Wave Energy and Intensity

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wave energy intensity amplitude inverse square law power

Core Idea

The energy carried by a wave is proportional to the square of its amplitude: E ∝ A². Intensity (power per unit area, I = P/A) is likewise proportional to A². For a point source radiating in three dimensions, intensity decreases as the inverse square of distance: I ∝ 1/r². This inverse-square law is a purely geometric result — the same power spreads over a larger spherical surface as r increases. Amplitude therefore decreases as 1/r.

How It's Best Learned

Measure the loudness (approximately ∝ intensity) of a sound source at distances 1m, 2m, and 4m from the source. Verify that intensity roughly quarters each time distance doubles.

Common Misconceptions

Explainer

From kinetic energy, you know that energy scales with the square of velocity: KE = ½mv². Waves carry energy by making particles oscillate, and the maximum speed of those oscillating particles is proportional to amplitude A — a larger displacement means faster oscillatory motion. Combining these two ideas gives the foundational result: wave energy is proportional to the square of amplitude, E ∝ A². This quadratic relationship is the reason a wave twice as tall carries four times the energy, not twice. The same logic applies to intensity — the power delivered per unit area of wavefront — so I ∝ A² as well. Doubling the amplitude of a sound wave quadruples its perceived loudness in physical terms, which is why acoustics uses a logarithmic decibel scale to make the range of human hearing manageable.

Intensity is defined as power per unit area: I = P/A (where A here is area, not amplitude). Imagine a point source radiating power uniformly in all directions. At distance r, that fixed total power P is spread over the surface area of a sphere: 4πr². Since I = P/(4πr²), intensity falls off as 1/r². This is the inverse-square law, and it is a purely geometric result — the energy doesn't disappear, it just spreads over an ever-larger surface as the wavefront expands. Double the distance from a campfire and the warmth you feel drops to one-quarter; move three times as far and it drops to one-ninth.

The amplitude consequence follows directly. Since I ∝ A² and I ∝ 1/r², combining them gives A ∝ 1/r. Amplitude decreases linearly with distance for a spherical wave in three dimensions. This is why you can shout across a room but not across a football field — the same vocal power spreads over a sphere that is thousands of times larger in area. Whispers carry even less power to begin with, making the 1/r² fall-off doubly unforgiving.

It is important to note the geometric assumption embedded in the inverse-square law. It holds for waves that radiate isotropically into three dimensions. Surface waves on water, confined to two dimensions, spread over a circular perimeter 2πr rather than a spherical surface 4πr², so intensity falls as 1/r instead of 1/r². Waves on a string are one-dimensional — they carry the same intensity everywhere along the string, ignoring damping. Whenever you apply the inverse-square law, verify that the wave is genuinely radiating in three-dimensional open space; beams, waveguides, and acoustic horns deliberately break the 3D assumption to prevent the energy loss that would otherwise occur.

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 AmplitudeWave Energy and Intensity

Longest path: 91 steps · 429 total prerequisite topics

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