Waves are fundamental to physics, describing how energy moves through space and time. The wave equation and wave speed are key concepts, helping us understand how waves behave in different media and situations.
This section dives into the math behind waves, showing how they're described and how fast they move. We'll see how these ideas apply to real-world examples, from guitar strings to light in diamonds.
Derivation of the Wave Equation
Fundamental Principles and Concepts
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Wave equation describes propagation of waves in a medium using second-order partial differential equation
Derivation utilizes Newton's Second Law of Motion and Hooke's Law as foundational principles
Process involves analyzing forces acting on small element of the medium
Equation relates spatial and temporal derivatives of wave function
One-dimensional wave equation takes form ∂ 2 y ∂ t 2 = v 2 ∂ 2 y ∂ x 2 \frac{\partial^2y}{\partial t^2} = v^2\frac{\partial^2y}{\partial x^2} ∂ t 2 ∂ 2 y = v 2 ∂ x 2 ∂ 2 y
y represents displacement
t denotes time
x indicates position
v signifies wave speed
Extension to higher dimensions allows for more complex wave propagation scenarios
Two-dimensional equation used for waves on surfaces (membranes)
Three-dimensional equation applied to sound waves in air or seismic waves in Earth's crust
Mathematical Derivation Steps
Begin with small element of medium (string segment)
Apply Newton's Second Law F = m a F = ma F = ma to element
Express forces in terms of tension and displacement using Hooke's Law
Derive equation of motion for element
Take limit as element size approaches zero
Simplify resulting equation to obtain wave equation
Identify wave speed in terms of medium properties (tension and mass density for string)
Mechanical Waves
Wave speed depends on medium properties through which wave propagates
General formula for mechanical waves v = elastic property inertial property v = \sqrt{\frac{\text{elastic property}}{\text{inertial property}}} v = inertial property elastic property
Specific formulas for different media:
Strings or wires: v = T μ v = \sqrt{\frac{T}{\mu}} v = μ T (T tension, μ linear mass density)
Sound waves in fluids: v = B ρ v = \sqrt{\frac{B}{\rho}} v = ρ B (B bulk modulus, ρ density)
Longitudinal waves in solids: v = Y ρ v = \sqrt{\frac{Y}{\rho}} v = ρ Y (Y Young's modulus)
Examples of wave speeds:
Guitar string (nylon, medium tension) approximately 500 m/s
Sound in air at room temperature roughly 343 m/s
Seismic P-waves in granite about 5000 m/s
Electromagnetic Waves
Speed of electromagnetic waves in medium given by v = c n v = \frac{c}{n} v = n c
c represents speed of light in vacuum (299,792,458 m/s)
n denotes refractive index of medium
Examples of electromagnetic wave speeds:
Light in water (n ≈ 1.33) approximately 225,000,000 m/s
Light in diamond (n ≈ 2.42) roughly 124,000,000 m/s
Factors Affecting Wave Speed
Temperature influences wave speed
Sound waves travel faster in warmer air
Affects speed of waves in solids (thermal expansion)
Pressure impacts wave propagation
Higher pressure increases speed of sound in gases
Affects wave speed in compressed solids
Other physical properties affect wave speed
Salinity changes speed of sound in water
Humidity alters speed of sound in air
Solving the Wave Equation
Boundary Conditions and Their Effects
Boundary conditions specify wave behavior at medium edges or interfaces
Common boundary conditions:
Fixed ends (string tied at both ends)
Free ends (string with loose ends)
Periodic boundaries (circular membrane)
Fixed ends lead to standing waves with nodes at boundaries
Example: guitar string produces harmonics
Free ends allow antinodes at boundaries
Example: open-ended organ pipe
Periodic boundaries result in waves repeating in space
Example: vibrations on surface of drum
Solution Methods and Applications
Separation of variables technique often employed to solve wave equation
Assumes solution can be written as product of functions of space and time
Leads to two separate ordinary differential equations
Solutions with boundary conditions introduce concepts of:
Normal modes (standing wave patterns)
Natural frequencies (resonant frequencies of system)
Examples of applications:
Calculating resonant frequencies of musical instruments
Designing acoustic spaces for optimal sound quality
Analyzing vibrations in engineering structures (bridges, buildings)
Dispersion Relation for Waves
Concept and Mathematical Representation
Dispersion relation describes relationship between wave frequency and wavenumber
General form ω = ω ( k ) \omega = \omega(k) ω = ω ( k )
ω represents angular frequency
k denotes wavenumber
Non-dispersive media have linear dispersion relation ω = v k \omega = vk ω = v k
v signifies constant wave speed
Dispersive media exhibit frequency-dependent phase velocity
Phase velocity v p = ω k v_p = \frac{\omega}{k} v p = k ω varies with frequency
Group velocity v g = d ω d k v_g = \frac{d\omega}{dk} v g = d k d ω differs from phase velocity
Examples and Phenomena
Water waves in deep water show dispersion
Dispersion relation ω = g k \omega = \sqrt{gk} ω = g k (g gravitational acceleration)
Longer wavelengths travel faster than shorter ones
Electromagnetic waves in certain materials display dispersion
Leads to phenomena like chromatic aberration in lenses
Analysis of dispersion relation reveals:
Wave packet spreading in dispersive media
Anomalous dispersion in certain frequency ranges
Example: light passing through glass near absorption frequencies