exchemist
Valued Senior Member
I think you both have the better explanation. The vids interested me but your explanations are better.
If we think of refraction as a bulk effect acting on the wave velocity then we can almost dispense with trying to trace the path at the level of the atomic interstitial space. Actually in the first vid the prof is saying glass, which is almost always amorphous, but he's drawing crystalline material. Minor point, but it serves to show the advantage of keeping this at the bulk level.
I would have just said that whenever the impedance changes, the phase shifts and hence the velocity changes. I'm pretty sure I can calculate the characteristic impedance if I know the polarization and susceptibility, so I think I'm on the right track. And there is a dual for the velocity change for acoustic waves in air vs water which uses the stiffness (or compliance) and density (I think) which are duals of something like permittivity (or polarization) and permeability (or susceptibility)-- from which we can calculate a characteristic impedance for both of them.
So using your better explanations as the gold standard, I'm betting that if we reduced this to a single parameter it's probably impedance.
Also, velocity (esp c) can be written as the inverse of the geometric mean of permittivity and permeability. And they establish the impedance.
Interesting. The only problem I see with this idea of impedance is that one also has to account for dispersion, i.e. the fact that refractive index is a function of frequency and changes in a rather interesting way as one approaches, passes through, and then retreats from, an absorption resonance frequency. I like the concept of the forced oscillation because the idea of "lead" and "lag" of the driven oscillation, relative to the forcing frequency, gives one a picture that incorporates this and relates it to spectroscopic absorption and emission at the same time.