Summary: The WKB approximation works for potentials which are slowly-varying on the scale of the wavelength of the particle and is particularly useful for describing tunnelling.
The WKB approximation is named for G. Wentzel, H.A. Kramers, and L. Brillouin, who independently developed the method in 1926. There are pre-quantum antecedents due to Jeffreys and Raleigh, though.
We can always write the one-dimensional Schrödinger equation as
where . We could think of the quantity as a spatially-varying wavenumber (), though we anticipate that this can only make sense if it doesn’t change too quickly with position - else we can’t identify a wavelength at all.
Let’s see under what conditions a solution of the form
might be a good approximate solution. Plugging this into the SE above, the LHS reads . (Here and hereafter, primes denote differentiation wrt x — except when they indicate an integration variable.) So provided , or , this is indeed a good solution as the second term can be ignored. And does indeed mean that the wavelength is slowly varying. (One sometimes reads that what is needed is that the potential is slowly varying. But that is not a well defined statement, because is not dimensionless. For any smooth potential, at high-enough energy we will have . What is required is that the lengthscale of variation of , or , or (the scales are all approximately equal) is large compared with the de Broglie wavelength of the particle.
An obvious problem with this form is that the current isn’t constant: if we calculate it we get . A better approximation is
which gives a constant flux. (Classically, the probability of finding a particle in a small region is inversely proportional to the speed with which it passes through that region.) Furthermore one can show that if the error in the first approximation is , the residual error with the second approximation is . At first glance there is a problem with the second form when , ie when . But near these points - the classical turning points - the whole approximation scheme is invalid, because and so the potential cannot be “slowly varying” on the scale of .
For a region of constant potential, of course, there is no difference between the two approximations and both reduce to a plain wave, since .
For regions where , will be imaginary and there is no wavelength as such. But defining still, the WKB approximation will continue to be valid if .
Tunnelling and bound-state problems inevitably include regions where and the WKB approximation isn’t valid. This would seem to be a major problem. However if such regions are short the requirement that the wave function and its derivative be continuous can help us to “bridge the gap”.