Anisotropic Geodesic Photon Scattering as a Mechanical Driver of Terrestrial, Planetary, and Galactic Core Heating: A BH-WW Framework

Modern geophysics and astrophysics rely heavily on radiogenic decay and primordial accretion heat to explain the internal temperatures of celestial bodies, alongside feedback accretion models for galactic cores. However, severe thermodynamic deficits persist: empirical geoneutrino assessments account for less than half of Earth’s ∼ 47 TW surface heat flux; gas giants (Jupiter, Saturn) radiate nearly twice the solar irradiance they intercept; small frozen satellites (Enceladus, Europa) sustain enduring hydrothermal activity defying conductive freezing timescales; and galactic cluster cores resist expected radiative cooling flows. Within the Black Hole–White Wall (BH-WW) theoretical framework, this paper proposes an opto-geometric mechanism: anisotropic geodesic photon scattering. Because gravitational wells deform local spacetime into narrow and temporally elongated axial geometries, thermal and radiative photons inside matter do not scatter isotropically. Outward-directed photons face an uphill gravitational redshift penalty, whereas inward-directed scattering trajectories follow geodesic convergence and blueshifting. This microscopic directional asymmetry acts as an inescapable, steady-state radiative heat pump driving energy toward mass centers. Where mass remains below the topological puncture threshold (M < M critical ), the sought Klein drainage throat cannot open, causing inwardly driven flux to accumulate at the core as sustained kinetic thermal pressure. This mechanism offers a unified, non-radiogenic explanation for long-standing geophysical and astrophysical heat anomalies.