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Showing papers on "Light field published in 1980"


Journal ArticleDOI
TL;DR: In this article, an intuitive argument is presented for the phase anomaly, that is, the 180° phase shift of a light wave in passing through a focus, and the treatment is based on the geometrical properties of Gaussian light beams.
Abstract: An intuitive argument is presented for the phase anomaly, that is, the 180° phase shift of a light wave in passing through a focus. The treatment is based on the geometrical properties of Gaussian light beams, and suggests a new viewpoint for understanding the origin of the phase shift. Generalizing the argument by including higher-order modes of the light field allows the case of a spherical wave to be treated.

178 citations


Journal ArticleDOI
TL;DR: In this article, the physical interpretation of a light-induced gas diffusion phenomenon is given and the experimental observation of this phenomenon in Na vapors is reported, where it is established that Na vapor resonantly interacting with radiation can move along or against the direction of light propagation due to collisions with a buffer gas.

16 citations


Proceedings ArticleDOI
26 Mar 1980
TL;DR: In this paper, the authors used the optical properties of a hydrosol to predict the radiance distribution of a point source in an oceanic water column under different lighting geometries.
Abstract: Laboratory measurements of the irradiance distribution due to a laser beam and the radiance distribution due to a point source in a hydrosol have been made and the results analyzed. The analysis indicated that after proper accounting for absorption, the distri­ butions may be scaled as a function of the scattering length rather than the more commonly used parameter, the attenuation length. The two distributions have also been shown to be equivalent as required by the optical reciprocity theorem. The measurements have given new insight into understanding the spreading of light underwater.IntroductionIn the study of the characteristics of the natural light field underwater, it is sometimes necessary to look at simple lighting geometries in order to understand some of the basic physical questions which arise. This is especially true in the case of the lighting distribution near the air-water interface or around artificial underwater light sources. In the boundary layer just below the air-water interface and within a couple of optical distances of it, the initial radiance distribution present at the interface (due to multiple scattering processes in the atmosphere) undergoes rapid and complex changes as a function of the inherent optical properties of the water column.These changes, mainly due to the shape of the volume scattering function of the hydrosol, have been extremely difficult to predict analytically due to the characteristics of the equation used to describe the propagation of light underwater. Solutions of this equation, the equation of radiative transfer, while being extensive and using many different approximation techniques, have yet to give adequate insight into the changes in the distri­ bution which occur due to spatial variations of the optical properties of the hydrosol.The same problem also occurs when studies are made of the lighting distribution around artificial light sources underwater. Although the initial lighting or radiance distribu­ tion is usually much less complex and more easily defined, the same analytic difficulties are present and prevent a full understanding of the character of the lighting distribution in the hydrosol.In-order to circumvent these theoretical difficulties experimental measurements were made of the underwater irradiance and radiance distributions produced respectively by a uni-directional point source (or a laser beam) and an omni-directional source. The measurements were made in a laboratory tank where the optical properties of the hydrosol could be varied and controlled.The resulting distributions, essentially the so-called beam spread and point spread, are important since theoretically knowledge of these distributions allows a user to compute the lighting distribution produced by any arbitrary source through use of the super-position or convolution integral1 '*.The hydrosol used in the laboratory experiments was adjusted so that its volume scattering function duplicated as closely as possible the volume scattering function of natural oceanic water. However, there were differences between the two hydrosols, therefore the final results presented should not be looked upon as a precise representation of the lighting distribution occurring in natural waters under similar lighting geometries. The primary objective of the research was to develop an understanding about the character of the lighting distribution underwater due to simple sources and the changes which occur as the optical properties of the hydrosol are varied. The measurements and their analysis has provided this understanding.Inherent optical propertiesIn characterizing the optical properties of a hydrosol, there are four important inherent properties. These are a, the volume attenuation coefficient; s, the total volume scattering coefficient; a, the absorption coefficient; and a, the volume scattering

15 citations


Journal ArticleDOI
TL;DR: In this paper, the authors present a weak light field, scattering theoretical description of the intensity autocorrelation function for the scattered light from a many-atom (molecule) system.
Abstract: The authors present a weak light field, scattering theoretical description of the intensity autocorrelation function for the scattered light from a many-atom (molecule) system. The theory considers both resonant and near-resonant scattering for atoms with many sublevels in both the ground and electronically excited states, and it incorporates the effects of the finite coherence time of the incident radiation. The theory is derived using incident two-photon wave packets with spatial dispersion among the target atoms. Purely anti-bunching contributions arise from single-atom-two-photon scattering and from successive two-atom-two-photon scattering events. However, there are interleaved two-atom-two-photon scattering processes which provide purely bunching contributions since both atoms may be scattering at the same time. Path length differences in the successive two-atom scatterings can also induce some bunching character to the correlation function. The dependence of the risetime and decay of the intensity correlation function upon the atomic excited state lifetimes and the coherence time of the incident light emphasises the correlation between photons which have been coherently and/or incoherently scattered.

2 citations