SLIDE 18 Introduction GR JT gravity Conclusions
The symplectic potential only depend on δgab not on δΦ Θtot[gµν, Φ; δgµν, δΦ] =
√σ(−1)tρ[gµρΦ∇νδgµν − gνρ∇µΦδgµν −Φ∇ρ(gµνδgµν) + ∇ρΦgµνδgµν] +
i Φuλnρδgρλ |∂i
When δgµν = ∇µξν + ∇νξµ δΦ = 0 Θtot =
i 2[−ΦuρK ρνξν + nν∇νΦuρξρ
+ΦuλDλ(nνξν) − uρ∇ρΦnνξν] |∂i Θtot =
i 2[ c2 φ0 δρ0,i + c φ0 ρ0,iδc]
Ωtot = δΘtot = 2 c
φ0 δc ∧ δ(ρ0,R + ρ0,L) = δH ∧ δ(ρ0,L + ρ0,R)
Phase space (H, ρ0,L), sympletic form Ω = δH ∧ δρ0,L
Harlow, Jafferis 1804.01081
Geometric description of ρ0,L: We start from the right end of Cauchy surface, and shoot in a geodesic orthogonal to the boundary. It touches the left
- boundary. The relative distance to the left end of Cauchy is
ρ0,L
Jie-qiang Wu Covariant Phase Space with Boundaries