Acoustic wave equation

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In physics, the acoustic wave equation is a second-order partial differential equation that governs the propagation of acoustic waves through a material medium resp. a standing wavefield. The equation describes the evolution of acoustic pressure Template:Mvar or particle velocity Template:Mvar as a function of position Template:Mvar and time Template:Mvar. A simplified (scalar) form of the equation describes acoustic waves in only one spatial dimension, while a more general form describes waves in three dimensions.

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.[1]

Definition in one dimension

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

pxx1c2ptt=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.[2]

Derivation

Template:See also 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.

File:Derivation of acoustic wave equation.png
Derivation of the acoustic wave equation

The conservation of mass and conservation of momentum can be written as a closed system of two equationsTemplate:Sfn 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, letTemplate:Sfn q(x,t)=q0+q~(x,t), where q0=(ρ0,ρ0u0) is the (constant) background state and q~ is a sufficiently small pertubation, 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)]=[01u2+P(ρ)2u]. This results in the linearized equation q~t+f(q0)q~x=0ρ~t+(ρu~)x=0(ρu~)t+(u02+P(ρ0))ρ~x+2u0(ρu~)x=0 Likewise, small pertubations 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 pertubations relate to density pertubations 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-strenght 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=[ptpx],A^=[0c0210], where matrix A and A^ are similar.Template:Sfn

Solution

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

p=f(ctx)+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(ωtkx).

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

In three dimensions

Equation

Feynman[3] provides a derivation of the wave equation for sound in three dimensions as

2p1c22pt2=0,

where 2 is the Laplace operator, p is the acoustic pressure (the local deviation from the ambient pressure), and c is the speed of sound.

A similar looking wave equation but for the vector field particle velocity is given by

2𝐮1c22𝐮t2=0.

In some situations, it is more convenient to solve the wave equation for an abstract scalar field velocity potential which has the form

2Φ1c22Φt2=0

and then derive the physical quantities particle velocity and acoustic pressure by the equations (or definition, in the case of particle velocity):

𝐮=Φ,
p=ρtΦ.

Solution

The following solutions are obtained by separation of variables in different coordinate systems. They are phasor solutions, that is they have an implicit time-dependence factor of eiωt where ω=2πf is the angular frequency. The explicit time dependence is given by

p(r,t,k)=Real[p(r,k)eiωt]

Here k=ω/c  is the wave number.

Cartesian coordinates

p(r,k)=Ae±ikr.

Cylindrical coordinates

p(r,k)=AH0(1)(kr)+ BH0(2)(kr).

where the asymptotic approximations to the Hankel functions, when kr, are

H0(1)(kr)2πkrei(krπ/4)
H0(2)(kr)2πkrei(krπ/4).

Spherical coordinates

p(r,k)=Are±ikr.

Depending on the chosen Fourier convention, one of these represents an outward travelling wave and the other a nonphysical inward travelling wave. The inward travelling solution wave is only nonphysical because of the singularity that occurs at r=0; inward travelling waves do exist.

See also

Notes

Template:Reflist

References

  1. S. P. Näsholm and S. Holm, "On a Fractional Zener Elastic Wave Equation," Fract. Calc. Appl. Anal. Vol. 16, No 1 (2013), pp. 26-50, DOI: 10.2478/s13540-013--0003-1 Link to e-print
  2. Richard Feynman, Lectures in Physics, Volume 1, Chapter 47: Sound. The wave equation, Caltech 1963, 2006, 2013
  3. Richard Feynman, Lectures in Physics, Volume 1, 1969, Addison Publishing Company, Addison