Mercury and its Behavior

This paper presents a theoretical explanation of thermal behavior within the framework of the Solitonic Universe Model (SEM). In SEM, temperature is not defined as particle motion or kinetic agitation, but as the manifestation of wave-order disruption in the finite solitonic domain of the Universe. Atoms are described as vortex-like structures whose nuclei bend the universal medium, forming stable electron channels. When the universal field becomes wavy, these channels oscillate vertically, producing what is classically perceived as heat. However, certain heavy elements—most notably mercury—possess intrinsic nuclear asymmetry that generates lateral (forward–backward) oscillations instead of vertical ones. This internal topological irregularity causes thermal energy to spread slowly, diffusively, and without a clear direction. As a result, mercury behaves like a warm fluid even when it is physically cold. Its apparent warmth does not arise from external excitation or classical heat, but from the broken symmetry and topological dynamics of its own nucleus.