Students should learn the method of steepest descent
Today I gave a lecture to a Solid State Physics class on " Magnetic quantum oscillations and mapping out the Fermi surface ." I basically follow chapter 14 of Ashcroft and Mermin. The central result is Onsager 's 1952 equation that the period of the magnetic oscillations is related to extremal areas of the Fermi surface perpendicular to the magnetic field. [Aside: This is an amazing result because it only involves fundamental constants and so the interpretation of the experiments is not "theory laden", a rare thing in condensed matter]. There is one point I struggle to explain: why extremal areas? Ashcroft and Mermin have a figure to justify this. It is lost on me, no matter how many times I read it and stare at the pictures. Does anyone know a clear and convincing way to demonstrate this? The only way I know how to get this result of extremal areas is to do a very fancy calculation (Lifshitz-Kosevich) which evaluates the magnetisation (or thermodyn