7.1 The Wave Equation

7.1.1 Mathematical Description of a Wave

A wave is a periodic variation or disturbance which travels at a well defined speed through space. How do we describe waves mathematically? Suppose f(χ) is some periodic function which takes a phase χ measured in radians (fractions of 2π). Then we can describe the variation in space at a specific point in time as a snapshot:

y(x)=Af(2πλx+δ), (7.1)

where λ is the wavelength of the wave (the spatial period). We can also describe the variation in amplitude at a single point in space over time:

y(t)=Af(2πTt+θ), (7.2)

where T is the temporal period.

To put these pictures together, we can consider the snapshot picture with a shift xvt where v is the speed of the wave. Then we have

y(x,t) =Af(2πλ(xvt)+ϕ) (7.3)
=Af(2πλx2πvλt+ϕ) (7.4)
=Af(2πλx2πTt+ϕ) (7.5)
=Af(kxωt+ϕ). (7.6)

Where we have defined the wavenumber (spatial frequency measured in radians/m) k=2π/λ and recalled v=fλ, f=1/T and ω=2πf.

Example 7.1.

Suppose we have a sinusoidal wave given by y(x,t)=Acos(kxωt+ϕ). What is the particle velocity at fixed position x?

To solve this, we take the partial derivative with respect to time (to keep x constant)

y(x,t)t=Aωsin(kxωt+ϕ). (7.7)

Note that this is different to the propagation speed of the wave itself, which is constant.

7.1.2 Constructing the Wave Equation

For simplicity, let’s consider a general right-travelling wave f(xvt). We can make a substitution u=xvt. Then we get

fx =fuux (7.8)
=fu (7.9)
2fx2 =2fu2, (7.10)
ft =fuut (7.11)
=vfu (7.12)
2ft2 =v22fu2. (7.13)

If we do this same calculation with a left-travelling wave f(x+vt), we get the same relation. Thus, by construction, the general solution to the differential equation

2ft2=v22fx2, (7.14)

is f(x,t)=fl(x+vt)+fr(xvt). This linear differential equation is known as the wave equation. All functions which satisfy our definition of a wave solve this equation.