Simulations of Mpemba effect in water and Lennard-Jones models
摘要
Understanding why hotter water can freeze faster than colder water — a phenomenon known as the Mpemba effect — is important for gaining deeper insights into systems far from equilibrium. Despite growing interest, this effect has not been demonstrated in computer simulations of ice formation. Using the TIP4P/Ice model, we show that the Mpemba effect appears in our simulated systems and observe its manifestation also during fluid-to-solid transitions in the case of simpler Lennard-Jones systems. We extend this investigation to magnetic transitions, revealing that the effect can arise from different mechanisms: for the TIP4P/Ice model, the effect arises from how long the system remains in a metastable state, while for other systems, it results from differences in critical fluctuations in the initial states. These findings suggest a universal behavior and are contrary to the common belief that metastability is a necessary requirement.