As developed elsewhere, we can write the interaction Hamiltonian as
A reasonable way to look at this is to see that if the field gains a photon ( ) then the single oscillator should loose one and vice versa; the prefactor is a coupling constant that will generally depend on the specifics of the system. The system is now governed by the total Hamiltonian,
Let us call the new density operator corresponding to our environmentally coupled system (S: Single original oscillator; E: Environment) where the individual density operators can be retrieved via a trace, i.e.
Trace over environment states | |||
Trace over local states |
The dynamics of the system evolve as (Liouville equation),
(4.1) |
We can then easily find that (since , letting ),
(4.3) |
(4.4) |
It follows that
Taking the trace of the Equation 4.5 gives,
(4.6) |
0 | |||
c.c. | (4.7) |
(4.8) |
Conventionally, we start with the so-called normally ordered characteristic function,
We take the time derivative of this function, and using the property
producing [8,9]
(4.9) | |||
(4.10) | |||
(4.11) |
Where . Finding our initial conditions as
(4.12) |
(4.13) |
And thus,
and , the density matrix becomes,
(4.14) |
(4.15) |
or |
The diagonal states will decay into the ground state as they reach equilibrium with the bath. However, this decay will generally be much slower than the decoherence. Finally we must note that decoherence has brought us into a classical density matrix, but the question still remains about which state we will find the particle in when an actual measurement is taken.
We summarize that decoherence is that part of dampening, caused by a coupling to an environment, which produces a decay (a stronger decay) of off-diagonal elements of a density matrix. Thus, in short time, the local quantum density matrix assumes a classical appearance. Since Decoherence is much quicker than normal dissipation, it has become a major engineering problem in the search for a quantum computer.