Wave Physics – How Vibrating a String Inverts Vibration to Create an Opposite Traveling Wave

boundary conditionsreflectionstringwavelengthwaves

I am currently trying to understand standing waves. The key to the phenomenon is that:
$$A\sin(kx+\omega t) + A\sin(kx-\omega t)=2A\sin(kx)\cos(\omega t)$$
The shape of $2A\sin(kx)\cos(\omega t)$ is constant, as only the amplitude changes with time due to the $\cos(\omega t)$. This creates the familiar "standing wave", as the shape remains the same while the amplitude goes up and down, occasionally hitting $0$. The following post also explains that the wavelength is not actually required to fit $L/0.5n$ to form a standing wave: That is only a requirement if the amplitude on both ends of the string has to be $0$. In most string setups, the ends are fixed though, so practically speaking this is a requirement.

Suppose that I have a string of length $L$ with fixed ends, and that I have somehow managed to make a perfect sin-wave on one side of the string. This wave is traveling to the other side of the string:

enter image description here

As most articles and videos have described it, when a wave hits the end, it will both change direction, and flip/be inversed. But I have great difficulty seeing how this ends up creating an identical wave with identical phase to the first one. There is also a great deal of ambiguity in how one is supposed to visualize this flip and reverse action:

  • Is the whole wave flipped at once, or is it flipped "gradually" as each point of it hits the end?
  • Does the wave move while it's in the action of being inverted? If so, wouldn't that mean that a lot of parts of it never hit the end, and are thus never reflected properly?
  • Does the standing wave phenomena only occur because new waves are constantly created on one end. Is it these waves that the original waves form interference with, or does the wave form interference with "itself"?

The problem isn't that I don't get how the initial wave is created on a string instrument:
I get that when plucking a string instrument, a triangle shape is created, and that this shape can be described as a sum of harmonic frequencies of varying amplitudes. The problem is that I don't really get the geometry of this whole inversion process, and how it forms two identical waves.

Best Answer

Propagation of waves is described by the wave equation $$\frac{d^2u}{dx^2}=\frac{1}{c^2}\frac{d^2u}{dt^2}.$$ But on its own this is not enough: we also need boundary conditions. You are describing what's called fixed boundary conditions or Dirichlet boundary conditions. This amounts to setting $u(x,t)$ to a fixed value on the boundary. It turns out in 1D this is quite easy; in 1D you can always decompose a solution to the wave equation in a left- and right travelling part $$u(x,t)=u_R(x-vt)+u_L(x+vt).$$ Now let's say we want to impose $u=0$ at $x=0$. In that case we get \begin{align} u(0,t)=0&\implies u_R(-vt)=-u_L(+vt)\\ &\implies u_R(-z)=-u_L(z) \end{align} where I used $z$ to remind you that $u_R,u_L$ are just functions of one variable. So we can conclude $u_R,u_L$ have the same shape, but they are reflected in the y-axis (one is upside down) and reflected in the x-axis (they are mirrored around $x=0$). So as a recap because we set $u$ to some fixed value at a particular $x$ the left- and right travelling solutions are mirror images of eachother: the reflected wave is minus the incoming wave. To see this in action look at the following animation.

enter image description here

Here the green line shows the actual solution $u$: it is a sum of the blue and red lines which are the right- and left travelling solutions. The blue and red lines are extended past the domain to make it more clear what is happening. Notice how blue and red work together to keep the boundary point of green at a fixed height.


Edit in response to Michael. I saved the code to make this gif so here's a version with a wave that has no symmetry at all

enter image description here

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