#fluiddynamics — Public Fediverse posts

Capillary Slinkies

Nature is full of helical fibers, including in plants and bird feathers. In this study, researchers explore how these soft springs react to droplets. When the pitch of the spring (roughly speaking, the spacing between coils) is small, droplets can flow down in a plug (not shown). But as the pitch increases, droplets can take on a caterpillar-like (or, eruciform) shape. These drops descend quickly, in part, the team found, because internal flows within the droplet help it along.

Other drops maintain a spherical shape as they descend the widely-spaced coils of the spring. These drops tend to spin around the coil as they go, with their center of mass actually moving side-to-side as they descend. (Image and research credit: B. Bhatt and A. Carlson)

Capillary Slinkies

Nature is full of helical fibers, including in plants and bird feathers. In this study, researchers explore how these soft springs react to droplets. When the pitch of the spring (roughly speaking, the spacing between coils) is small, droplets can flow down in a plug (not shown). But as the pitch increases, droplets can take on a caterpillar-like (or, eruciform) shape. These drops descend quickly, in part, the team found, because internal flows within the droplet help it along.

Other drops maintain a spherical shape as they descend the widely-spaced coils of the spring. These drops tend to spin around the coil as they go, with their center of mass actually moving side-to-side as they descend. (Image and research credit: B. Bhatt and A. Carlson)

Dragonfly Dogfights

Like fighter pilots of old, male dragonflies engage in aerial combat where each tries to outmaneuver the other to keep a sight on their rival’s tail. A recent study observed this combat in the field and uncovered some surprising similarities to dogfighting. Like pilots, dragonflies used spiraling turns and other high-g moves to gain an advantageous position behind the other. In human combat, that position favors the forward-facing weapons of the pilot in back; for dragonflies, it keeps their rival in the part of their vision that best detects movement.

Interestingly, the team found that–even in the midst of combat–dragonflies spent at least a third of their time gliding. It’s unclear whether they glide to conserve energy or because it’s easier to track a rival when gliding.

The authors dig into the control rules needed for dragonflies to execute these chases and found that even relatively simple control schemes–constrained by the dragonfly’s physical limits–result in complex flight contests. (Image and research credit: S. Fabian et al.; via Ars Technica)

Dragonfly Dogfights

Like fighter pilots of old, male dragonflies engage in aerial combat where each tries to outmaneuver the other to keep a sight on their rival’s tail. A recent study observed this combat in the field and uncovered some surprising similarities to dogfighting. Like pilots, dragonflies used spiraling turns and other high-g moves to gain an advantageous position behind the other. In human combat, that position favors the forward-facing weapons of the pilot in back; for dragonflies, it keeps their rival in the part of their vision that best detects movement.

Interestingly, the team found that–even in the midst of combat–dragonflies spent at least a third of their time gliding. It’s unclear whether they glide to conserve energy or because it’s easier to track a rival when gliding.

The authors dig into the control rules needed for dragonflies to execute these chases and found that even relatively simple control schemes–constrained by the dragonfly’s physical limits–result in complex flight contests. (Image and research credit: S. Fabian et al.; via Ars Technica)

Salt and Dunes

Photographer Barbara Brown captured these striking aerial views in Namibia. Coastal dunes and saltworks feature in the photos from Walvis Bay, where wind, waves, evaporation, and humankind have shaped the landscape. The colorful and dendritic dune images come from Sossusvlei, where the ephemeral Tsauchab River ends in the Namib Desert. Recent flooding left its mark on the dry landscape. (Image credit: B. Brown/IAPOTY; via Colossal)

Salt and Dunes

Photographer Barbara Brown captured these striking aerial views in Namibia. Coastal dunes and saltworks feature in the photos from Walvis Bay, where wind, waves, evaporation, and humankind have shaped the landscape. The colorful and dendritic dune images come from Sossusvlei, where the ephemeral Tsauchab River ends in the Namib Desert. Recent flooding left its mark on the dry landscape. (Image credit: B. Brown/IAPOTY; via Colossal)

Microplastics in the Water Column

Of the more than 9 billion metric tons of plastic that’s been produced, a mere 9% has been recycled. About 12% has been incinerated, and the remainder is just out there–in our homes, our landfills, and, unfortunately, in our oceans. Exactly where all the plastic is continues to be an active question of research.

Plastic’s density is similar to that of water; some versions are a little denser than water, and some are a little lighter. So whether a piece of plastic floats at the ocean surface or sinks to the bottom depends on several factors, including its density, size, and shape. A large, dense plastic–think laundry detergent bottles–can float if it displaces enough water; after all, metal ships float!

But as sunlight and abrasion breaks that big container into smaller fragments, their buoyancy shrinks. Eventually, these small, millimetric pieces sink, carrying our pollution to ecosystems we once thought remote. Some of the highest rates of microplastic ingestion are found in nonmigratory species living between 1200 and 1500 meters below the surface. We may never visit those depths, but our garbage does. (Image credit: iStock/dottedhippo; via Eos)

Microplastics in the Water Column

Of the more than 9 billion metric tons of plastic that’s been produced, a mere 9% has been recycled. About 12% has been incinerated, and the remainder is just out there–in our homes, our landfills, and, unfortunately, in our oceans. Exactly where all the plastic is continues to be an active question of research.

Plastic’s density is similar to that of water; some versions are a little denser than water, and some are a little lighter. So whether a piece of plastic floats at the ocean surface or sinks to the bottom depends on several factors, including its density, size, and shape. A large, dense plastic–think laundry detergent bottles–can float if it displaces enough water; after all, metal ships float!

But as sunlight and abrasion breaks that big container into smaller fragments, their buoyancy shrinks. Eventually, these small, millimetric pieces sink, carrying our pollution to ecosystems we once thought remote. Some of the highest rates of microplastic ingestion are found in nonmigratory species living between 1200 and 1500 meters below the surface. We may never visit those depths, but our garbage does. (Image credit: iStock/dottedhippo; via Eos)

Fluid dynamics is the subdiscipline of fluid mechanics that studies the macroscopic physical behavior of liquids and gases in motion. Its primary goal is to quantitatively describe, model, and predict the physical properties of fluids—such as velocity, pressure, density, and temperature—as continuous functions of space and time.
#FluidDynamics #Physics #sflorg
https://www.sflorg.com/2026/08/cat08012602.html

Fluid dynamics is the subdiscipline of fluid mechanics that studies the macroscopic physical behavior of liquids and gases in motion. Its primary goal is to quantitatively describe, model, and predict the physical properties of fluids—such as velocity, pressure, density, and temperature—as continuous functions of space and time.
#FluidDynamics #Physics #sflorg
https://www.sflorg.com/2026/08/cat08012602.html

Ice Giant or Magma Ocean World?

Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

Ice Giant or Magma Ocean World?

Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

Giant Water Balloon to the Face

It’s the summertime, so Gav and Dan of the Slow Mo Guys are back to experimenting with giant water balloons. In this video, they send several careening down a slope into Dan’s face. Watching the balloons descend and pop is (unsurprisingly) my favorite part. It’s neat to see how the elasticity of the balloon acts like a beefed-up surface tension to make this enormous blob of water act like an oversized droplet. (Video and image credit: The Slow Mo Guys)

Giant Water Balloon to the Face

It’s the summertime, so Gav and Dan of the Slow Mo Guys are back to experimenting with giant water balloons. In this video, they send several careening down a slope into Dan’s face. Watching the balloons descend and pop is (unsurprisingly) my favorite part. It’s neat to see how the elasticity of the balloon acts like a beefed-up surface tension to make this enormous blob of water act like an oversized droplet. (Video and image credit: The Slow Mo Guys)

One of the most complex #visualizations of #Earth’s ocean dynamics to date, by #NASA.

Leveraging #satellite #altimetry, #scatterometry, and state-of-the-art numerical #ocean #models, the #map exposes the planet’s vast current systems: oceanic jets, #mesoscale eddies spanning hundreds of kilometers, and the Gulf Stream.

(Looks quite a bit like Van Gogh’s Starry Night! Yet, this is pure fluid dynamics, no #AI involved.)

Video cut: Gregory Bufithis

#Oceanography #FluidDynamics #DataViz

One of the most complex #visualizations of #Earth’s ocean dynamics to date, by #NASA.

Leveraging #satellite #altimetry, #scatterometry, and state-of-the-art numerical #ocean #models, the #map exposes the planet’s vast current systems: oceanic jets, #mesoscale eddies spanning hundreds of kilometers, and the Gulf Stream.

(Looks quite a bit like Van Gogh’s Starry Night! Yet, this is pure fluid dynamics, no #AI involved.)

Video cut: Gregory Bufithis

#Oceanography #FluidDynamics #DataViz

Múlajökull

Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

Múlajökull

Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

Convection Inside the Mantle

Most of what we know about Earth’s interior comes from observing how seismic waves–mostly from earthquakes–bounce around. As our observations have gotten better–more seisometers, better imaging techniques–scientists have identified two large anomalies sitting near the bottom of the mantle. Known as large low-velocity provinces, or LLVPs, these zones take up continent-sized areas beneath parts of Africa and the Pacific.

The LLVPs are hot, which would normally make them buoyant, but their stationary nature suggests they are made up of extremely dense material. Narrow plumes of hot material make their way up from the LLVPs to form volcanic hotspots like those that made the Hawaiian and Galapagos Islands. Balancing that upward convection is the downward convection of former tectonic material carried into the mantle at subduction zones.

What the LLVPs are made of remains an active research question. One suggestion is that they contain remnants of Theia, the planet thought to have impacted the proto-Earth to form our Moon. (Image credits: E. Garnero and C. Richardson; see also Physics Today)

Convection Inside the Mantle

Most of what we know about Earth’s interior comes from observing how seismic waves–mostly from earthquakes–bounce around. As our observations have gotten better–more seisometers, better imaging techniques–scientists have identified two large anomalies sitting near the bottom of the mantle. Known as large low-velocity provinces, or LLVPs, these zones take up continent-sized areas beneath parts of Africa and the Pacific.

The LLVPs are hot, which would normally make them buoyant, but their stationary nature suggests they are made up of extremely dense material. Narrow plumes of hot material make their way up from the LLVPs to form volcanic hotspots like those that made the Hawaiian and Galapagos Islands. Balancing that upward convection is the downward convection of former tectonic material carried into the mantle at subduction zones.

What the LLVPs are made of remains an active research question. One suggestion is that they contain remnants of Theia, the planet thought to have impacted the proto-Earth to form our Moon. (Image credits: E. Garnero and C. Richardson; see also Physics Today)

Even Penguins Love Bubbles

Walter, a young African penguin at the New York Aquarium, loves soap bubbles. In fairness to Walter, so do most people I’ve met. There’s just something that feels a bit magical about these ephemeral rainbow spheres that pop at a (dry) touch.

Bubbles owe their colors to thin film interference–the colors actually indicate how thick the bubble film is–and their stability (and fast disintegration) to surface tension. With schlieren photography or flow visualization, watching bubbles gets even cooler. Do you suppose a penguin would appreciate bubbles popping at 50,000 fps? (Image credit: New York Aquarium; via PopSci)

Even Penguins Love Bubbles

Walter, a young African penguin at the New York Aquarium, loves soap bubbles. In fairness to Walter, so do most people I’ve met. There’s just something that feels a bit magical about these ephemeral rainbow spheres that pop at a (dry) touch.

Bubbles owe their colors to thin film interference–the colors actually indicate how thick the bubble film is–and their stability (and fast disintegration) to surface tension. With schlieren photography or flow visualization, watching bubbles gets even cooler. Do you suppose a penguin would appreciate bubbles popping at 50,000 fps? (Image credit: New York Aquarium; via PopSci)

Where Waves Carry Plastics

The classic theory of steady wave motion predicts a phenomenon called Stokes drift, in which particles spread horizontally in the direction of wave travel. That means that something like microplastics will drift in the direction that waves are traveling. But in the real world, ocean waves aren’t quite so neat and unchanging. A new study looks at what happens when waves are decaying in strength–in other words, what happens in our world when the wind dies down.

In those circumstances, the researchers found that particles did not just drift horizontally–they drifted vertically, too. Further, how much a particle drifts vertically depends on its initial depth. Since plastics vary in their buoyancy–and can be found in varying numbers and sizes throughout the upper layer of the ocean–this mechanism could significantly affect how waves mix and transport pollution. (Image credit: N. Jensen; research credit: T. Izawa et al.; via Physics World)

Where Waves Carry Plastics

The classic theory of steady wave motion predicts a phenomenon called Stokes drift, in which particles spread horizontally in the direction of wave travel. That means that something like microplastics will drift in the direction that waves are traveling. But in the real world, ocean waves aren’t quite so neat and unchanging. A new study looks at what happens when waves are decaying in strength–in other words, what happens in our world when the wind dies down.

In those circumstances, the researchers found that particles did not just drift horizontally–they drifted vertically, too. Further, how much a particle drifts vertically depends on its initial depth. Since plastics vary in their buoyancy–and can be found in varying numbers and sizes throughout the upper layer of the ocean–this mechanism could significantly affect how waves mix and transport pollution. (Image credit: N. Jensen; research credit: T. Izawa et al.; via Physics World)

Bio-inspired mechano-fluidic metamaterials are artificially engineered structures designed to simultaneously optimize load-bearing mechanical strength and smooth fluid flow dynamics.
#MechanicalEngineering #MaterialsScience #FluidDynamics #Biomimetics #sflorg
https://www.sflorg.com/2026/07/eng07212601.html

Bio-inspired mechano-fluidic metamaterials are artificially engineered structures designed to simultaneously optimize load-bearing mechanical strength and smooth fluid flow dynamics.
#MechanicalEngineering #MaterialsScience #FluidDynamics #Biomimetics #sflorg
https://www.sflorg.com/2026/07/eng07212601.html

Making Quieter Shock Waves

NASA’s X-59 aircraft is intended to demonstrate supersonic flight without the boom. Although it’s broken into supersonic speeds, we haven’t yet heard its “sonic thump” because, so far, it’s been accompanied by conventional supersonic aircraft, which are louder.

The idea behind the long, skinny X-59 is to create weaker, widely-spaced shocks along the aircraft body. Weaker shocks are easier for atmospheric effects to damp out before they reach the ground, and spacing them out makes it harder for them to “pile up” at the nose and tail to create the strong double shocks that merge into a sonic boom.

NASA is preparing to test the X-59’s in-flight shocks soon, including with in-air schlieren photography like they’ve done in the past for other aircraft. But we’ve already have a glimpse of what to expect, thanks to wind tunnel testing, shown above. Ignore the three dark diagonal lines in the middle of the image (those are from the wind tunnel, not the model aircraft), and focus instead on the thin bright lines coming off the plane. Those are some impressively subtle shock waves!

Hear more from the aircraft’s designer and test pilots in this Ars Technica article. (Image credit: NASA; see also: Ars Technica, M. Ahaus et al.)

Making Quieter Shock Waves

NASA’s X-59 aircraft is intended to demonstrate supersonic flight without the boom. Although it’s broken into supersonic speeds, we haven’t yet heard its “sonic thump” because, so far, it’s been accompanied by conventional supersonic aircraft, which are louder.

The idea behind the long, skinny X-59 is to create weaker, widely-spaced shocks along the aircraft body. Weaker shocks are easier for atmospheric effects to damp out before they reach the ground, and spacing them out makes it harder for them to “pile up” at the nose and tail to create the strong double shocks that merge into a sonic boom.

NASA is preparing to test the X-59’s in-flight shocks soon, including with in-air schlieren photography like they’ve done in the past for other aircraft. But we’ve already have a glimpse of what to expect, thanks to wind tunnel testing, shown above. Ignore the three dark diagonal lines in the middle of the image (those are from the wind tunnel, not the model aircraft), and focus instead on the thin bright lines coming off the plane. Those are some impressively subtle shock waves!

Hear more from the aircraft’s designer and test pilots in this Ars Technica article. (Image credit: NASA; see also: Ars Technica, M. Ahaus et al.)

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

Pacific Surf

Life in Venice Beach lends itself to wave-watching, or so it seems for photographer Craig Hubbard. His portraits of waves and surfers are ethereal, every swell capped by a cloud-like swath of spray. Somehow, every photographer seems to capture breaking waves a little differently! (Image credit: C. Hubbard; via Colossal)

Pacific Surf

Life in Venice Beach lends itself to wave-watching, or so it seems for photographer Craig Hubbard. His portraits of waves and surfers are ethereal, every swell capped by a cloud-like swath of spray. Somehow, every photographer seems to capture breaking waves a little differently! (Image credit: C. Hubbard; via Colossal)

Researchers have developed a novel mechanism that uses interfacial water flow to induce the controlled, unidirectional rotation of floating microscopic objects, enabling the contact-free assembly of ultra-fine fibers into bundles.
#Microtechnology #FluidDynamics #MaterialsScience #Physics #sflorg
https://www.sflorg.com/2026/07/mcrt07172601.html

Researchers have developed a novel mechanism that uses interfacial water flow to induce the controlled, unidirectional rotation of floating microscopic objects, enabling the contact-free assembly of ultra-fine fibers into bundles.
#Microtechnology #FluidDynamics #MaterialsScience #Physics #sflorg
https://www.sflorg.com/2026/07/mcrt07172601.html

A Fluidic Space Telescope

A telescope’s resolution is set by the size of its reflective surface. Our largest space telescope, JWST, has a 6.5-meter reflector, the largest we could manage given manufacturing constraints and the need to launch it in a rocket. To reach even larger sizes, researchers are considering a new type of reflector: one made of liquid.

A fluidic telescope has some obvious advantages: surface tension makes it atomically smooth, and liquids can be packed into any convenient shape for launch. But there are challenges, also. Like, what happens to the reflector when you point it in an new direction?

That’s what this study looks at, mathematically. Using a mathematical model of a 50-meter-wide, millimeter-thick fluid, the researchers analyzed how different maneuvers over the telescope’s lifetime would affect the image quality.

Shifting the reflector creates perturbations in the surface, initially at the mirror’s edges. Over time, those perturbations move toward the center of the mirror and, at the same time, decay. The team found that, while typical space telescope operations distorted parts of the mirror beyond the limits of good optical quality, the inner 80% of the mirror could remain undisturbed for twenty or more years. That would be like having a 40-meter telescope in orbit with more than 6x the resolution of JWST. (Image credit: NASA; research credit: I. Gabay et al.)

A Fluidic Space Telescope

A telescope’s resolution is set by the size of its reflective surface. Our largest space telescope, JWST, has a 6.5-meter reflector, the largest we could manage given manufacturing constraints and the need to launch it in a rocket. To reach even larger sizes, researchers are considering a new type of reflector: one made of liquid.

A fluidic telescope has some obvious advantages: surface tension makes it atomically smooth, and liquids can be packed into any convenient shape for launch. But there are challenges, also. Like, what happens to the reflector when you point it in an new direction?

That’s what this study looks at, mathematically. Using a mathematical model of a 50-meter-wide, millimeter-thick fluid, the researchers analyzed how different maneuvers over the telescope’s lifetime would affect the image quality.

Shifting the reflector creates perturbations in the surface, initially at the mirror’s edges. Over time, those perturbations move toward the center of the mirror and, at the same time, decay. The team found that, while typical space telescope operations distorted parts of the mirror beyond the limits of good optical quality, the inner 80% of the mirror could remain undisturbed for twenty or more years. That would be like having a 40-meter telescope in orbit with more than 6x the resolution of JWST. (Image credit: NASA; research credit: I. Gabay et al.)

Mirabilite Mounds at Great Salt Lake

In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

Mirabilite Mounds at Great Salt Lake

In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

Can geometry control where and when condensed water drips?

Researchers from the @UniversitedeLiege Matteo Leonard and Nicolas Vandewalle, show that simple grooves can turn random edge dripping into regular, predictable release, opening new possibilities for dew harvesting and passive cooling.

🔗 https://pubs.acs.org/doi/10.1021/acs.langmuir.6c00977

#Condensation #FluidDynamics #HeatTransfer #SurfaceEngineering #geometry

Can geometry control where and when condensed water drips?

Researchers from the @UniversitedeLiege Matteo Leonard and Nicolas Vandewalle, show that simple grooves can turn random edge dripping into regular, predictable release, opening new possibilities for dew harvesting and passive cooling.

🔗 https://pubs.acs.org/doi/10.1021/acs.langmuir.6c00977

#Condensation #FluidDynamics #HeatTransfer #SurfaceEngineering #geometry

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ ICYMI: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ NEW: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

💁🏻‍♀️ NEW: 🐧🤖 Engineers at #MIT and #EPFL built a flapping-wing #robot that swims #underwater and flies into the air.

Inspired by diving #birds like #puffins, the small #vehicle folds its #wings to handle water density. This #technology could help scientists collect environmental samples from both air and #water.

👉 Learn more at https://seethis.tv/post/a-puffin-inspired-flapping-robot-that-swims-underwater-then-flies-into-the-air

#aerodynamics #animals #biomechanics #biomimicry #design #engineering #fluiddynamics #flying #locomotion #physics #research #science #tech #tksst #video

Droplets Can Climb Sugar Fibers

In nature, droplets and fibers can meet on a spider’s web, on fur, or on a dew-gathering cactus. Here, researchers explore what happens when the droplet can dissolve the fiber it’s suspended on. As the authors note, a lumberjack who cuts the branch they sit on makes a fatal choice. The droplet sees a different outcome.

As the droplet hangs on the fiber, it dissolves the fiber’s sugar. Dense, sugar-laden water flows downward along the fiber and a replenishing upward flow goes along the droplet’s exterior. Because the sugar concentration is lower near the top of the drop, the fiber thins most quickly there.

The droplet has capillary forces along its top and bottom, where it meets the fiber. At the top, the droplet is free to expand, wetting more fiber, but the bottom of the drop is pinned to the fiber. The excess capillary force there goes into compressing the fiber.

As soon as the fiber breaks, the capillary force is no longer balanced, and the droplet jumps upward. If the drop and fiber are sized just right, the drop will jump upward enough to stay attached to the fiber instead of falling off. (Image and research credit: S. Dorbolo et al.)

Droplets Can Climb Sugar Fibers

In nature, droplets and fibers can meet on a spider’s web, on fur, or on a dew-gathering cactus. Here, researchers explore what happens when the droplet can dissolve the fiber it’s suspended on. As the authors note, a lumberjack who cuts the branch they sit on makes a fatal choice. The droplet sees a different outcome.

As the droplet hangs on the fiber, it dissolves the fiber’s sugar. Dense, sugar-laden water flows downward along the fiber and a replenishing upward flow goes along the droplet’s exterior. Because the sugar concentration is lower near the top of the drop, the fiber thins most quickly there.

The droplet has capillary forces along its top and bottom, where it meets the fiber. At the top, the droplet is free to expand, wetting more fiber, but the bottom of the drop is pinned to the fiber. The excess capillary force there goes into compressing the fiber.

As soon as the fiber breaks, the capillary force is no longer balanced, and the droplet jumps upward. If the drop and fiber are sized just right, the drop will jump upward enough to stay attached to the fiber instead of falling off. (Image and research credit: S. Dorbolo et al.)

🚨BREAKING NEWS🚨: #Water isn't just for drinking! 🤯 Apparently, some smarty-pants scientists have discovered that simple fluids can actually #fracture. 🥴 Who knew liquid could be so rebellious? 📚🔬
https://www.quantamagazine.org/we-know-simple-fluids-can-flow-turns-out-some-can-fracture-20260710/ #Science #Discovery #LiquidResearch #FluidDynamics #HackerNews #ngated

🚨BREAKING NEWS🚨: #Water isn't just for drinking! 🤯 Apparently, some smarty-pants scientists have discovered that simple fluids can actually #fracture. 🥴 Who knew liquid could be so rebellious? 📚🔬
https://www.quantamagazine.org/we-know-simple-fluids-can-flow-turns-out-some-can-fracture-20260710/ #Science #Discovery #LiquidResearch #FluidDynamics #HackerNews #ngated

“Tadpoles: The Big Little Migration”

Amphibians like toads are often indicator species for their ecosystem because they are vulnerable to changes on both land and water. In this short film, videographer Maxwel Hohn follows the migration of western toad tadpoles in British Columbia, showing their daily underwater journey from deep waters, where they can hide, to warmer, shallow waters, where they eat. Over the days and weeks of their early life, millions of tadpoles make the journey, their bodies morphing as they do. Eventually, they will hop away as toadlets. (Video and image credit: M. Hohn et al.)

“Tadpoles: The Big Little Migration”

Amphibians like toads are often indicator species for their ecosystem because they are vulnerable to changes on both land and water. In this short film, videographer Maxwel Hohn follows the migration of western toad tadpoles in British Columbia, showing their daily underwater journey from deep waters, where they can hide, to warmer, shallow waters, where they eat. Over the days and weeks of their early life, millions of tadpoles make the journey, their bodies morphing as they do. Eventually, they will hop away as toadlets. (Video and image credit: M. Hohn et al.)

Burning Oil Spills With Fire Whirls

Though they are relatively infrequent, large marine oil spills, like 2010’s Deepwater Horizon, are devastating and incredibly difficult to clean up. In many locations, the “best” option for responding to such disasters is burning off the oil before it can absorb enough water to sink. But these floating fires leave behind unburned oil and produce soot. To enhance the burn, researchers are looking at the possibility of triggering large-scale fire whirls.

Often seen in wildfires, these fire vortices are intense and localized. Researchers made a more than 5-meter tall version in these experiments by arranging three walls that spun up the in-flowing air. The fire whirl sat above a pool of water topped in a layer of oil that served as the whirl’s fuel.

Within the whirl, the fire’s burn rate was 40% higher than a typical pool fire, and soot production was 40% lower–showing that fire whirls can burn cleaner. But the whirls are more finicky to start and maintain. It’s not yet clear whether such intense whirls are possible in the chaotic conditions on the ocean. (Research and image credit: W. Cui et al.; via Eos)

Burning Oil Spills With Fire Whirls

Though they are relatively infrequent, large marine oil spills, like 2010’s Deepwater Horizon, are devastating and incredibly difficult to clean up. In many locations, the “best” option for responding to such disasters is burning off the oil before it can absorb enough water to sink. But these floating fires leave behind unburned oil and produce soot. To enhance the burn, researchers are looking at the possibility of triggering large-scale fire whirls.

Often seen in wildfires, these fire vortices are intense and localized. Researchers made a more than 5-meter tall version in these experiments by arranging three walls that spun up the in-flowing air. The fire whirl sat above a pool of water topped in a layer of oil that served as the whirl’s fuel.

Within the whirl, the fire’s burn rate was 40% higher than a typical pool fire, and soot production was 40% lower–showing that fire whirls can burn cleaner. But the whirls are more finicky to start and maintain. It’s not yet clear whether such intense whirls are possible in the chaotic conditions on the ocean. (Research and image credit: W. Cui et al.; via Eos)

Fixing Mosul Dam

Keeping the water in a reservoir is an obvious challenge for any dam. But for Iraq’s Mosul Dam, it’s especially challenging because the dam was built on a foundation of gypsum, a highly water-soluble mineral. Since it was built, Mosul Dam’s water has been eating away at the underlying bedrock, making sinkholes, forcing gaps, and generally working its way out. That, obviously, creates a huge risk for dam failure and massive downstream flooding.

To get the dam stabilized–at least to a point where Iraqi engineers could keep up with filling the holes as they form–took a massive international engineering project, carried out in the shadow of armed conflict. (Video and image credit: Practical Engineering)

Fixing Mosul Dam

Keeping the water in a reservoir is an obvious challenge for any dam. But for Iraq’s Mosul Dam, it’s especially challenging because the dam was built on a foundation of gypsum, a highly water-soluble mineral. Since it was built, Mosul Dam’s water has been eating away at the underlying bedrock, making sinkholes, forcing gaps, and generally working its way out. That, obviously, creates a huge risk for dam failure and massive downstream flooding.

To get the dam stabilized–at least to a point where Iraqi engineers could keep up with filling the holes as they form–took a massive international engineering project, carried out in the shadow of armed conflict. (Video and image credit: Practical Engineering)

The Disappearing Great Salt Lake

Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

The Disappearing Great Salt Lake

Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)