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Feynman Path Integral Formulation

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28 1 Continuum <strong>Formulation</strong><br />

and the spin zero or trace part<br />

are such that their sum gives the original field h<br />

with the quantity P μν defined as<br />

h T μν = 1 3 P μνP αβ h αβ , (1.144)<br />

h = h TT + h L + h T , (1.145)<br />

P μν = η μν − 1<br />

∂ 2 ∂ μ∂ ν , (1.146)<br />

or, equivalently, in k-space P μν = η μν − k μ k ν /k 2 .<br />

One can learn a number of useful aspects of the theory by looking at the linearized<br />

form of the equations of motion. As before, the linearized form of the action<br />

is obtained by setting g μν = η μν +h μν and expanding in h. Besides the expressions<br />

given in Eq. (1.45), one needs<br />

√ gR 2 =(∂ 2 h λ λ − ∂ λ ∂ κ h λκ ) 2 + O(h 3 )<br />

√<br />

gRλμνκ R λμνκ = 1 4 (∂ μ∂ κ h νλ + ∂ λ ∂ ν h μκ − ∂ λ ∂ κ h μν − ∂ μ ∂ ν h κλ ) 2 + O(h 3 ) ,<br />

(1.147)<br />

from which one can then obtain, for example from Eq. (1.135), an expression for<br />

√ g(Rμν ) 2 ,<br />

√<br />

gRαβ R αβ = 1 4 (∂ 2 h μ μ∂ 2 h α α + ∂ 2 h μα ∂ 2 h μα − 2∂ 2 h μ μ∂ α ∂ β h αβ<br />

−2∂ α ∂ ν h ν μ∂ α ∂ β h μβ + 2∂ μ ∂ ν h μν ∂ α ∂ β h αβ )+O(h 3 ) .<br />

(1.148)<br />

Using the three spin projection operators defined previously, the action for linearized<br />

gravity without a cosmological constant term, Eq. (1.7), can then be re-expressed as<br />

∫<br />

I lin = 1 4 k dx h μν [P (2) − 2P (0) ] μναβ ∂ 2 h αβ . (1.149)<br />

Only the P (2) and P (0) projection operators for the spin-two and spin-zero modes,<br />

respectively, appear in the action for the linearized gravitational field; the spin-one<br />

gauge mode does not enter the linearized action. Note also that the spin-zero mode<br />

enters with the wrong sign (in the linearized action it appears as a ghost contribution),<br />

but to this order it can be removed by a suitable choice of gauge in which the<br />

trace mode is made to vanish, as can be seen, for example, from Eq. (1.13).<br />

It is often stated that higher derivative theories suffer from unitarity problems.<br />

This is seen as follows. When the higher derivative terms are included, the corresponding<br />

linearized expression for the gravitational action becomes

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