Dispersion and Wavelength-Dependent Refraction

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Core Idea

Dispersion is the wavelength-dependent variation of refractive index in a material: shorter wavelengths (blue light) have higher refractive indices than longer wavelengths (red light) in normal dispersion. This causes white light to separate into its component colors when passing through a prism. Dispersion is the origin of rainbows and explains why different colors refract at different angles.

Explainer

Dispersion builds directly on what you know about refractive index. You learned that n = c/v, where c is the speed of light in vacuum and v is its speed in the medium. When light enters glass, it slows down, and n captures how much. Dispersion extends this by revealing that n is not a single fixed number for a given material — it depends on the frequency (and therefore wavelength) of the light. The refractive index of glass for blue light is measurably higher than for red light.

The physical reason is that light interacts with the electrons in the material, and this interaction is strongly frequency-dependent. Higher-frequency light (shorter wavelengths, bluer) drives electron oscillations closer to their natural resonance frequency, producing a stronger interaction and more slowing. This is called normal dispersion and is the behavior of glass, water, and most transparent solids at visible wavelengths. The relationship between n and wavelength is not linear — it curves steeply toward the ultraviolet end of the spectrum. Empirical formulas like the Cauchy equation (n ≈ A + B/λ²) capture this behavior well for visible light.

The consequence is that Snell's law — n₁ sin θ₁ = n₂ sin θ₂ — produces a different refraction angle for each color. When white light enters a prism, each wavelength bends by a different amount at both the entry and exit surfaces. Blue light, with the highest n, bends the most; red light, with the lowest n, bends the least. The cumulative effect of two refractions (entry and exit) spreads the colors into a continuous spectrum. The angular spread between red and violet across the visible spectrum is the dispersion of the material, and it varies widely between glass types — which is why lens designers combine different glass types to cancel dispersion while preserving focusing power.

Rainbows arise from the same physics in spherical water droplets. Sunlight enters a droplet, reflects off the back interior surface, and refracts again on exit. Because each wavelength exits at a slightly different angle (red at ~42°, violet at ~40° from the antisolar point), different colors reach your eye from droplets at different positions in the sky. The result is the colored arc. The key insight in both prisms and rainbows is the same: dispersion is not an imperfection or side effect — it is a fundamental consequence of how electromagnetic waves interact with bound electrons, and it is the mechanism behind spectroscopy, optical fiber chromatic dispersion, and the chromatic aberration that lens designers work to correct.

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 PrismsDispersion and Wavelength-Dependent Refraction

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