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Kiefer C. Quantum gravity

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246 QUANTUM COSMOLOGY<br />

8.1.2 Quantization of a Friedmann universe<br />

As an example, we shall treat in some detail the case of a closed Friedmann<br />

universe with a massive scalar field; cf. <strong>Kiefer</strong> (1988) and Halliwell (1991). Classically,<br />

the model is thus characterized by the scale factor a(t) and the homogeneous<br />

field φ(t)withmassm. In the quantum theory, the classical time parameter<br />

t is absent, and the system is fully characterized by a wave function ψ(a, φ). The<br />

ansatz for the classical line element is<br />

ds 2 = −N 2 (t)dt 2 + a 2 (t)dΩ 2 3 , (8.1)<br />

where dΩ 2 3 =dχ2 +sin 2 χ(dθ 2 +sin 2 θdϕ 2 ) is the standard line element on S 3 .A<br />

special foliation has thus been chosen in order to capture the symmetries of this<br />

model. For this reason no shift vector appears, only the lapse function N. The<br />

latter naturally occurs in combination with dt, expressing the classical invariance<br />

under reparametrizations of the time parameter; see Chapter 3.<br />

The three-metric h ab is fully specified by the scale factor a. The second fundamental<br />

form, cf. (4.48), reads here<br />

K ab = 1 ∂h ab<br />

= ȧ<br />

2N ∂t aN h ab . (8.2)<br />

Its trace is<br />

K ≡ K ab h ab = 3ȧ<br />

Na , (8.3)<br />

which is thus proportional to the Hubble parameter ȧ/a. Itsinverse,K −1 ,isfor<br />

this reason called ‘extrinsic time’; cf. Section 5.2.<br />

Since the model fulfils the symmetric criticality principle, we can insert the<br />

ansatz (8.1) directly into the Einstein–Hilbert action (1.1) and derive the Euler–<br />

Lagrange equations from the reduced action. For the surface term in (1.1), one<br />

obtains<br />

Inserting<br />

∫<br />

1<br />

8πG<br />

d 3 x √ hK = 3 ∫<br />

8πG<br />

d 3 x √ h ȧ<br />

Na .<br />

√<br />

h d 3 x = a 3 sin 2 χ sin θ dχdθdϕ ,<br />

one finds that this surface term is cancelled by a term that appears after partial<br />

integration from the first term in (1.1). This is how the general surface term is<br />

constructed. More explicitly, one has for the curvature scalar:<br />

(<br />

R = 6<br />

N 2 − Ṅȧ<br />

Na + ä [ȧ ] ) 2<br />

a + + 6 a a 2 .<br />

Partial integration of the second term in the parentheses cancels both the surface<br />

term and the first term and changes the sign of the third term.

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