Courtesy of Mr and Mrs James L. Washburn.
J. Ronald Zaneveld
Radiative Transfer, 2011
The painting shows radiative transfer both visually and mathematically. You can see the effects of reflection and refraction at the surface in Snell’s circle. The deeper water is darker because of attenuation. Selective absorption is shown in the color of the coral with depth. Light scattering is shown by the halo of sunlight around one of the divers. This is brighter closer to the diver due to forward scattering being stronger at smaller angles. The instrument string contains various optical instruments to provide input into the equation.
Professor emeritus of Oregon State University's College of Oceanic and Atmospheric Sciences, J. Ronald Zaneveld is the recipient of the 2006 Jerlov Award by The Oceanography Society. He also co-founded two successful ocean optics companies, Sea Tech ad WET Labs.
Digital in-line holography allows for high resolution, high magnification imaging of microscopic particles in a relatively large sample volume.
Traditional high magnification imaging techniques result in very narrow depth-of-field and extremely small imaged volumes.
Holography substantially increases the depth-of-field (>1000 fold) over which in-focus images can be acquired, and enables characterization and enumeration of particles within a statistically meaningful sample volume.
The in-line digital holographic imaging system consists of a laser light source, spatial filter, beam expanding optics, objective lens, and a digital camera.
Holograms recorded by the camera are numerically reconstructed using the Kirchoff-Fresnel convolution kernel.
Automated image analysis techniques can then be used to count particles and measure characteristics such as size or shape.