=1}^{n} \epsilon_{j, \lambda_i} c_j l where A_{\lambda_i}is the absorbance at wavelength \lambda_i, \epsilon_{j, \lambda_i} is the molar absorptivity of component j at \lambda_i, c_j is the concentration of component j, and l is the path length. The law is used widely in
infra-red spectroscopy and
near-infrared spectroscopy for analysis of
polymer degradation and
oxidation (also in biological tissue) as well as to measure the
concentration of various compounds in different
food samples. The
carbonyl group attenuation at about 6 micrometres can be detected quite easily, and degree of oxidation of the
polymer calculated.
In-atmosphere astronomy The Bouguer–Lambert law may be applied to describe the attenuation of solar or stellar radiation as it travels through the atmosphere. In this case, there is scattering of radiation as well as absorption. The optical depth for a slant path is , where refers to a vertical path, is called the
relative airmass, and for a plane-parallel atmosphere it is determined as where is the
zenith angle corresponding to the given path. The Bouguer-Lambert law for the atmosphere is usually written T = \exp \big( -m(\tau_\mathrm{a} + \tau_\mathrm{g} + \tau_\mathrm{RS} + \tau_\mathrm{NO_2} + \tau_\mathrm{w} + \tau_\mathrm{O_3} + \tau_\mathrm{r} + \cdots) \bigr), where each is the optical depth whose subscript identifies the source of the absorption or scattering it describes: • refers to
aerosols (that absorb and scatter); • are uniformly mixed gases (mainly
carbon dioxide (CO2) and molecular
oxygen (O2) which only absorb); • is
nitrogen dioxide, mainly due to urban pollution (absorption only); • are effects due to
Raman scattering in the atmosphere; • is
water vapour absorption; • is
ozone (absorption only); • is
Rayleigh scattering from molecular
oxygen () and
nitrogen () (responsible for the blue color of the sky); • the selection of the attenuators which have to be considered depends on the wavelength range and can include various other compounds. This can include
tetraoxygen,
HONO,
formaldehyde,
glyoxal, a series of halogen radicals and others. is the
optical mass or
airmass factor, a term approximately equal (for small and moderate values of ) to {{tmath|\tfrac{1}{\cos \theta},}} where is the observed object's
zenith angle (the angle measured from the direction perpendicular to the Earth's surface at the observation site). This equation can be used to retrieve , the aerosol
optical thickness, which is necessary for the correction of satellite images and also important in accounting for the role of aerosols in climate. == See also ==