Schrödinger equation
The Schrödinger equation is one of the fundamental equations of quantum mechanics and describes the spatial and temporal behavior of quantum-mechanical systems. Austrian physicist Erwin Schrödinger first proposed the equation in early 1926.
Mathematically, the Schrödinger equation is an example of an eigenvalue problem whose eigenvectors are called "wavefunctions" or "quantum states" and whose eigenvalues correspond to energy levels. Built into the eigenvectors are the probabilities of measuring all values of all physical observables, meaning that a solution of the Schrödinger equation provides a complete physical description of a system. The equation can be written in terms of Hamiltonians for both classical and quantum mechanical systems; in the latter case, the Hamiltonian functions are replaced by Hamiltonian operators.
Derivation
The wavefunction describes a wave of probability, the square of whose amplitude is equal to the probability of finding a particle at position x and time t. But what is the form of Schrödinger's equation, which describes the time and position evolution of the wavefunction?
We start by assuming that a beam of particles will have a wavefunction of the form
The square of this function (its probability amplitude) is a constant independent of position and time, which makes sense for a constant beam of particles: there is an equal probability of finding a particle at every point along the beam and any time. Using de Broglie's relations,
Based on the functional form of , we see that
Using the classical relationship between energy and momentum,
Substituting for p and E yields the one-dimensional time-dependent Schrödinger equation,
When the probability amplitude of the wavefunction is independent of time, it can be shown that energy is constant, and so the equation reduces to