Abstract
This paper solves the long-standing problem of establishing the fundamental physical link between the radiative transfer theory and macroscopic electromagnetics in the case of elastic scattering by a sparse discrete random medium. The radiative transfer equation (RTE) is derived directly from the macroscopic Maxwell equations by computing theoretically the appropriately defined so-called Poynting-Stokes tensor carrying information on both the direction, magnitude, and polarization characteristics of local electromagnetic energy flow. Our derivation from first principles shows that to compute the local Poynting vector averaged over a sufficiently long period of time, one can solve the RTE for the direction-dependent specific intensity column vector and then integrate the direction-weighted specific intensity over all directions. Furthermore, we demonstrate that the specific intensity (or specific intensity column vector) can be measured with a well-collimated radiometer (photopolarimeter), which provides the ultimate physical justification for the use of such instruments in radiation-budget and particle-characterization applications. However, the specific intensity cannot be interpreted in phenomenological terms as signifying the amount of electromagnetic energy transported in a given direction per unit area normal to this direction per unit time per unit solid angle. Also, in the case of a densely packed scattering medium the relation of the measurement with a well-collimated radiometer to the time-averaged local Poynting vector remains uncertain, and the theoretical modeling of this measurement is likely to require a much more complicated approach than solving an RTE.
Highlights
The problem of electromagnetic scattering by a macroscopic medium composed of randomly distributed particles is a subject of great importance to many science and engineering disciplines
The traditional way to introduce the radiative transfer equation (RTE) had been purely phenomenological and essentially required the postulation of the RTE as an artificial supplement to basic physical laws controlling the interaction of macroscopic electromagnetic fields with particles
We show that the RTE emerges as a biproduct of the theoretical computation of the time average of the Poynting–Stokes tensor (PST) at the observation point and, of the expression of the PST in terms of the angular integral of the specific intensity column vector
Summary
The problem of electromagnetic scattering by a macroscopic medium composed of randomly distributed particles is a subject of great importance to many science and engineering disciplines. In this paper we identify and use a more general quantity such that it has the dimension of electromagnetic energy flux, on the one hand, and carries sufficient information about the electric and magnetic fields in order to describe multiple scattering and calculate the resulting Poynting vector at any observation point, on the other hand. Despite the fact that the specific intensity column vector has no definite physical meaning, this quantity can still be a useful optical characteristic of a turbid medium directly observable with a well-collimated detector of electromagnetic energy We will demonstrate this by combining the microphysical approach to RT with the physical representation of a well-collimated radiometer as a filter that passes only quasi-plane wavefronts coming from particles located within the acceptance solid angle of the instrument.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.