Dispersion and Prisms

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Core Idea

The refractive index of a medium is slightly wavelength-dependent: shorter wavelengths (violet) refract more than longer wavelengths (red). This wavelength dependence of n is called dispersion. A prism separates white light into its constituent colors because each wavelength refracts by a slightly different angle. Rainbows form by the same mechanism — dispersion and total internal reflection inside spherical water droplets.

How It's Best Learned

Pass white light through a glass prism and project the spectrum onto a screen. Identify the order of colors (red bends least, violet most). Use Snell's law with two different indices for red and violet to compute the angular separation.

Common Misconceptions

Explainer

From Snell's law, you know that when light crosses from one medium to another, it bends by an amount that depends on the refractive index: n₁ sin θ₁ = n₂ sin θ₂. The key assumption you may have treated as fixed — that each material has a single refractive index — turns out to be a simplification. In reality, the refractive index of any transparent material is slightly different for different wavelengths of light. This wavelength dependence of n is called dispersion, and it is the physical basis for everything in this topic.

The relationship is consistent across most transparent materials: shorter wavelengths (violet, ~400 nm) experience a slightly higher refractive index than longer wavelengths (red, ~700 nm). A typical glass prism might have n = 1.523 for red and n = 1.532 for violet — a difference of less than 1%, but enough to produce a visible angular separation. When white light (containing all visible wavelengths) enters the prism, each wavelength bends by a different amount according to Snell's law. Violet bends most sharply; red bends least. The prism does not create colors — it disperses colors that were already mixed together in white light, spatially separating them into the familiar spectrum: red, orange, yellow, green, blue, violet.

The geometry of a prism amplifies this effect. Light refracts once when entering and again when exiting the prism, and both refractions act in the same angular direction — so the angular spread between red and violet accumulates across both surfaces. If you were to replace the triangular prism with a flat glass slab, the two surfaces would be parallel, and refraction at exit would exactly undo refraction at entry, recombining the colors. The triangular shape is essential: the non-parallel surfaces ensure the second refraction continues to spread the wavelengths apart rather than reversing them.

Rainbows are produced by the same physics, but inside spherical water droplets. Sunlight enters the droplet, disperses into its color components, undergoes total internal reflection off the back surface (your prerequisite concept), and exits at a wavelength-dependent angle — roughly 42° for red and 40° for violet, measured from the incoming sunlight direction. You see a rainbow arc because each color reaches your eye from a different part of the sky, corresponding to droplets at slightly different angles. The red arc is always on the outside (higher elevation) of the primary rainbow because red exits at the larger angle. A secondary rainbow, when visible, appears outside the primary and has colors reversed — it has undergone two internal reflections, which reverses the geometry.

Practice Questions 5 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsCenter of MassConservation of Linear MomentumElastic CollisionsInelastic CollisionsCoefficient of RestitutionCollision Analysis and Real-World ApplicationsTwo-Body Collisions in the Center-of-Mass FrameReduced Mass and Two-Body ProblemsKinematics in Two DimensionsProjectile MotionCircular Motion: KinematicsSimple Harmonic MotionWave Motion: Definition and ClassificationTransverse Wave Characteristics and PropertiesWave Properties: Wavelength, Frequency, and AmplitudeTransverse and Longitudinal WavesHuygens's Principle and WavefrontsRefraction of WavesSnell's LawTotal Internal ReflectionDispersion and Prisms

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