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Frenkel line of Yukawa fluids within the self-consistent relaxation theory

This paper utilizes self-consistent relaxation theory to define the Frenkel line in Yukawa fluids as the thermodynamic boundary where the roton minimum in the longitudinal excitation dispersion relation vanishes, demonstrating that this dynamic crossover can be directly determined from the static structure factor and aligns with molecular dynamics simulation results.

Original authors: Ilnaz I. Fairushin, Anatolii V. Mokshin

Published 2026-09-04
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Original authors: Ilnaz I. Fairushin, Anatolii V. Mokshin

Original paper licensed under CC BY 4.0 (http://creativecommons.org/licenses/by/4.0/). This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer

In the world of matter, there is a state that exists beyond the familiar boundaries of liquid and gas. When a substance is heated and pressurized past a certain critical point, the sharp line that usually separates a boiling liquid from a rising vapor disappears. The result is a supercritical fluid, a unique state where the substance behaves like a hybrid, possessing the density of a liquid but the ability to diffuse like a gas. Scientists have long been interested in mapping this hidden territory, looking for invisible lines that separate different kinds of behavior within this fluid. One such line, known as the Frenkel line, marks a fundamental shift in how the particles inside the fluid move. On one side of this line, the particles are locked in a rhythmic, vibrating dance, moving together in a way that resembles a solid. On the other side, they break free, moving more like a gas where they drift and collide without a coordinated rhythm. Understanding where this line lies is crucial because it tells us when a fluid stops acting like a solid and starts acting like a gas, a transition that governs everything from the behavior of deep-earth minerals to the efficiency of industrial cooling systems.

Researchers Ilnaz Fairushin and Anatolii Mokshin have taken a fresh look at this problem using a specific type of fluid called a Yukawa fluid. This is a theoretical model used to describe systems where particles push each other away with a force that gets weaker as they get farther apart, a behavior seen in things like dusty plasmas. Instead of trying to watch every single particle move in a computer simulation, which is a common but computationally heavy method, the authors used a mathematical framework called self-consistent relaxation theory. This approach allows them to predict how the fluid behaves by looking at its structure—specifically, how the particles are arranged relative to one another. They focused on the sound waves that travel through the fluid, which are actually vibrations of the particles moving together. In a solid or a dense liquid, these waves have a specific pattern: their speed changes as their wavelength changes, creating a curve that dips down to a low point before rising again. This dip is called a roton minimum.

The team discovered that this roton minimum acts as a reliable signpost for the Frenkel line. When the fluid is in the solid-like regime, where particles are tightly packed and vibrating together, this dip in the wave pattern is clearly visible. However, as the fluid becomes hotter or less dense, the particles begin to move more freely and the collective rhythm breaks down. At a specific point, the dip in the wave pattern disappears entirely. The researchers found that the exact moment this roton minimum vanishes corresponds consistently with the Frenkel line. By calculating the conditions under which this dip disappears, they were able to map out the line on the fluid's phase diagram. Their results matched closely with previous studies that used massive computer simulations to track individual particles, confirming that this structural feature is a consistent indicator of the transition, with the numerical procedure showing an error not exceeding 5%.

What makes this finding particularly powerful is that it offers a direct way to identify the Frenkel line using only static data. Usually, determining where this line lies requires complex measurements of how the fluid moves over time. The authors showed that if you know the static structure of the fluid—essentially a snapshot of how the particles are arranged—you can calculate the behavior of the sound waves and predict exactly where the transition happens. They also proposed a physical explanation for what the roton minimum represents. They suggest that the frequency of this minimum is directly tied to how long it takes for a particle to escape its temporary cage of neighbors. When the particles are stuck in a solid-like rhythm, this time is long, and the minimum is present. When they break free, the time becomes short, and the minimum vanishes.

The study also addressed a competing idea that had been proposed recently, which suggested the Frenkel line could be found by looking at the height of the peak in the particle arrangement graph. The authors found that their method, based on the disappearance of the wave dip, produced a different result, noting a significant deviation from the alternative criterion. However, since their work mainly focused on a specific range of fluid states, they concluded that it is difficult to draw a definite conclusion as to how the alternative approach relates to theirs. Their work confirms that the disappearance of the roton minimum is a consistent and measurable marker for the shift from solid-like to gas-like dynamics. By linking the invisible line of the Frenkel transition directly to a visible feature in the fluid's wave patterns, the researchers have provided a clearer, more direct tool for scientists to understand the complex behavior of supercritical fluids. This approach not only validates previous findings but also simplifies the process of mapping these dynamic boundaries, offering a new perspective on how matter changes its nature under extreme conditions.

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