NanakiXIII said:
The propagator D for a particle is basically the Green's function of the differential operator that describes that particle, e.g.
<br />
(\partial^2 + m^2) D(x-y) = \delta^4 (x-y).<br />
This propagator is supposed to give the probability of the particle propagating from x to y. Why does this make sense? Why would the inverse of the differential operator have something to do with probabilities?
OK, I decided to forget about trying to explain this in a nonstandard fancy-schmancy
way. Let's just go back to a textbook treatment...
Have you studied Peskin & Schroeder pp29-31 (subsection titled "The Klein Gordon
Propagator") ? If not, that's a reasonably direct route to get an answer (imho).
P&S give the calculation for the retarded propagator
<br />
D_R(x - y) ~:=~ \theta(x^0 - y^0) \; \langle 0|\, [\phi(x), \phi(y)]\, |0\rangle<br />
and show that when you apply the KG operator to the RHS you get a delta function.
I.e., the retarded propagator as defined above is indeed a KG Green's function.
This example might be a little difficult to relate to simple particle propagation
from x to y since there's a commutator in there. But if you study their
calculation in eq(2.56) and then apply the same techniques to the Feynman
propagator eq(2.60), i.e.,
<br />
D_F(x - y) ~:=~ \theta(x^0 - y^0) \; \langle 0| \phi(x) \phi(y) |0\rangle<br />
~+~ \theta(y^0 - x^0) \; \langle 0| \phi(y) \phi(x) |0\rangle<br />
you can still show that it's also a KG Greens function, and it's more obviously
got something to do with particle propagation, -- correctly time-ordered.
I'm not sure whether this is enough for you to complete the details of the
answer yourself, so I'll add a couple more remarks...
\phi(x) satisfies the KG equation, and is interpreted as the operator for
creating a particle at x. Its adjoint is correspondingly for destroying a particle at x.
A particle "propagating from x to y" means creating it at x and destroying it at y.
That's why we use expressions of the form
<br />
\langle 0| \phi(y) \phi(x) |0\rangle<br />
to mean propagation from x to y. The extra step functions involving the
time component are just to get the physical time ordering right.
If you don't have access to P&S, or have trouble following their
calculation leading to eq(2.56), let me know and I'll try to post
a more detailed calculation.