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Feynman Path Integral Formulation

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92 3 Gravity in 2 + ε Dimensions<br />

order in the ε expansion these authors then find<br />

β(G) =ε G − (9 − c)G 2 + ... (3.112)<br />

and therefore a non-trivial ultraviolet fixed point close to two dimensions at G c =<br />

ε/(9−c), where c is the central charge of the superconformal matter multiplet, such<br />

as c free scalars and spinor fields. Taken at face value, these result would suggest<br />

that, besides ordinary Einstein gravity, also N = 1 supergravity could have a nontrivial<br />

strong coupling phase, which appears for G > G c .<br />

3.6 Phases of Gravity in 2+ε Dimensions<br />

The gravitational β-function of Eqs. (3.106) and (3.110) determines the scale dependence<br />

of Newton’s constant G for d close to two. It has the general shape shown<br />

in Fig. 3.7. Because one is left, for the reasons described above, with a single coupling<br />

constant in the pure gravity case, the discussion becomes in fact quite similar<br />

to the non-linear σ-model case.<br />

For a qualitative discussion of the physics it will be simpler in the following<br />

to just focus on the one loop result of Eq. (3.106); the inclusion of the two-loop<br />

correction does not alter the qualitative conclusions by much, as it has the same<br />

sign as the lower order, one-loop term. Depending on whether one is on the right<br />

(G > G c )orontheleft(G < G c ) of the non-trivial ultraviolet fixed point at<br />

G c = d − 2<br />

β 0<br />

+ O[(d − 2) 2 ] , (3.113)<br />

(with G c positive provided one has c < 25) the coupling will either flow to increasingly<br />

larger values of G, or flow towards the Gaussian fixed point at G = 0, respectively.<br />

In the following we will refer to the two phases as the strong coupling and<br />

weak coupling phase, respectively. Perturbatively one only has control on the small<br />

Fig. 3.7 The renormalization<br />

group β-function for gravity<br />

in 2 + ε dimensions. The<br />

arrows indicate the coupling<br />

constant flow as one approaches<br />

increasingly larger<br />

distance scales.<br />

β (G)<br />

Gc<br />

G

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