Schrödinger's Equation
The basic premise of wave mechanics is that a massive particle of energy and linear momentum , moving in the -direction (say),
can be represented by a one-dimensional complex wavefunction of the form
|
(11.15) |
where the complex amplitude, , is arbitrary, while the wavenumber, , and the angular frequency, ,
are related to the particle momentum, , and energy, , via the fundamental
relations (11.3) and (11.1), respectively. The previous one-dimensional wavefunction is the solution of
a one-dimensional wave equation that determines how the wavefunction evolves in time.
As described below, we can guess the form of this wave equation by drawing an analogy with classical physics.
A classical particle of mass , moving in a one-dimensional potential , satisfies the energy conservation
equation
|
(11.16) |
where
|
(11.17) |
is the particle's kinetic energy (Fitzpatrick 2012). Hence,
|
(11.18) |
is a valid, but not obviously useful, wave equation.
However, it follows from Equations (11.1) and (11.15) that
|
(11.19) |
which can be rearranged to give
|
(11.20) |
Likewise, from Equations (11.3) and (11.15),
|
(11.21) |
which can be rearranged to give
|
(11.22) |
Thus, combining Equations (11.18), (11.20), and (11.22), we obtain
|
(11.23) |
This equation, which is known as Schrödinger's equation—because it was first formulated by Erwin Schrödinder in 1926—is the fundamental equation of wave mechanics (Dirac 1982).
For a massive particle moving in free space (i.e., ), the complex wavefunction (11.15) is a
solution of Schrödinger's equation, (11.23), provided
|
(11.24) |
The previous expression can be thought of as the dispersion relation (see Section 4.2) for matter waves in free space. The
associated phase velocity (see Section 6.3) is
|
(11.25) |
where use has been made of Equation (11.3). However, this phase velocity is only half the classical velocity, ,
of a massive (non-relativistic) particle.