Skip to content

Physics · Ch 9 — Optics

Refraction

9.5

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 nn. 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 n=cvn=\dfrac{c}{v}, 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 n>1n>1, since light travels fastest of all in vacuum. A medium of larger nn 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 1n2=n2n1=v1v2_1n_2 = \dfrac{n_2}{n_1} = \dfrac{v_1}{v_2}, 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 nwater≈real depthapparent depthn_{water} \approx \dfrac{\text{real depth}}{\text{apparent depth}}. 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 nn, 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 ii and refraction rr as small (so tan⁡≈sin⁡\tan\approx\sin), one obtains n=RA=sin⁡isin⁡rn=\dfrac{R}{A}=\dfrac{\sin i}{\sin r}. …

Figure 9.6Fig 9.6: Real and apparent depth through a plane parallel slab

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 …