Nicole Sharp
Nicole Sharp

Celebrating the physics of all that flows with Nicole Sharp, Ph.D.

4,101 posts
325 followers
  • Pathlines vs. Streaklines

    When considering fluid motion, there are many ways to describe trajectories through the flow. One is the pathline, the trajectory followed by an individual fluid particle. Imagine releasing a rubber duck down a stream. Following the duck’s position over time would give you a pathline. Now imagine that instead of releasing a single rubber duck…

  • Bouncing Off The Surface

    For the right angles and flow rates, it’s possible to bounce a fluid jet off a pool of the same fluid. As the jet flows, it pulls a thin layer of air with it, entraining the air. This air film is what keeps the jet separate from the pool when it initially hits. In the…

  • Liquid Crystal Films

    Smectic liquid crystals can form extremely thin films, similar to a soap bubble, that are sensitive to electrically-induced convection. Here an annular smectic film lies between two electrodes. When a voltage is applied across it, positive and negative charges build up on the surface of the film near their respective electrodes. The electrical field surrounding…

  • APS DFD etc.

    It’s time! The American Physical Society’s Division of Fluid Dynamics meeting opens in Pittsburgh tomorrow morning. It promises to be a very busy few days. Most of that activity will probably not be immediate apparent here on FYFD, but I encourage you to follow along on @fyfluiddynamics, where I’ll be giving a running commentary. For…

  • Start Your Rocket Engine

    When supersonic flow is achieved through a wind tunnel or rocket nozzle, the flow is said to have “started”. For this to happen, a shock wave must pass through, leaving supersonic flow in its wake. The series of images above show a shock wave passing through an ideal rocket nozzle contour. Flow is from the…

  • The Glory of a Roll Cloud

    Roll clouds stretch like a long horizontal tube, spinning as they process across the sky. This class of arcus cloud is relatively rare but occasionally forms in areas where cool air is sinking, along the downdraft of an oncoming storm or in coastal regions as a result of sea breezes. The cooler, sinking air displaces…

  • Shocked Interfaces

    The Richtmyer-Meshkov instability occurs when two fluids of differing density are hit by a shock wave. The animation above shows a cylinder of denser gas (white) in still air (black) before being hit with a Mach 1.2 shock wave. The cylinder is quickly accelerated and flattened, with either end spinning up to form the counter-rotating vortices that dominate the instability.…

  • The Challenges of Trapping Carbon Dioxide

    One way to reduce carbon dioxide in the atmosphere is to pump the CO2 into saline aquifers deep below the surface. Such aquifers are thin but stretch over large areas and are sometimes gently sloping. Since carbon dioxide is relatively buoyant, it may migrate up-slope after injection and potentially leak elsewhere. Dissolving the carbon dioxide…

  • Volcanic Vortices from Etna

    Italy’s Mount Etna is erupting again, producing a series of beautiful vortex rings. Like a dolphin’s bubble ring or a vortex cannon, the volcano’s rings are formed when gases are rapidly expelled through a narrow opening. Such formations are extremely common but are generally not visible to the eye. In this case, steam has gotten…

  • Fluids Round-up – 16 November 2013

    Time for another fluids round-up. Here are your links: PhysicsBuzz takes a look at the use of plasma actuators to control airflow. Over at Deep Sea News, you can learn about parasitic capillary waves. NanoWerk reports on self-steering particles in microfluidic devices. The 9th drop of the Queensland pitch drop experiment–believed to be the longest continuously running experiment in…