Export citation

Export citation

Choose format for download:

Download Citation

    Brown-York surface energy density and the geodesic equation

    Bjoern S. Schmekel*

    • Department of Physics, College of Studies for Foreign Diploma Recipients at the University of Hamburg, 20355 Hamburg, Germany

    • *Contact author: bss28@cornell.edu

    Phys. Rev. D 114, 084041 – Published 13 October, 2026

    DOI: https://doi.org/10.1103/8j2l-lqht

    Abstract

    The Brown-York quasilocal energy is traditionally obtained from the Hamilton-Jacobi formulation of general relativity as the boundary contribution to the gravitational Hamiltonian. In the present work we investigate whether the same boundary geometry also appears in the dynamics of freely falling particles. Starting from the autoparallel equation, we derive the normal projection of the geodesic equation with respect to the Brown-York boundary foliation. The resulting expression naturally separates into a geometric contribution involving the combination k−Θ, a kinematical term associated with the particle motion, and a mixed observer/particle contribution determined by the foliation geometry. The combination k−Θ is free of the reference-subtraction ambiguity inherent in integrated quasilocal energies. For a time-symmetric foliation Kij=0, and for geodesic configurations stationary with respect to the observer congruence, £uβ=0, the mixed observer/particle term vanishes. In Schwarzschild spacetime the remaining equation reproduces the Newtonian inverse-square law in the weak-field limit. The result may be interpreted geometrically as arising from the mismatch between the spatial embedding of a closed two-surface and the embedding of its timelike evolution in spacetime. We further derive the normal variation of the referenced Brown-York energy and show that, for Schwarzschild spheres, it satisfies the exact relation −dEBY/ds=EBYN(1+N)−1(k−Θ), thereby relating the acceleration term entering the projected geodesic equation directly to the radial variation of the integrated quasilocal energy. The analysis does not derive the geodesic equation from the Brown-York energy functional. Rather, it demonstrates that the same boundary geometry underlying Brown-York quasilocal energy also governs the normal component of free-fall dynamics, thereby establishing a direct geometrical connection between Hamiltonian boundary geometry and geodesic motion.

    Physics Subject Headings (PhySH)

    Authorization Required

    We need you to provide your credentials before accessing this content.

    References (Subscription Required)

    Outline

    Information

    Sign In to Your Journals Account

    Filter

    Filter

    Article Lookup

    Enter a citation