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5.1 Super-potential method

Up to 2.5 PN order, we have solved all the Poisson equations necessary to derive the 2.5 PN gravitational field. At 3 PN order, we have found a part of the solutions of the Poisson equations, which we call (super-)potentials10. For example,
ri rjrkrl [ 1 ∂4 1 ] -1--15-13-2 = Δ − ----i---j--k---lf (1,− 1) +--(δij∂zk1 + δik∂zj1 + δjk∂zi1)∂zl2 ln S , (135 ) r1 r2 3 ∂z1∂z 1 ∂z1 ∂z2 3
where S = r1 + r2 + r12, and f (1,−1) which satisfies Δf (1,− 1) = r1∕r2 is given in [99Jump To The Next Citation Point] as
(1,−1) 1-- 2 2 2 1- 2 2 2 f = 18(− r1 − 3r1r12 − r12 + 3r1r2 + 3r12r2 + r2) + 6(− r1 + r12 + r2)lnS. (136 )

It is possible to add any homogeneous solution to super-potentials. In our formalism, the only place where we use super-potentials is Equation (101View Equation). In the case above, we could add, say, 1∕r1 to f (1,−1). (Note that to evaluate the surface integrals in the general form of equations of motion (111View Equation) we need super-potentials in the spatial region N ∕B which do not include any singularity due to the point particle limit.) It is easy to see that contribution from a possible additional homogeneous solution cancels out between the “− 4πg(⃗x)” term and the surface integral in Equation (101View Equation).

Useful super-potentials for derivation of the 3 PN field are given in [30Jump To The Next Citation Point27Jump To The Next Citation Point91Jump To The Next Citation Point99].


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