6.2 Bringing it All Back Home
Combining the wave equation, the de Broglie equation and the principle of conservation of energy leads us to the Schrödinger equation.
Let’s set about finding the Schrödinger equation. This is where everything starts to come together: we are going to need to combine a whole lot of the ideas we’ve developed in these first five chapters.
The wave function of an electron in an atom should be a standing wave.
We can begin by remembering our proposition from chapter one: if an electron is in a stable state in an atom, its wavefunction should represent a standing wave, meaning that the peaks oscillate in sign and intensity but do not shift in space. In chapter four, we explored the idea that a standing wave can be understood as a superposition of travelling waves, identical except that they are travelling in opposite directions. This led us to an equation for a simple sinusoidal standing wave:
Ψ = 2Asin(2πx/λ)cos(2πvt/λ) (VI-1)
The crucially helpful thing about this expression is that the space and time-dependent terms are separate – just two terms multiplied together – which makes it different from equations describing travelling waves. This is going to help us immensely in working out the maths to come.
Now we know from the previous chapter that a particle waveform won’t be a simple sinusoid like this – although, as Prof. Fourier was once again about to remind us, it should be possible to represent it as a sum of sinusoids - because that would not localise the particle in space. Moreover, particles are three dimensional, whereas all our theory has been confined to 1-dimension. But don't worry: the principles are exactly the same, the maths just gets more complicated and challenging once we introduce extra dimensions. So we'll keep thinking 1-dimensionally and trust that we can generalise down the line.
If we can describe our particle in terms of a standing wave, it seems reasonable to suggest that, since the space and time-dependent parts of the function are separate, only the spatial part needs to be different in order to get a standing wave that's appropriate to a localised particle. Therefore, by direct analogy with equation IV-2, we can propose that our wavefunction is of the form:
Ψ(x,t) = ψ(x).cos(2πvt/λ) (VI-2)
where ψ(x) is the spatial part. This massively simplifies our problem: now we only have to try to find ψ(x). How are we going to do that?
The wave function must obey the wave equation
In Chapter 4, we developed the wave equation (equation IV-5). This should be obeyed by any wave, including our proposed wave function for a particle. It provides a connection between the time and space parts of the wave function, at the level of second derivatives. Now that we have introduced Ψ as the wave function, we can write the wave equation as: