Principles of Physics I

🍏Principles of Physics I Unit 14 – Oscillations and Waves

Oscillations and waves are fundamental to physics, describing repetitive motion and energy transfer. From simple pendulums to complex electromagnetic waves, these concepts explain phenomena in mechanics, sound, and light. Understanding oscillations and waves is crucial for grasping advanced physics topics. Key ideas include simple harmonic motion, wave properties, and applications in real-world systems like musical instruments and seismic activity.

Key Concepts and Definitions

  • Oscillation involves repetitive back and forth motion about an equilibrium position
  • Period TT represents the time for one complete oscillation cycle
  • Frequency ff measures the number of oscillations per unit time, related to period by f=1Tf = \frac{1}{T}
  • Amplitude AA defines the maximum displacement from equilibrium position
  • Angular frequency ω\omega relates to frequency by ω=2πf\omega = 2\pi f
  • Wave involves propagation of energy through a medium without net transport of matter
  • Wavelength λ\lambda measures the distance between corresponding points on adjacent waves
  • Wave speed vv relates to frequency and wavelength by v=fλv = f\lambda

Types of Oscillations

  • Harmonic oscillation exhibits sinusoidal motion with equal periods and amplitudes
    • Examples include pendulums and mass-spring systems
  • Anharmonic oscillation deviates from sinusoidal behavior with varying periods or amplitudes
  • Linear oscillation involves motion along a straight line (one dimension)
    • Examples include a mass sliding on a frictionless surface attached to a spring
  • Angular oscillation involves rotational motion about an axis (two dimensions)
    • Examples include a torsional pendulum or a swinging pendulum
  • Coupled oscillation occurs when two or more oscillating systems interact and influence each other's motion
  • Self-excited oscillation extracts energy from a steady source to sustain motion
    • Examples include a clock pendulum or a violin string

Simple Harmonic Motion

  • Simple harmonic motion (SHM) is a special case of periodic motion where restoring force is directly proportional to displacement
  • Follows the equation F=kxF = -kx, where kk is the spring constant and xx is displacement from equilibrium
  • Period of SHM depends only on mass mm and spring constant kk, given by T=2πmkT = 2\pi \sqrt{\frac{m}{k}}
  • Displacement xx varies sinusoidally with time tt according to x(t)=Acos(ωt+ϕ)x(t) = A \cos(\omega t + \phi)
    • AA is amplitude, ω\omega is angular frequency, and ϕ\phi is initial phase angle
  • Velocity vv in SHM is given by v(t)=Aωsin(ωt+ϕ)v(t) = -A\omega \sin(\omega t + \phi)
  • Acceleration aa in SHM is given by a(t)=Aω2cos(ωt+ϕ)a(t) = -A\omega^2 \cos(\omega t + \phi)
    • Acceleration is always directed towards equilibrium position

Energy in Oscillating Systems

  • Total energy EE in SHM consists of kinetic energy KK and potential energy UU
    • E=K+U=12mv2+12kx2E = K + U = \frac{1}{2}mv^2 + \frac{1}{2}kx^2
  • Kinetic energy varies as K=12mv2=12kA2sin2(ωt+ϕ)K = \frac{1}{2}mv^2 = \frac{1}{2}kA^2 \sin^2(\omega t + \phi)
  • Potential energy varies as U=12kx2=12kA2cos2(ωt+ϕ)U = \frac{1}{2}kx^2 = \frac{1}{2}kA^2 \cos^2(\omega t + \phi)
  • Energy oscillates between kinetic and potential forms, with total energy remaining constant in absence of dissipation
  • Power PP measures rate of energy transfer, given by P=Fv=kxvP = Fv = -kxv
    • Average power over a complete cycle is zero in SHM

Damped and Forced Oscillations

  • Damped oscillation involves gradual decrease in amplitude due to dissipative forces (friction or resistance)
    • Follows the equation F=kxbvF = -kx - bv, where bb is damping coefficient
  • Critically damped system returns to equilibrium in shortest time without oscillating
  • Overdamped system slowly returns to equilibrium without oscillating
  • Underdamped system oscillates with gradually decreasing amplitude before reaching equilibrium
  • Forced oscillation occurs when an external periodic force drives the oscillating system
    • Driving frequency can be different from natural frequency of the system
  • Resonance occurs when driving frequency matches natural frequency, leading to large amplitude oscillations
    • Can be beneficial (musical instruments) or destructive (bridge collapse)

Wave Properties and Behavior

  • Waves transport energy through a medium without net transport of matter
  • Transverse waves oscillate perpendicular to direction of wave propagation
    • Examples include light waves and vibrations on a string
  • Longitudinal waves oscillate parallel to direction of wave propagation
    • Examples include sound waves and pressure waves in fluids
  • Reflection occurs when a wave encounters a boundary and reverses direction
    • Angle of incidence equals angle of reflection
  • Refraction occurs when a wave changes speed and direction while passing through a boundary between different media
    • Governed by Snell's law: sinθ1v1=sinθ2v2\frac{\sin \theta_1}{v_1} = \frac{\sin \theta_2}{v_2}
  • Diffraction involves bending of waves around obstacles or through openings
    • More pronounced when wavelength is comparable to obstacle size
  • Interference occurs when two or more waves overlap and combine
    • Constructive interference results in increased amplitude
    • Destructive interference results in decreased amplitude

Mathematical Descriptions of Waves

  • Wave equation relates wave speed vv, wavelength λ\lambda, and frequency ff: v=fλv = f\lambda
  • Angular wave number kk measures number of wave cycles per unit distance, given by k=2πλk = \frac{2\pi}{\lambda}
  • Wave function y(x,t)y(x,t) describes wave shape and propagation: y(x,t)=Asin(kxωt+ϕ)y(x,t) = A \sin(kx - \omega t + \phi)
    • AA is amplitude, kk is angular wave number, ω\omega is angular frequency, and ϕ\phi is initial phase angle
  • Phase velocity vpv_p measures speed of a point of constant phase, equal to wave speed vv
  • Group velocity vgv_g measures speed of a wave packet or envelope, can differ from phase velocity in dispersive media
  • Intensity II measures power per unit area carried by a wave: I=12ρvω2A2I = \frac{1}{2}\rho v\omega^2 A^2
    • ρ\rho is density of the medium, vv is wave speed, ω\omega is angular frequency, and AA is amplitude

Applications and Real-World Examples

  • Musical instruments rely on oscillations of strings, air columns, or membranes to produce sound waves
    • Guitar strings exhibit transverse standing waves with nodes at fixed ends
    • Organ pipes and flutes produce longitudinal standing waves in air columns
  • Seismic waves from earthquakes include both transverse (S-waves) and longitudinal (P-waves) components
    • P-waves travel faster and arrive first, while S-waves cause more damage due to larger amplitudes
  • Electromagnetic waves, including light and radio waves, are transverse waves that can propagate through vacuum
    • Different frequencies correspond to different parts of the electromagnetic spectrum (radio, microwave, infrared, visible, ultraviolet, X-ray, gamma)
  • Doppler effect occurs when a wave source or observer is moving relative to the medium
    • Observed frequency increases when source and observer move towards each other
    • Observed frequency decreases when source and observer move away from each other
  • Interferometry uses wave interference to make precise measurements of distances or changes in distance
    • Applications include gravitational wave detection (LIGO) and measuring surface flatness in manufacturing


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AP® and SAT® are trademarks registered by the College Board, which is not affiliated with, and does not endorse this website.
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