PlanetPhysics/Solving the Wave Equation Due to D Bernoulli

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A string has been strained between the points\,

(0,0)

\, and\,

(p,0)

\, of the

x

-axis.\, The transversal vibration of the string in the

xy

-plane is determined by the one-dimensional [[../WaveEquation/|wave equation]]

2ut2=c22ux2

satisfied by the ordinates\, u(x,t)\, of the points of the string with the abscissa x on the time moment\, t(0). The [[../PiecewiseLinear/|boundary]] conditions are thus u(0,t)=u(p,t)=0. We suppose also the initial conditions u(x,0)=f(x),ut(x,0)=g(x) which give the initial [[../Position/|position]] of the string and the initial [[../Velocity/|velocity]] of the points of the string.

For trying to separate the variables, set u(x,t):=X(x)T(t). The boundary conditions are then\, X(0)=X(p)=0,\, and the [[../DifferentialEquations/|partial differential equation]] (1) may be written

c2XX=TT.

This is not possible unless both sides are equal to a same constant k2 where k is positive; we soon justify why the constant must be negative.\, Thus (2) splits into two ordinary linear [[../DifferentialEquations/|differential equations]] of second order:

Failed to parse (unknown function "\begin{matrix}"): {\displaystyle \begin{matrix} X'' = -\left(\frac{k}\right)^2 X,\quad T'' = -k^2T \end{matrix}}

The solutions of these are, as is well known,

Failed to parse (unknown function "\begin{cases}"): {\displaystyle \begin{matrix} \begin{cases} X = C_1\cos\frac{kx}+C_2\sin\frac{kx}\\ T = D_1\cos{kt}+D_2\sin{kt}\\ \end{cases} \end{matrix}}

with integration constants Ci and Di.

But if we had set both sides of (2) equal to\, +k2, we had got the solution\, T=D1ekt+D2ekt\, which can not present a vibration.\, Equally impossible would be that\, k=0.

Now the boundary condition for X(0) shows in (4) that\, C1=0,\, and the one for X(p) that C2sinkp=0. If one had\, C2=0,\, then X(x) were identically 0 which is naturally impossible.\, So we must have sinkp=0, which implies kp=nπ(n+). This means that the only suitable values of k satisfying the equations (3), the so-called eigenvalues, are k=nπcp(n=1,2,3,). So we have infinitely many solutions of (1), the eigenfunctions u=XT=C2sinnπpx[D1cosnπcpt+D2sinnπcpt] or u=[Ancosnπcpt+Bnsinnπcpt]sinnπpx (n=1,2,3,) where An's and Bn's are for the time being arbitrary constants.\, Each of these [[../Bijective/|functions]] satisfy the boundary conditions.\, Because of the linearity of (1), also their sum series

u(x,t):=n=1(Ancosnπcpt+Bnsinnπcpt)sinnπpx

is a solution of (1), provided it converges.\, It fulfils the boundary conditions, too.\, In order to also the initial conditions would be fulfilled, one must have n=1Ansinnπpx=f(x), n=1Bnnπcpsinnπpx=g(x) on the interval\, [0,p].\, But the left sides of these equations are the Fourier sine series of the functions f and g, and therefore we obtain the expressions for the coefficients: An=2p0pf(x)sinnπxpdx, Bn=2nπc0pg(x)sinnπxpdx.

All Sources

[1]

References

  1. {\sc K. V ais al a:} Matematiikka IV .\, Hand-out Nr. 141.\quad Teknillisen korkeakoulun ylioppilaskunta, Otaniemi, Finland (1967).

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