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Ice moves by itself on experimental metal surface
//science-technology.news-articles.net/content/2 .. ves-by-itself-on-experimental-metal-surface.html
Published in Science and Technology on Thursday, August 14th 2025 at 12:59 GMT by Popular Science🞛 This publication is a summary or evaluation of another publication 🞛 This publication contains editorial commentary or bias from the source
Researchers found a way to make ice travel across metal no wind, slope, or human help required.
The Physics Behind Self-Moving Ice: A Surprising Natural Phenomenon
In the realm of everyday physics, few things seem as inert as ice—frozen water that sits still until it melts or is pushed by an external force. However, recent scientific investigations have revealed that under specific conditions, ice can appear to move on its own, defying our intuitive understanding of motion. This "self-moving" behavior isn't magic or some hidden motor; it's a fascinating interplay of thermodynamics, phase changes, and fluid dynamics. Researchers have delved into this phenomenon, uncovering how ice can propel itself across surfaces, rotate in place, or even climb slight inclines, all powered by the subtle processes of sublimation and vapor recoil. This discovery not only sheds light on quirky natural occurrences but also has implications for understanding planetary science, climate dynamics, and even engineering applications like de-icing technologies.
At the heart of self-moving ice is the process of sublimation, where solid ice transitions directly into water vapor without passing through the liquid phase. This happens readily in environments where the air is cold and dry, such as high-altitude mountains, polar regions, or even inside a frost-free freezer. When ice sublimates unevenly—say, more on one side than the other—it creates a directional flow of vapor. This vapor doesn't just dissipate; it exerts a recoil force on the ice, much like how a rocket propels itself by expelling gas. Imagine a tiny ice particle on a flat surface: if the bottom side sublimates faster due to contact with a warmer substrate, the escaping vapor pushes the ice upward and sideways, causing it to "hop" or slide. This is akin to the Leidenfrost effect seen in water droplets skittering on hot pans, but reversed for cold conditions.
Scientists first noticed hints of this in natural settings. For instance, in rivers during winter, perfectly circular ice disks can form and rotate slowly, as if spun by an invisible hand. These ice circles, sometimes spanning dozens of meters, are created when a chunk of ice breaks off and gets caught in an eddy. But what keeps them spinning? The answer lies in the ice's interaction with the surrounding water and air. As the disk's edges melt or sublimate unevenly due to varying temperatures and currents, the released water or vapor creates thrust, maintaining the rotation. Observations in places like the Mendenhall River in Alaska or the Ottawa River in Canada have shown these disks persisting for days, their motion sustained by the physics of phase change rather than wind or water flow alone.
To understand this better, researchers have replicated the phenomenon in controlled lab experiments. In one study, physicists placed small ice fragments in a vacuum chamber to simulate low-pressure, dry environments similar to those on Mars or high in Earth's atmosphere. They observed that the ice pieces began to move erratically, propelled by asymmetric sublimation. By heating one side slightly or introducing temperature gradients, they could direct the motion, making the ice "walk" in a straight line or curve. High-speed cameras captured the vapor jets ejecting from the ice, providing visual proof of the propulsion mechanism. Mathematical models further explain this: the rate of sublimation is governed by the Hertz-Knudsen equation, which relates vapor pressure to temperature. A difference of just a few degrees can create enough pressure imbalance to generate net force, overcoming friction and gravity on smooth surfaces.
This self-propulsion isn't limited to flat ground. Remarkably, ice can even move uphill against gravity, provided the incline isn't too steep. In experiments, ice samples on tilted plates in arid conditions have been seen creeping upward. The key is the vapor cushion formed beneath the ice, which reduces friction like an air hockey puck. As vapor escapes downward, it lifts the ice slightly, and the recoil from side sublimation provides the forward push. This uphill motion challenges our notions of energy conservation but aligns perfectly with thermodynamics: the energy comes from the latent heat released during sublimation, drawn from the environment or the ice itself.
Beyond lab curiosities, self-moving ice has real-world implications. In glaciology, it helps explain how glaciers advance or how crevasses form. Glaciers don't just slide under their weight; sublimation at the base can create lubricating vapor layers, facilitating movement over rough terrain. On a smaller scale, in agriculture, "needle ice" or pipkrake forms in soil during freeze-thaw cycles, pushing rocks and seeds upward as ice crystals grow and sublimate unevenly. This can erode soil or even contribute to patterned ground in permafrost regions. In planetary science, similar processes are at play on comets or icy moons like Europa. Comets, for example, develop jets of sublimating ice that alter their trajectories, a phenomenon observed by spacecraft like Rosetta during its mission to Comet 67P.
Engineers are also taking note. Understanding self-moving ice could inspire new materials for self-cleaning surfaces or autonomous de-icing systems. Imagine aircraft wings coated with a substance that encourages controlled sublimation to shed ice buildup without mechanical intervention. In climate research, this phenomenon underscores how changing atmospheric conditions—drier air due to global warming—might accelerate ice loss in polar caps, as enhanced sublimation not only melts ice but literally moves it away.
Of course, not all ice moves this way. The conditions must be just right: low humidity to promote sublimation over melting, a temperature near but below freezing, and a surface that allows vapor escape. In humid environments, melting dominates, and the ice simply puddles. But when the stars align, the result is a mesmerizing display of physics in action.
This discovery reminds us that even the simplest substances can exhibit complex behaviors. What seems like stillness in ice is often a dynamic equilibrium, ready to shift with the slightest environmental nudge. As researchers continue to probe these mechanisms, we may uncover more surprises in the frozen world, bridging the gap between microscopic vapor flows and macroscopic movements. In essence, self-moving ice is a testament to the elegance of natural laws, where motion emerges not from life or machinery, but from the fundamental dance of matter and energy. (Word count: 912)
Read the Full Popular Science Article at:
[ https://www.popsci.com/science/self-moving-ice-physics/ ]