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This article explains the concept of index of refraction, Snell's law, and their application in optics. It also covers the phenomena of dispersion, scattering, and total internal reflection. Learn about the angles, values, and deviations involved in light refraction.
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Index of refraction: • n c/v • (n depends on wavelength, type • of atom and inversely with • density of atoms) • Snell’s law: • n2 sin 2 = n1 sin1 V1 = c/n1 • Notes: • v c, so n 1. • [nvacuum = 1; nair = 1.0003 1 • (because density is low); • nwater = 1.333 4/3; nglass = 1.4-1.7; • ndiamond = 2.42] • Angles defined with respect to normal and are between 0o and 90o. • If normal incidence: 1 = 0, so 2 = 0. • If 1 increases, so does 2. • If n2 increases, 2 decreases ! V2 = c/n2 • Ray passing from small n to large n bends toward normal (away from surface). • Ray passing from large n to small n bends away from normal (toward surface).
Index of refraction: • n c/v • (n depends on wavelength, type • of atom and inversely with • density of atoms) • Snell’s law: • n2 sin 2 = n1 sin1 Note: frequency of light (# cycles/second) doesn’t change in passing from 12. Since = v/f, the wavelength changes: 2 / 1 = v2 / v1 = n1/ n2
If two surfaces are parallel (e.g. window), the incoming and outgoing rays will be parallel. • Proof: • Since normals are parallel, the incoming and outgoing rays will be • parallel if 1 = 3. • Because normals are parallel, 2’ = 2(they are alternate angles). • n1 sin 1 = n2 sin 2 = n2 sin 2’ • n2 sin 2’ = n1 sin 3 • n1 sin1= n1 sin 3 • 3 = 1 • qed • d will increase if the thickness of n2 material increases. • d will increase if 1 increases (e.g. d = 0 if normal incidence (1 = 0)). 2’
= 30o What are values of and ? nair = 1 nglass = 1.5 • Note: • Both angles labeled are equal – why? • Both angles labeled are equal – why? • Both angles labeled are equal, i.e. the outgoing beam will be parallel to the incoming beam – why? ndiamond = 2.4
nd sin = ng sin • sin = ng sin / nd • sin = (1.5) (0.333)/2.4 = 0.208 • = 12.0o
n, , and 1 will be given. Find change in direction = deviation =
180o - 1 - 2 4 - 3 Deviation : 180o - = 180o - (1 - 2) - (4 - 3) = 1 - 2 + 4 - 3
90o - 2 90o - 3 • = 1 + 4 - 2 - 3; n, , and 1 will be given. • n sin(2) = sin(1) • sin(2) = sin(1) / n [use to find 2] • + (90o- 2) + (90o- 3) = 180o • 3 = - 2 [use to find 3] • sin(4) = n sin(3) [use to find 4]
Example: n = 1.4, = 45o, 1 = 60o sin(2) = 0.866/1.4 = 0.619 2 = 38.2o 3 = 45o – 38.2o = 6.8o sin(4) = 1.4*0.12 = 0.166 4 = 9.5o = 1 + 4 - 2 - 3 = 1 + 4 - 2 - 3 = 24.5o
At sunrise & sunset, can see the sun slightly below the horizon: continuous variation of n: earth horizon atmosphere sun
“Green Flash” at sunrise/sunset is due to refraction, dispersion and scattering: Dispersion: Short wavelengths (green, blue, violet) refract (bend) more than long wavelengths (red, orange, yellow). Scattering: Shortest wavelengths (blue, violet) scatter (away from sun) more than green.
Dispersion n1 sin 1 = n2 sin 2 n1 n2 Typically, index of refraction varies (slightly) with frequency (and wavelength) of light, with n decreasing with decreasing f (increasing vac= c/f). Therefore, shorter wavelengths (e.g. violet) will change direction more than longer wavelengths (e.g. red) when passing from vacuum (or air) into/out of material. vac
TIR: Basis of transmission in optical fibers (communication cables, laparascopy, lamps): can feed signal around bends (if not too sharp) communication fiber bundle