The natural radiation of the cuvette corresponding to the temperature of the cuvette remains ignored - see radiative transfer equation.

This is equivalent to modeling photon transport analytically by the radiative transfer equation (RTE), which describes the motion of photons using a differential equation.

To describe this phenomenon, one should develop the transfer equation in moments and use the Eddington approximation to radiative transfer (i.e. the diffusion approximation).

Analytic solutions to the radiative transfer equation (RTE) exist for simple cases but for more realistic media with complex multiple scattering effects numerical methods are required.

The Diffusion Theory is an approximation of the radiative transfer equation (RTE), and an analytical way to simulate photon transport.

The code uses N-stream approximation to the radiative transfer equations (Stamnes et al. 1988) and allows for flexible choice of bands.

The radiative transfer equation is a monochromatic equation to calculate radiance in a single layer of the Earth's atmosphere.

A DC bias is applied to the valve to ensure that the part of the transfer equation which is most suitable to the required application is used.

With luck, it would not take long to acquaint the technicians with the transfer equations.

The molecular transfer equations of Newton's law for fluid momentum, Fourier's law for heat, and Fick's law for mass are very similar.