And there we have it: localisation of a wave (to form a wave packet) can be understood as a superposition of simple sinusoidal wave forms, with different wavelengths. When we are concerned with matter waves, each individual sinusoidal wave has an associated momentum (defined by the de Broglie equation). Therefore a wave packet, corresponding to a particle localised in a specific region of space, is associated not with a single, specific momentum but with a distribution of momenta. Like the spatial distribution this is effectively a probability distribution for the particle momentum, where the probability reflects the weighting of an individual sinusoidal component in constructing the wave packet.
"Now hold on there, Bald Eagle" interjects Cormorant, "I thought you were all telling me that I should think of a particle as a standing wave." (He is, of course, right: see section 5.5, for example). "So, if it's standing still, how does it have momentum?" That's a fair point, but Nefertiti is quick to remind him that we are thinking of our quantum mechanical waves as "probability waves", rather than conventional physical waves. A wave packet is a superposition of such waves and, therefore, carries with it a range of possible momenta, which might be measured, if a measurement were to be made. Moreover, a standing wave is (as we established in section 4.5) a superposition of waves travelling in opposite directions and, therefore, with momenta of opposite sign. Again this can be interpreted as meaning that if a measurement of a particle's momentum is made, we cannot be certain even of the direction of the momentum arising from its waviness.
"We must not lose time getting upset about these physical interpretations" insists Werner. "As my friend Niels Bohr has said, "if anybody says he can think about quantum theory without getting giddy it merely shows that he hasn't understood the first thing about it!." Cormorant does his best to look consoled. The key result we have found is this: the more we try to narrow a wave packet – in effect, to pin down a particle to a specific region of space – the greater the required range of wavelengths of the component sinusoids and therefore the greater the uncertainty there will be in the particle's momentum. What we have here is an enormously important principle, which is at the heart of quantum physics:
"I was the first to make this connection", explains Werner: “You will refer to it as the uncertainty principle, and it will be obeyed, without question, at all times.”
All of this is quite shocking. As Cormorant flies majestically across the sky, he knows where he is and he knows where he’s going and he knows how fast. Sir Isaac backs him up, so is he going to let Werner tell him that he can’t really be sure? He is not. But, as we have seen before, it could be just a matter of scale. So we need to try to quantify things a bit.
In our formulation, we have been generating wave packets by superposing y = cos (kx) over a range of k, the angular wavenumber (k = 2π/λ). Prince Louis’ equation (p = h/λ) then establishes the momentum connection: p = (hk/2π). So the uncertainty in any measurement of momentum would be related to the spread in the values of k. The uncertainty in position is related to the width of the wave packet – and, more specifically, to the probability density distribution obtained by squaring the wavefunction.
Recall that we worked out, in section 5.7, an expression for the function we get by superposing all functions y = cos (kx), over a range of k from k1 to k2. The equation we got, scaled so that it is in effect the mean of the superposition, is: