Information, Quantum Probability and Reflection/Refraction Part IV Particle Wave Duality
Francesco R. Ruggeri
In a number of notes (Parts I,II,III) we considered the problem of photons A moving in the positive x direction striking a medium at x=0 and reflecting B and refracting C. In (1) conservation of energy: I(A)/c1 = I(B)/c1 + I(C)/c2 ((1)), where I(A) is intensity which has the form of energy * velocity i.e. a flux, is given. Thus I(A)/c1 = n1 E , I(B)=n2 E and I(C)=n3 E, where E is constant energy of a photon and ni are the number of photons. Conservation of energy/or photon is a conservation law in terms of “particles” and is furthermore a time averaged result. A single photon either reflects or refracts. In both cases conservation of particle number and energy exists and so one may wonder why one needs a time averaged “particle” type conservation equation in the first place. We argue that it demonstrates the role of flux in this problem - a role which differs from that of hydrodynamics in classical physics. ((1)) shows immediately that there is neither conservation of flux i.e. I(A) values or momentum even in a steady state scenario (i.e. time averaged scenario) represented by ((1)). This is different from an incompressible liquid moving from a wide pipe to a narrow one. In such a case flux is conserved yet microscopic particles change velocity, momentum and energy. As noted in Part I, one may write: I(A)/c1 - I(B)/c1 = I(C)/c2 , multiply by E (energy) and use E=pc. This yields a “kind” of momentum conservation equation, but not in terms of particle numbers (i.e. not in a particle picture). Rather I(A)p is momentum multiplied by flux which is unusual. ((1)) is a conservation of particle number and energy, but does not include conservation of flux or momentum flux which one might expect in a steady state flow equation and which appears in classical fluid dynamics. As noted in Part I to obtain these additional conservation/balance equations one is forced to use square root probabilities i.e. I(A)=AA with A representing a square root flux or dynamic probability. Using the idea of differences of squares, one may write: A + B = C ((2a)) and Ap1 -p1B = p2C ((2b)) and solve for B and C in terms of A. In other words a hydrodynamical approach applies to the square root probabilities A,B,C and not to I(A)=AA etc. Ultimately squaring, one obtains I(A),I(B) and I(C) showing that the square root probability or wave/dynamical probability represents balance and conservation. In ((2a)) and ((2b)) i.e. with square root probabilities one has dropped the view of particles and changed to a square root flux/ new dynamical probability picture together with its balances. This is in fact the wave picture because A,B,C are linked with exp(ip1x),exp(-ip1x) and exp(ip2x) (which for photons are associated with the wave picture of the electric and magnetic fields). Thus even though there is particle wave duality, in terms of conservation waves (square root probabilities) yield particle conservation equations. For example, it is the wave picture which allows one to solve for B and C in terms of A. The wave picture may be associated with a steady state (time removed) equilibrium scenario in which dynamical (square root) probabilities add in space (not by time grouping) and it contains both conservation of probability and momentum probability while momentum (of the particles) may not be conserved in the particle picture as is the case for the reflection/refraction problem. Particle number/energy are also guaranteed.
•Dec 12, 2022•0 citations