FYFD

Search results for: “art”

  • Tumbling in Air

    Tumbling in Air

    When snowflakes and volcanic ash fall, they tumble. Historically, it’s been too hard to observe this behavior first hand — the particles are too small to easily follow with a camera — so scientists instead looked at larger particles falling through water. That change preserves important characteristics of the physics, but it misses out on one key feature: in air, the density of the falling particle is much higher than air’s.

    A football-shaped particle wobbles around its stable orientation as it falls through air.
    A football-shaped particle wobbles around its stable orientation as it falls through air.

    To account for that, researchers built a special apparatus that drops particles one-at-a-time through the field of view of four high-speed cameras. This setup gave them a narrow 1-mm band where they could track a falling particle’s orientation — provided the particle fell through the band, which happened about 20% of the time. Their results show that particles in air tumble and oscillate back and forth around their stable orientation more than in water experiments. This difference affects how quickly particles settle, which, in turn, affects how much they tend to clump and grow. (Image credit: snow – A. Burden, experiment – T. Bhowmick et al.; research credit: T. Bhowmick et al.; via APS Physics)

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    Icelandic Eruption

    When I started FYFD, volcano footage was far rarer. These days the affordability and durability of drones and action cameras — along with the relative accessibility of eruptions in places like Iceland and Hawaii — means we get to see volcanic flows in glorious high definition. This footage comes from the recent Icelandic eruption on the Reykjanes peninsula. Lava fountains line the four-kilometer lava vent seen here, and flows from the vent spread into a delta-like fan in the field below. I never get tired of staring at molten rock that flows like water. (Video and image credit: I. Finnbogason; via Colossal)

  • Water Reduces Coffee’s Charge

    Water Reduces Coffee’s Charge

    Grinding coffee beans builds up electrical charge as the beans fracture into smaller and smaller pieces. The polarity of the charge depends on the bean’s moisture content; lighter roasts tend toward a positive charge, and darker roasts skew negative. The finer the grind, the stronger the electrical charge and the greater the problem of clumping grains becomes. Adding a few drops of water to the beans before grinding, researchers found, drastically reduces the electrical charge and clumping. This, the team reports, would let espresso lovers brew a stronger cup with less material. A well-compacted bed of unclumped grains has less void space, which slows down water’s percolation and increases the amount of coffee the water can extract. The authors encourage readers to try adding water in their own home brews, but they caution that coffee mass and grind setting should also be variables in the experiment. (Image credit: N. Van; research credit: J. Harper et al.; via APS Physics)

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    Visualizing Changes

    This rather mesmerizing video by Michiel de Boer uses a video editing technique to highlight movement and changes in video clips. From falling rain to rising mist to passing footsteps, the relatively simple technique visualizes all kinds of motion. De Boer calls it “motion extraction,” but it’s essentially a way to play with autocorrelation, a mathematical technique often used in fluid dynamics. It’s especially prevalent in turbulence, where it helps researchers identify parts of the flow that are closely related to one another. (Video and image credit: M. de Boer; via Colossal)

  • Reimagining Mars’ Interior

    Reimagining Mars’ Interior

    Older models of Mars assumed a liquid metal core beneath a solid mantle of silicates, but recent studies indicate that structure is missing at least one layer. Using data from the InSight lander’s seismometer, two teams independently calculated that a liquid silicate layer must surround the planet’s core. In September 2021, three meteorite pieces impacted Mars far from the InSight lander’s position. Since the Mars Reconnaissance Orbiter could exactly pinpoint the impact location, researchers were able to calculate just how long it took seismic waves from the impact to reach the lander.

    Like on Earth, Mars has two varieties of seismic wave: transverse S-waves that only travel through solids and longitudinal P-waves that travel through both liquid and solid layers. S-waves reflect off any liquid-solid boundary, following a different path to a seismometer than P-waves that refract across the boundary and travel through liquid. For more of the story behind this discovery, check out this article at Physics Today. (Image credit: Mars – NASA/JPL-Caltech/University of Arizona, illustration – J. Sieben/J. Keisling; research credit: H. Samuel et al. and A. Khan et al.; via Physics Today)

    An illustration of Mars' interior and the paths followed by seismic waves before InSight picked them up.
    An illustration of Mars’ interior and the paths followed by seismic waves before InSight picked them up.
  • February Events

    February Events

    I have a couple of public(ish) events coming up this month, so I wanted to share the details for anyone interested in joining.

    Exploring By The Seat Of Your Pants – Feb 16

    This virtual event is part of a series of talks by myself and other AAAS IF/THEN ambassadors about our STEM careers. It’s geared toward K-12 classrooms, and any teachers who want to bring their class to my session (or another one) can register here. If you’d just like to tune in on your own, you can do that here. My talk takes place starting at 2:00pm Eastern time, and I’ll be discussing what I do as a science communicator, how I got here, and what traits might make you a good science communicator, too.

    Improbable Research Show – Feb 17

    The AAAS conference is in Denver this year, and I’m making a return to the annual Improbable Research show held at the conference. This will be a live event only. It’s free to attend, but I believe registration is required. The show begins at 8:00pm Mountain time, but in years past, showing up early has been required to get a seat. I’ll be talking about past Ig Nobel prize winners that connect to fluid dynamics. Like the Igs themselves, you can expect this show to be a little zany.

    (Image credit: Lyda Hill Philanthropies)

  • Upwelling at Cabo Frio

    Upwelling at Cabo Frio

    The shores of the Brazilian state of Rio de Janeiro boast turquoise waters, white sands, and green lagoons, but European explorers discovered the waters around one promontory were unusually cold, leading to the name Cabo Frio. The chilly waters can be 8 degrees Celsius cooler than nearby surface temperatures, thanks to cold water upwelling near the coast. The upwelling is wind-driven; the dominant northeasterly winds push water out to sea, allowing colder waters to rise from the deep. (Image credit: L. Dauphin; via NASA Earth Observatory)

    A map of sea surface temperatures near Cabo Frio in Brazil.
    A map of sea surface temperatures near Cabo Frio in Brazil.
  • Flexy Fur Foils Fouling

    Flexy Fur Foils Fouling

    Inspired by a muddy hike with a dog, today’s study looks at how fur in a flow can shed dirt and debris. Researchers placed beaver, coyote, and synthetic hairs in a flow chamber with a slurry of titanium dioxide particles in water. After 24 hours, they counted the particles stuck on each hair. The more flexible a hair, the cleaner it stayed. Long hairs collected fewer particles per unit surface area than short ones, thanks to their larger deflection in the flow. The effect, they discovered, is a bit like when paint or glue dries on your hand. The more you move and flex your skin, the harder it is for crusty material to stick. This self-cleaning with flex and flow occurs in nature, too: the only furry mammal with consistently dirty fur is the notoriously inactive sloth. (Image credit: T. Umphreys; research credit: M. Krsmanovic et al.; via APS Physics)

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    The Miscible Faraday Instability

    Vibrate a pool of water in air and the interface will form a distinctive pattern of waves called the Faraday instability. But what happens when you vibrate the interface between two fluids that can mix? That’s the question at the heart of this video. The researchers consider the situation both in simulation and experiment, showing how what begins as a smooth interface quickly becomes a thick turbulent mixture. Since the thickness of that mixing layer can be predicted theoretically, this set-up could be useful in industrial applications where mixing is needed. (Video, image, and research credit: G. Louis et al.)

  • Fire in Ice

    Fire in Ice

    This false-color satellite image of Malaspina Glacier (Sít’ Tlein) is a riot of color. Composed of coastal/aerosol, near infrared, and shortwave infrared bands from Landsat 9, the colors highlight features otherwise hard to identify. Watery features appear in reds, oranges, and yellows; vegetation is green and rock appears in blue. The glacier covers more than 4000 square kilometers, an area larger than the state of Rhode Island. The dark lines atop the glacier are moraines, where rock, soil, and other debris has been scraped up along the glacier’s edge. Over time, changes in the glacier’s velocity cause the moraines to fold and shear, creating the zigzag pattern seen here. (Image credit: W. Liang; via NASA Earth Observatory)

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