Droplets with particles in them can leave complex stains when they dry — just look at coffee rings and whiskey marks! Here, researchers look at the patterns left on glass by small droplets that evaporated and left behind their nanoparticles. As evaporation takes place, the droplet’s shape changes, adding stress to the growing layer of nanoparticle residue. Cracking is one way to relieve that stress. Another method is delamination — peeling up from the surface. On the leftmost drop, the outer rim of nanoparticles delaminated — as seen from the circular fringes — which released stress without cracking. The rightmost drop, which had a smaller contact angle with the surface, couldn’t delaminate and instead cracked throughout. (Image credit: M. Ibrahim et al.)
Search results for: “art”
Banzai Pipeline From Above
On the north shore of O’ahu, Hawaii, Banzai Pipeline is known for some of the most thrilling and deadly surfing in the world. The area’s barrel rolls are triggered when incoming waves break over the shallow reef. Photographer Kevin Krautgartner captures the waves from above, showcasing the incredible energy inherent in the ocean. The motion and texture of the water is mesmerizing. I feel like I could stare at these all day long! (Image credit: K. Krautgartner; via Colossal)
Switchable Explosives
Explosives are used in many fields, including mining and demolition, but storing these devices is difficult and dangerous. Hundreds of accidents — many resulting in fatalities — have happened over the decades, simply because there is no true “off-switch” for explosive devices. But a group out of Los Alamos believe they’ve changed that.
Without water in the device, the outer surfaces burn, but no explosion takes place. Using 3D-printing, the researchers built an explosive lattice filled with empty voids. With air in these gaps, any attempt to light the explosive fizzle. The outer layers of the explosive burn, but there’s no detonation. It is, relatively speaking, safe for storage.
When the voids are filled with water, the explosive detonates when lit. But once the device is filled with water (or another liquid), the story is different. In this situation, the blast wave propagates and the explosive detonates, releasing 98% more energy than in its “storage” mode. Changing the liquid inside the device can enhance the explosive energy, too, which could allow users to tune the discharge. (Image credit: S. Moses; video and research credit: C. Brown et al.; via APS Physics)
Polygonal Jumps
When you turn on your kitchen faucet, you may have noticed a big circle that forms on the bottom of the sink. This is a hydraulic jump, a region where fast-moving, shallow flow shifts to a slower-moving, deeper flow. Although these jumps start out circular, if the fluid is deeper than a critical value, the jump will break down and form polygons, like the one above. Exactly what shape the jump forms depends on many factors: flow speed, fluid depth, and flow history. The same flow conditions can even form more than one shape. But all of these shapes have one thing in common: their corners are universally around 114 degrees with a radius of 3.5 millimeters. (Image and research credit: S. Tamim et al.; via PRF)
100 For the Ocean
One hundred photographers of all genres are coming together this month to raise money for ocean conservation in “100 For the Ocean.” Through the end of this month, they’re selling prints of these and other images, starting at $100 apiece. All proceeds will go to ocean conservation. Check out all the prints here, and if your wall has a bare spot, now’s a great time to add some artwork on a fluidsy nature. (Image credits: 100 For the Ocean, individual photographers listed in gallery titles; via Colossal)
Disclosure: I have no affiliation whatsoever with this fundraiser. I just like great photos and preserving nature.
Honeybee Feeding
Busy bees feed on millions of flowers for each kilogram of honey they produce. To gather nectar, bees use their hairy tongues, which project out of a sheath-like cover. Protraction (i.e., sticking their tongue out) is relatively fast because all the hairs on the tongue initially lie flat. In the nectar, those hairs flare out, creating a miniature forest that traps viscous nectar and drags it back into the bee during retraction.
Bees feed by projecting their tongues into nectar. Tongue extension is faster because the tongue’s hairs lie flat. During the slower retraction phase, the hairs flare out, trapping nectar and pulling it back into the bee. Through modeling and experiments, researchers found that the time it takes a bee to retract its tongue depends on the bee’s overall mass. Smaller bees are slower to the retract their tongues, likely to allow enough time for their shorter tongues to capture enough nectar. With bee populations on the decline, the team’s predictions may help communities select flowers with nectar concentrations that best fit their local bees’ needs. (Image credits: top – J. Szabó, bee eating – B. Wang et al.; research credit: B. Wang et al.; via APS Physics)
Ominous Mammatus
Mammatus clouds are fairly unusual and often look quite dramatic. Most clouds have flat bottoms, caused by the specific height and temperature at which their droplets condense. But mammatus clouds have bubble-like bottoms that are thought to form when large droplets of water or ice sink as they evaporate. Although they can occur in the turbulence caused by a thunderstorm, mammatus clouds themselves are not a storm cloud. They appear in non-stormy skies, too. The clouds are particularly striking when they’re lit from the side, as in the image above. (Image credit: J. Olson; via APOD)
The Physics of Clogging
Clogging is one of those phenomenons that we encounter constantly, from overflowing storm drains to the traffic jam at the door when a lecture ends. It happens at all scales, too; ink-jet cartridges and microfluidic circuits can jam up just as thoroughly as a grain silo. Although there are many complexities to clogging, the basic mechanisms fall into three categories: sieving, bridging, and aggregation.
Of these, sieving is the most familiar; it occurs when a particle too large for the constriction gets stuck. That includes both a rock too large to fit down a storm drain and a leaf that gets caught in the wrong orientation.
Bridging, on the other hand, occurs when too many small particles reach a constriction at the same time. Although each one is small enough to fit on its own, their simultaneous arrival means that they jam together into a bridge that blocks the constriction. Given time, all flow comes to a stand still, as seen in the images below.
Sequence of images showing the formation of a particle bridge and subsequent clogging of the entire constriction. The last mechanism, aggregation, is a more gradual blockage, formed as individual particles begin sticking to a surface, making the constriction progressively smaller. Think of those hard-water buildups that eventually block your shower head.
Some of these mechanisms are easier to prevent or clear than others, but researchers are making progress. For an overview of the field’s current standing, check out this Physics Today article. (Image credit: drain – R. Rampsch, bridging – D. Jeong et al.; see also B. Dincau et al. at Physics Today)
“Evanescent”
Giant iridescent inflatables dot public spaces in the “Evanescent” exhibit. The “bubble-tecture” is the work of Sydney-based artistic collaboration Atelier Sisu. Conceived during the pandemic, the duo “endeavoured to communicate this feeling of transient beauty and the need to live in the moment through the idea of the bubble.” The exhibit has appeared in more than 22 cities in 12 different countries. (Image credit: Atelier Sisu; via Colossal)
Water Builds Static Charge
The ancient Greeks first recognized static electricity, but the mechanisms behind it remain somewhat mysterious. In particular, it’s unclear how two pieces of the same material can build a charge between them simply by touching. Yet we regularly see examples of this when volcanic ash creates enough charge to discharge lightning. A new study sheds light on the question by studying the impact of a single grain of silica on a silica disk.
The researchers used acoustic levitation to hold their silica particle in place. By turning the acoustic waves off, they could bounce the grain off the disk, then catch the particle again with the acoustic field. After a bounce, they swept an electrical field across the particle and observed its oscillations to determine how much charge the particle held. When necessary, they could also discharge the particle.
This animation demonstrates the three phases of an experiment. In the first (left), the acoustic field is shut off, allowing the silica grain to fall and strike the disk. Then the field is turned back on to “catch” the particle. In the second phase (middle), the researchers use a sweeping electrical field to determine the charge built up on the grain. In the third phase (right), they periodically discharge the built-up charge on the particle. What they found was that charge on the particle grew with the number of impacts. They also saw that they could reverse the polarity of the charge with careful cleaning and baking of their objects. Their conclusion is that adsorption of water from the surrounding air is what enables the build-up of static charge on identical materials. (Image credit: volcano – M. Szeglat, experiment – G. Grosjean and S. Waitukaitis; research credit: G. Grosjean and S. Waitukaitis; via APS Physics)