Quantifying Planetary Laminar Slip: A Prandtl Boundary Layer Analysis of Earth within a Fluidic Vacuum Substrate

This text presents a macro scale-up analysis within the Unified Space Theory (UST) framework. By scaling classical fluid mechanics to planetary systems using NASA Lense-Thirring frame-dragging telemetry, we map the physical boundary layer between Earth and the vacuum substrate. The raw linear baseline reveals a severe 557-billion Reynolds paradox. This high-turbulence barrier is resolved via a non-linear 7.83 Hz Schumann Resonance governor that collapses the shear gradient down to a frictionless laminar slip profile. The planetary system achieves full-film hydroplaning isolation, verified by a Tallian Lubrication Index of 28,400,000, allowing core-mantle topography to harvest ambient boundary energy as internal geodynamic heat.