Phase-change systems with self-propelled matter: Disks, droplets, and bubbles
| dc.contributor.author | Tapocik, Jack Thomas | en |
| dc.contributor.committeechair | Boreyko, Jonathan Barton | en |
| dc.contributor.committeemember | Qiao, Rui | en |
| dc.contributor.committeemember | Coutier-Delgosha, Olivier | en |
| dc.contributor.committeemember | Cheng, Jiangtao | en |
| dc.contributor.department | Mechanical Engineering | en |
| dc.date.accessioned | 2026-09-30T08:00:16Z | en |
| dc.date.available | 2026-09-30T08:00:16Z | en |
| dc.date.issued | 2026-09-29 | en |
| dc.description.abstract | Phase-change phenomena such as boiling, condensation, and melting are ubiquitous in both natural and engineered systems. One example of a phase-change process producing motion is the Leidenfrost ratchet, where a superheated asymmetrically patterned surface rectifies the vapor flow to generate net viscous propulsion. Leidenfrost ratchets have been demonstrated for liquid–vapor and solid–vapor systems, yet solid–liquid systems remain largely uncharacterized. We first performed experiments with melting ice on a herringbone ratchet to characterize the governing physical mechanism. Two surface wettabilities were tested: hydrophilic and superhydrophobic. On the hydrophilic surface, viscous entrainment analogous to that of the Leidenfrost ratchet was observed. On the superhydrophobic surface, a distinct ``slingshot" mechanism emerged, in which a Laplace pressure mismatch across the melt puddle drives rapid re-centering of the ice disk, propelling it forward. After characterizing the first solid–liquid ratchet, we extended the results using paraffin wax. The wax disks traveled ten times farther and twice as fast as the ice. The improved mobility of wax disks enables several practical applications for enhanced heat and mass transfer. The self-propelled motion reduces the melt thickness by sevenfold, enabling faster melting and enhanced thermal conduction. Wax disks also enable mass transfer applications, including the transport of payloads up to 16× their own weight, self-cleaning of contaminated surfaces, and deposition of embedded particles. Another form of self-propulsion is jumping-droplet condensation, in which two quasi-spherical droplets on a superhydrophobic surface coalesce and spontaneously jump away from the surface. On superhydrophobic wheat leaves infected with pathogenic rust spores, coalescing droplets jump and carry spores away upon departure. Extending this study to infected barley leaves, a previously unreported ejection mechanism was observed, in which dry spores are launched during jumping-droplet condensation. This occurs when spores conglomerate into clusters, allowing droplets to nucleate and grow underneath the cluster of spores. Upon coalescence, the merged droplet jumps upward into the roof of the spore cluster, transferring its momentum and launching dry spores into the air. This previously unknown mode of spore dispersal carries implications for understanding disease transmission pathways in agricultural crops. The final phase-change process addressed in this thesis is bubble departure during pool boiling. Traditionally, buoyancy governs bubble departure, and methods to reduce the departure diameter have relied on nano/micro-structured surfaces, surfactants, electric fields, or surface wettability modifications. It was discovered that the coalescence of two bubbles during pool boiling can produce departure diameters an order of magnitude smaller than conventional values. Here, we designed and fabricated a custom pool boiling chamber that can visualize the individual bubble coalescence events on micron-sized features. After preliminary testing, we discovered that the bare silicon wafers result in high surface adhesion and don't allow for the bubbles to depart the surface. Instead, we investigated the spatial control and nucleation density of bubbles on a micro-patterned silicon chip using a custom boiling chamber. This thesis primarily details the design and construction of the custom boiling chamber and the rationale for the micro-patterned feature parameters. These collective works all leverage surface structures to impart dynamic heat and mass transfer phenomena to phase-change processes. Potential applications include: self-cleaning, accelerated energy transfer with phase-change materials, particle sensing, and enhanced heat transfer coefficients for boiling or condensation. Future work will include finishing ongoing projects related to the spatial control and coalescence-induced jumping of nucleating micro-bubbles, furthering our understanding of pathogenic spore dispersal, and extending the practicality of phase-change materials. | en |
| dc.description.abstractgeneral | Phase-change is a process that is so integrated into our daily lives, that I imagine most people don't think twice about common occurrences like boiling, condensation, and melting. Exploiting the process of phase-change is not an easy task and often requires complicated engineering practices to overcome limitations. One topic that I find particularly interesting is a phenomena referred to as the Leidenfrost effect. This effect occurs when a droplet is placed onto a significantly heated surface and creates an insulating blanket of vapor as it evaporates. You may be familiar with this effect if you like to cook, as most chefs prefer their pans to be in a Leidenfrost state to avoid food sticking, or if you've seen one of many kitchenware infomercials that utilize the Leidenfrost effect to show evaporation levitating food on pans to advertise products. Some brilliant researchers have found that certain patterned surfaces utilize this levitation effect to self-propel droplets. The vapor is directed into the patterns, causing the droplets to surf along the vapor blanket. Imagine this as a puck on an air hockey table levitating above the surface, where the air is being directed by a bunch of wooden blocks in a specific pattern. You can also observe the Leidenfrost effect in disks of dry ice because the ice instantly goes from a solid to a vapor. But what happens when we apply this effect to a melting solid like ice? At Racetrack Playa in Death Valley California, scientists noted the mysterious movement of large rocks (up to 17 kilograms) across the desert. In the cold months of the year, the rocks sit on a thin sheet of ice. As the weather warms in the spring, the combination of melting ice and small wind gusts cause the ice to slide hundreds of meters across the desert. We performed experiments inspired by this geological phenomenon. By melting ice disks on a V-shaped (herringbone) patterned surface, we were able to witness unaided movement, resembling the naturally occurring sliding of the Death Valley rocks. One a wetting surface, the melt water from the ice moves down the patterns, allowing the ice to ride along. A non-wetting surface behaves differently, where the water in general does not want to spread and rather create small spherical droplets or puddles. The melting ice sticks directly to the surface and allows the meltwater to create a puddle on the front and back sides of the ice disk. The puddles are different sizes due to the V-shaped channels not allowing for the water to flow backwards. This mismatch is puddle sizes creates a pressure difference, where the back puddle is a higher pressure and the front is a smaller pressure. Since we know that liquid flows from high pressure to low pressure, ice disks can be pushed back into the center of a puddle and be propelled to glide across the surface. This can resemble a slingshot, as the stretching of the puddle in the front spontaneously shifts the ice back into the center, slinging it forward. We can observe a very similar behavior when switching our material from ice to paraffin wax. Paraffin wax can travel about 10 times farther and almost twice as fast in comparison to ice. Because this material is able to travel faster and further, we can use the wax disks for practical applications. One example is to utilize the wax to take heat away from a surface faster. By moving a wax disk from one part of the heated surface to another, we can increase the amount of melting that occurs compared to that same disk melting stationary on a smooth plate. We can also use paraffin wax to move weights across the surface. As the wax melts and moves, it can carry up to about 16 times its own weight and still be in motion, analogous to an ant carrying 10--50 times its own weight. Another application is the direct deposition of particles. By filling the wax with particles the size of sand, we can deposit the particles directly onto the surface in the direction of motion. The final practical application we explored was exploiting the wax to clean a dirty surface. By depositing the same small particles on the herringbone, we found that the paraffin wax is able to push them as it glides across the surface, cleaning it with the motion of the disk. A surface that is wetting can grow a film of water, like the condensation on the outside of a glass soda bottle. Alternatively, a surface that is non-wetting will grow individual spherical droplets, rather than a large film. This is important because two droplets growing next to each other on a non-wetting surface can merge together and spontaneously jump from the surface. These jumping drops occur on natural surfaces such as lotus leaves, ferns, and even crops such as barley and wheat. Previously, this jumping-droplet effect was seen to take away small disease spores on wheat leaves. In an effort to observe this on more plants, we infected barley leaves with another type of rust spore and were able to witness jumping-droplet events. In addition to the droplets carrying spores away, we also observed a new type of spore launching event, in which spores can be launched off of the surface without being attached to a droplet. This occurs when the spores are clustered together in a large pile and the droplets grow in the spaces between them. The droplets merge underneath the spore pile and jump into the spore ceiling, launching the spores into the air. This would be like hitting a cue ball in a billiards game to scatter other balls across the table. These barley leaf billiards can help to inform how disease is spread among food crops, as the spores are capable of launching onto other leaves. Boiling water is one of the most commonly used methods of phase-change. As humans, we utilize water boiling in a wide variety of practical applications all the way from cooking pasta to generating power from nuclear reactors. The water takes heat away from the surface and uses that heat to warm itself, until it reaches a critical point where boiling occurs. The boiling point for water occurs at 100,$^circ$C, but what happens if the surface keeps adding heat to boiling water? The bubbles become larger and larger, until finally they merge into a continuous blanket of vapor. This vapor film the separates the water from the heated surface is called the Leidenfrost point, exactly the same as the droplet levitating. This is an undesirable condition because after this point, the surface rapidly heats up and can cause the surface to melt. To prevent this film from being created, it is important to limit the bubble size for departure, as well as control where the bubbles are able to grow. Analogous to droplets merging and jumping, bubbles that merge together during boiling can also jump and leave the surface at smaller diameters than a bubble leaving the surface normally. Here, we create a custom boiling experimental setup that can visualize the bubbles merging and jumping. It was shown during early experimental trials that a bubble leaves a feature and contacts a significant portion of the floor. This inhibits the jumping efficiency, as the more contact the bubble has to the floor, the more force is required to lift the bubble. Instead, we pivot to understanding how bubbles decide to nucleate within a grid-array of sub-millimeter sized holes. The joining theme of these research projects is the use of phase-change to propel a solid body. Melting ice propels down the herringbone aluminum plate by following its own meltwater on a wetting surface or by an uneven puddle distribution on a non-wetting surface. Pathogenic rust spores that are deadly to crops can be launched off the leaf by jumping droplets undergoing condensation. We can make boiling vapor bubbles come off of the surface at smaller sizes and predict the locations they grow. | en |
| dc.description.degree | Doctor of Philosophy | en |
| dc.format.medium | ETD | en |
| dc.identifier.other | vt_gsexam:47767 | en |
| dc.identifier.uri | https://hdl.handle.net/10919/143864 | en |
| dc.language.iso | en | en |
| dc.publisher | Virginia Tech | en |
| dc.rights | In Copyright | en |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
| dc.subject | self-propulsion | en |
| dc.subject | jumping-droplet condensation | en |
| dc.subject | pathogenic spread | en |
| dc.subject | pool boiling | en |
| dc.title | Phase-change systems with self-propelled matter: Disks, droplets, and bubbles | en |
| dc.type | Dissertation | en |
| thesis.degree.discipline | Mechanical Engineering | en |
| thesis.degree.grantor | Virginia Polytechnic Institute and State University | en |
| thesis.degree.level | doctoral | en |
| thesis.degree.name | Doctor of Philosophy | en |
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