- i\dot\varphi + A\varphi = 0 (1)
- \dot\varphi_1 =-A\varphi_2, \dot\varphi_2 = A\varphi_1 (2)
where the oscillatory nature is exhibited: \varphi_1 changes with input from A\varphi_2 and \varphi_2 changes with input from A\varphi_1. We understand that there is nothing magical in the complex-valued form (1) as it is only shorthand for the real-valued system (2) simply expressing oscillation between two states.
With different operators A the equation (1) (or system (2)) covers:
Hopefully, this can help to reduce the mystery of the complex form of Schrödinger's equation and give incentive to check out realQM.
The basic feature of (2) obtained by multiplication of the first equation by \varphi_1 (or -\dot\varphi_2) and the second by \varphi_2 (or \dot\varphi_1) and addition followed by integration in space, is conservation in time of
With different operators A the equation (1) (or system (2)) covers:
- Physics (Harmonic oscillator): A = identity, \varphi_2 position, \varphi_1 velocity,
- Electro-magnetics (Maxwell’s Equations): A =\nabla\times, \varphi_2=E electrical field, \varphi_1=B magnetic field,
- Mechanics (Vibrating Elastic Plate): A =\Delta, \varphi_2 displacement velocity, \varphi_1 moment,
- Chemistry (Foxes and Rabbits): A=identity, \varphi_1 and \varphi_2 species densities,
- Quantum Mechanics (Schrödinger’s Equation): A=H with H Hamiltonian, \varphi wave function.
Hopefully, this can help to reduce the mystery of the complex form of Schrödinger's equation and give incentive to check out realQM.
The basic feature of (2) obtained by multiplication of the first equation by \varphi_1 (or -\dot\varphi_2) and the second by \varphi_2 (or \dot\varphi_1) and addition followed by integration in space, is conservation in time of
- \int (\varphi_1^2+\varphi_2^2)dx,
- \int (\varphi_1A\varphi_1+\varphi_2A\varphi_2)dx,
capturing oscillation between two states; when \varphi_1 is big \varphi_2 is small, and vice versa.
Inviscid fluid mechanics can also be formulated as (a generalisation of ) (2):
Inviscid fluid mechanics can also be formulated as (a generalisation of ) (2):
- \dot v + \nabla p= 0, \dot p + \nabla\cdot v=0 with v velocity and p pressure.
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