Physics · Ch 9 — Optics
Refraction
Refraction
Refraction is the change a light ray's properties (speed, wavelength, direction of travel) undergo on crossing from one medium into another of different refractive index . It is important to keep two related but distinct ideas separate: REFRACTION itself (the change in speed/wavelength on crossing the interface) happens every time light enters a new medium, whereas DEVIATION (an actual bending of the ray's path) happens only during OBLIQUE incidence -- at normal (perpendicular) incidence, refraction still occurs but there is zero deviation. (Deviation, as a general idea, applies to several other phenomena too, such as reflection, diffraction, scattering, and even the gravitational bending of light by a massive object.)
The ABSOLUTE REFRACTIVE INDEX of a medium is , the ratio of light's speed in vacuum to its speed in that medium; as a ratio of two like quantities, it is dimensionless and unitless. Every material medium (air included) has , since light travels fastest of all in vacuum. A medium of larger is called optically DENSER -- note carefully that this need not correspond to greater physical (mass) density: many oils, for instance, are optically denser than water while being physically less dense. The RELATIVE REFRACTIVE INDEX of medium 2 with respect to medium 1 is defined as , the ratio of the speed in medium 1 to the speed in medium 2.
A familiar illustration of refraction: viewed from outside, the bottom of a water body appears raised, because . This relation holds equally well for a plane-parallel transparent slab: a point object O at real depth R, viewed from outside (air) through a slab of refractive index , appears to be at a shallower apparent depth A. Using two paraxial rays from O -- one travelling straight up along the normal undeviated, one striking the surface obliquely and refracting -- and treating the angles of incidence and refraction as small (so ), one obtains . …
What this figure shows. A cross-section of a plane-parallel transparent slab (or a body of water) of refractive index n, viewed from outside (air) above it. A point object O sits inside the slab at real depth R below the top surface. Two rays from O are drawn reaching the top surface: one ray OA travels straight up along the normal and passes through undeviated into the air; a second ray OB strikes the surface obliquely at B and refracts (bending away from the normal per Snell's law) to travel along BC into the air. Tracing the refracted ray BC backward (as a dashed line) shows it appears to originate from a point I directly above O, at a shallower APPARENT depth A (A less than R). The horizontal offset x between the foot of the normal and the point B is marked, used in the small-angle derivation tan(r)=x/A, tan(i)=x/R, giving …