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Acoustic wave equation

Equation for the propagation of sound waves through a medium

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Related on Lably

Through Physics, Standing wave and Speed of sound

For lossy media, more intricate models need to be applied in order to take into account frequency-dependent attenuation and phase speed. Such models include acoustic wave equations that incorporate fractional derivative terms, see also the acoustic attenuation article or the survey paper.

Definition in one dimension

The wave equation describing a standing wave field in one dimension (position x) is

pxx−1c2ptt=0,

where p is the acoustic pressure (the local deviation from the ambient pressure) and c the speed of sound, using subscript notation for the partial derivatives.

Derivation

Start with the ideal gas law

P=ρRspecificT,

where T the absolute temperature of the gas and specific gas constant Rspecific. Then, assuming the process is adiabatic, pressure P(ρ) can be considered a function of density ρ.

The conservation of mass and conservation of momentum can be written as a closed system of two equations ρt+(ρu)x=0,(ρu)t+(ρu2+P(ρ))x=0. This coupled system of two nonlinear conservation laws can be written in vector form as: qt+f(q)x=0, with q=[ρρu]=[q(1)q(2)],f(q)=[ρuρu2+P(ρ)]=[q(2)q(2)2/q(1)+P(q(1))].

To linearize this equation, let q(x,t)=q0+q~(x,t), where q0=(ρ0,ρ0u0) is the (constant) background state and q~ is a sufficiently small perturbation, i.e., any powers or products of q~ can be discarded. Hence, the Taylor expansion of f(q) gives: f(q0+q~)≈f(q0)+f′(q0)q~ where f′(q)=[∂f(1)/∂q(1)∂f(1)/∂q(2)∂f(2)/∂q(1)∂f(2)/∂q(2)]=[01−u2+P′(ρ)2u]. This results in the linearized equation q~t+f′(q0)q~x=0⇔ρ~t+(ρu~)x=0(ρu~)t+(−u02+P′(ρ0))ρ~x+2u0(ρu~)x=0 Likewise, small perturbations of the components of q can be rewritten as: ρu=(ρ0+ρ~)(u0+u~)=ρ0u0+ρ~u0+ρ0u~+ρ~u~ such that ρu~≈ρ~u0+ρ0u~, and pressure perturbations relate to density perturbations as: p=p0+p~=P(ρ0+ρ~)=P(ρ0)+P′(ρ0)ρ~+… such that: p0=P(ρ0),p~≈P′(ρ0)ρ~, where P′(ρ0) is a constant, resulting in the alternative form of the linear acoustics equations: p~t+u0p~x+K0u~x=0,ρ0u~t+p~x+ρ0u0u~x=0. where K0=ρ0P′(ρ0) is the bulk modulus of compressibility. After dropping the tilde for convenience, the linear first order system can be written as: [pu]t+[u0K01/ρ0u0][pu]x=0. While, in general, a non-zero background velocity is possible (e.g. when studying the sound propagation in a constant-strength wind), it will be assumed that u0=0. Then the linear system reduces to the second-order wave equation: ptt=−K0uxt=−K0utx=K0(1ρ0px)x=c02pxx, with c0=K0/ρ0 the speed of sound.

Hence, the acoustic equation can be derived from a system of first-order advection equations that follow directly from physics, i.e., the first integrals: qt+Aqx=0, with q=[pu],A=[0K01/ρ00]. Conversely, given the second-order equation ptt=c02pxx a first-order system can be derived: qt+A^qx=0, with q=[pt−px],A^=[0c0210], where matrix A and A^ are similar.

Solution

Provided that the speed c is a constant, not dependent on frequency (the dispersionless case), then the most general solution is

p=f(ct−x)+g(ct+x)

where f and g are any two twice-differentiable functions. This may be pictured as the superposition of two waveforms of arbitrary profile, one (f) traveling up the x-axis and the other (g) down the x-axis at the speed c. The particular case of a sinusoidal wave traveling in one direction is obtained by choosing either f or g to be a sinusoid, and the other to be zero, giving

p=p0sin⁡(ωt∓kx).

where ω is the angular frequency of the wave and k is its wave number.

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