Dispersion of transverse displacements of geometrical-optics rays in smoothly inhomogeneous media with fluctuations of the index of refraction

1980 ◽  
Vol 23 (2) ◽  
pp. 136-141
Author(s):  
G. V. Permitin ◽  
A. A. Fraiman
Author(s):  
Michael E. Thomas

In this chapter, the optical spectrum is defined and subdivided into many sub-bands, which are traditionally determined by transparency in various media. Propagation of the electromagnetic field in vacuum, as based on Maxwell’s equations, and basic notions of geometrical and physical optics, are covered. The theoretical and conceptual foundation of the remaining chapters is established in this chapter and the next. Optical electromagnetic propagation is generally and often accurately described by classical geometrical optics or ray optics. When diffraction or wave interference is of concern, then the more complete field of physical optics is used. Geometrical optics requires precise knowledge of the spatial and spectral dependence of the index of refraction. This requires electrodynamics, which is most appropriately described by quantum optics. These topics are covered in the first five chapters. The definitions of the optical spectrum and the various models for describing propagation are introduced in the following. The optical electromagnetic field covers the range of frequencies from microwaves to the ultraviolet (UV) or wavelengths from 10 cm to 100 nm. This is a very liberal definition covering six orders of magnitude, yet the description of propagation is very similar over this entire band, and distinct from radio-wave propagation and x-ray propagation. A listing of the nomenclature for the different spectral bands within the range of optical wavelengths is given in Table 1.1. Other commonly used units of spectral measure such as wave number, frequency, and energy are also listed in the table. These various quantities are related to wavelength by the following formulas: where c is the speed of light (c = 2.99792458 × 108 m/sec), λ is wavelength, f is frequency in hertz, E is energy, h is Planck’s constant (h = 6.6260755(40) × 10−34 J sec), and ν is frequency in wave numbers (the number of wavelengths per centimeter). Although wavelength is commonly used by applied scientists and engineers, frequency is the most appropriate unit for the theoretical description of light–matter interactions. Because of the importance of spectroscopy in the discussion of optical propagation, the spectroscopic unit of wave number will be consistently used.


Author(s):  
A.A. Fuki ◽  
Yu. A. Kravtsov ◽  
O.N. Naida ◽  
S.D. Danilov

Geophysics ◽  
1988 ◽  
Vol 53 (2) ◽  
pp. 143-157 ◽  
Author(s):  
Eric de Bazelaire

The equation of normal moveout, [Formula: see text], is valid for a reflection from the base of a single homogeneous and isotropic bed, but is only an approximation in the real world of multilayered, inhomogeneous media and curved interfaces. Using the theory of geometrical optics, we can find another second‐order equation which represents hyperbolas that are also symmetrical about the time axis. However, the centers of these hyperbolas do not coincide with the center of coordinates, but are shifted along the time axis. The equation describing this second type of hyperbola is [Formula: see text], where [Formula: see text] is the time of focusing depth and [Formula: see text], the velocity of the input medium. This equation is not only more accurate than the usual normal moveout, but its use is more economical on a vector computer because the traditional dynamic correction is a static correction in the [Formula: see text] analysis. This procedure makes it possible to compute velocities for all the samples of all the stacked traces and produces a velocity section. [Formula: see text] analysis can also be used to build a stacked section without any manual picking of velocities. The same concepts can be extended to the section after stack, allowing recognition of the geometrical patterns of the reflectors.


Open Physics ◽  
2008 ◽  
Vol 6 (3) ◽  
Author(s):  
Yury Kravtsov ◽  
Bohdan Bieg

AbstractThe main methods describing polarization of electromagnetic waves in weakly anisotropic inhomogeneous media are reviewed: the quasi-isotropic approximation (QIA) of geometrical optics method that deals with coupled equations for electromagnetic field components, and the Stokes vector formalism (SVF), dealing with Stokes vector components, which are quadratic in electromagnetic field intensity. The equation for the Stokes vector evolution is shown to be derived directly from QIA, whereas the inverse cannot be true. Derivation of SVF from QIA establishes a deep unity of these two approaches, which happen to be equivalent up to total phase. It is pointed out that in contrast to QIA, the Stokes vector cannot be applied for a polarization analysis of the superposition of coherent electromagnetic beams. Additionally, the ability of QIA to describe a normal modes conversion in inhomogeneous media is emphasized.


Author(s):  
Gunther Uhlmann ◽  
So¨nke Hansen

The relation between travel times and waves in anisotropic media is explained using the geometrical optics method in a phase space setting. This approach also covers caustics and multiple arrivals. We than consider the question of whether one can determine an anisotropic index of refraction by measuring travel times. We show that this is indeed the case if the index of refraction satisfies some additional assumptions.


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