When two jets of liquid collide, they form a sheet of fluid. As the speeds of the jets change, the sheet can become unstable, forming a set of liquid ligaments and droplets that look like a fish’s bones. This is shown in the video above. For purposes of orienting yourself, flow in the video is moving right to left and the video has been rotated 90-degrees clockwise (i.e. the two out-of-frame jets forming the flow seen are falling due to gravity). (Video credit: Sungjune Jung, University of Cambridge)
Category: Phenomena
Soap Bubbles Bursting
To the human eye, the burst of a soap bubble appears complete and instantaneous, but high-speed video reveals the directionality of the process. Surface tension is responsible for the spherical shape of the bubble, and, when the bubble is pierced, surface tension is broken, causing the soap film that was the bubble to contract like elastic that’s been stretched and released. Droplets of liquid fly out from the edges of the sheet until it atomizes completely.
Stalling a Wing
At small angles of attack, air flows smoothly around an airfoil, providing lifting force through the difference in pressure across the top and bottom of the airfoil. As the angle of attack increases, the lift produced by the airfoil increases as well but only to a point. Increasing the angle of attack also increases the adverse pressure gradient on the latter half of the top surface, visible here as an increasingly thick bright area. Over this part of the surface, the pressure is increasing from low to high–the opposite of the direction a fluid prefers to flow. Eventually, this pressure gradient grows strong enough that the flow separates from the airfoil, creating a recirculating bubble of air along much of the top surface. When this happens, the lift produced by the airfoil drops dramatically; this is known as stall.
Breaking Water with Sound
Previously we saw how vibration could atomize a water droplet, breaking it into a spray of finer droplets. Here astronaut Don Pettit shows us what the process looks like in microgravity using some speakers and large water droplets. At low frequencies the water displays large wavelength capillary waves and vertical vibrations. Higher frequencies–like the earthbound experiment on much smaller droplets–cause fine droplets to eject from the main drop when surface tension can no longer overcome their kinetic energy. (submitted by aggieastronaut, jshoer and Jason C)
(Source: /)Surface Tension Floats Coins
Surface tension arises from intermolecular forces along the interface of a fluid, but despite its molecular origins, it can have some substantial macroscopic effects. Here researchers demonstrate how surface tension can hold up metal coins that would otherwise sink. Moreover, when multiple coins are set on the surface of the water, surface tension draws them together into a closely packed array because it reduces the surface energy by creating a single large well instead of many small ones. This is the same reason that your Cheerios tend to clump together on the surface of your milk when you’re eating breakfast! (Video credit: Lawrence Berkeley National Lab)
How Are Sea Waves Created?
There are many different kinds of sea waves, some of which have fluid dynamical origins and some of which don’t. For example, tsunamis are caused by the sudden displacement of the ocean floor caused by earthquakes and the tides are caused by the pull of the moon on Earth’s oceans. But many of the waves we are accustomed to seeing are caused by the wind moving across open water, whether in the ocean, in a lake or a sea, or even a river or pond. When the wind blows across the free surface of the water, the difference in velocity between the two fluids causes shearing and the development of surface waves as a result of the Kelvin-Helmholtz instability. (Incidentally, this is why other examples of the K-H instability look so much like ocean waves.)
These wind-generated waves can take several forms. Ripples–or capillary waves–remain visible only as long as the wind is blowing. But under steady conditions, or after the wind has affected a large enough area, waves can form that will persist at the surface even if the wind stops blowing. At that point, even though the wind generated the waves, it is gravity that allows them to persist. This is the source of most of the waves we see on large bodies of water. (Photo credit: Travis Weins)
Barchan Dunes
The winds of Mars create sand dunes that seem to flow like a liquid across the planet’s surface. Here the wind blows from right to left around the flat top mesas on the right side of the image. The dark, arc-shaped dunes formed in the wake of the mesas are called barchans and can move downstream remarkably intact, even able to cross paths with other dunes. (Photo credit: MRO, NASA; via APOD)
Helicopter Vortices
When conditions are just right, the low pressure at the center of a wingtip vortex can drop the local temperature below the dew point, causing condensation to form. Here vortices are visible extending from the tips of the propellers in addition to the wingtip. Because of the spinning of the propeller and the forward motion of the airplane, the prop vortices extend backwards in a twisted spiral that will quickly break down into turbulence. The same behavior can be observed with helicopter blades. (Photo credit: benurs)
Convective Cells
Convective cells form as fluid is heated from below. As the fluid near the bottom warms, its density decreases and buoyancy causes it to rise while cooler fluid descends to replace it. This fluid motion due to temperature gradients is called Rayleigh-Benard convection and the cells in which the motion occurs are called Benard cells. This particular type of convection is essentially what happens when a pot is placed on a hot stove, so the shapes are familiar. Similar shapes also form on the sun’s photosphere, where they are called granules.
Supercritical Fluids
A supercritical fluid exists without a distinct liquid or gas phase and forms when temperatures and pressures exceed the substance’s critical point. Here supercritical transition is demonstrated with an ampule of liquid chlorine. When immersed in a hot bath, the temperature and pressure inside the ampule rises until around 0:20 when the meniscus marking the interface between liquid and gas disappears. The chlorine is now in its supercritical state. Around 0:43 the hot bath is removed and the chlorine begins to cool, reverting to distinct phases of matter around 0:55.
