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74 November 7, 2013<br />

− λ 4<br />

6<br />

(<br />

φ(y) 3 δ<br />

+ 3¯hφ(y)<br />

δJ(y) φ(y) + δ 2 )}<br />

¯h2 (δJ(y)) 2 φ(y)<br />

. (2.46)<br />

On this basis, we can now formulate Feynman rules for the continuum limit :<br />

x y<br />

↔ Π(x − y)<br />

↔ − λ 4<br />

¯h<br />

x ↔ +J(x) ¯h<br />

Feynman rules, version 2.3 (2.47)<br />

This comes with the understanding that the positions of all vertices are to be<br />

integrated over, and that the field function φ is now a functional of the source<br />

J. For a free theory there are no interactions, and we find<br />

∫<br />

φ(x) = dy Π(x − y) J(y) . (2.48)<br />

We see that the free field is the sum of its responses to the source, weighted<br />

by the correlation between the position where the field is measured and that<br />

of the strength of the source at all points. It is this property that establishes<br />

the propagator as the ‘differential-equation’ Green’s function; but note that this<br />

correspondence is only valid for non-interacting theories.<br />

2.3.5 Field configurations in one dimension<br />

Before entering spaces of more dimensions, we may have a look at the field<br />

variables. The zero-dimensional variable ϕ, with its integration element, is in<br />

the discrete one-dimensional formulation replaced by the whole set ϕ, for which<br />

the path integration element reads, of course,<br />

Dϕ = ∏ n<br />

dϕ n<br />

The continuum limit of this object is defined to be the continuum-formulation<br />

path integration element, however badly defined this may be. The assigning a<br />

functional value S[ϕ] to a given field ϕ(x) is not problematic ; rather it is the<br />

prescription of how all field configurations are to be summed over that makes<br />

it so hard to define path integrals rigorously 14 . It is instructive to consider the<br />

14 In fact, the mathematical definition of continuum path integrals relies on the discrete<br />

formulation !

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