Recent Articles

Contactless prompt tumbling rebound of drops from a sublimating slope

Carlo Antonini, Stefan Jung, Andreas Wetzel, Emmanuel Heer, Philippe Schoch, Ali Mazloomi Moqaddam, Shyam S. Chikatamarla, Ilya Karlin, Marco Marengo, and Dimos Poulikakos

Phys. Rev. Fluids 1, 013903 (2016) - Published 25 May, 2016

Experiments and simulations reveal that drops of highly viscous glycerol demonstrate a spectacular prompt tumbling rebound on sublimating slopes, bouncing like solid rocks while remaining in the liquid state, and rebounding much faster than low-viscosity liquid drops.

Quasisteady quasihomogeneous description of the scale interactions in near-wall turbulence

Chi Zhang and Sergei I. Chernyshenko

Phys. Rev. Fluids 1, 014401 (2016) - Published 25 May, 2016

A formal theory of scale interaction is presented. It links the superposition coefficient and the mean profile, explains why the log-law coefficients can depend on Re even though the log law itself is a Re-independent asymptotics, promises a method of interpolation to high Re, and more.

Motion of a hot particle in viscous fluids

Naomi Oppenheimer, Shahin Navardi, and Howard A. Stone

Phys. Rev. Fluids 1, 014001 (2016) - Published 18 May, 2016

A hot sphere creates a viscosity variation that couples to the sphere’s motion. A method for finding the leading order force and torque acting on the sphere for any thermal distribution is presented, showing, in particular, that rotation and translation are coupled for a thermal dipole (Janus sphere).

Dense spray evaporation as a mixing process

A. de Rivas and E. Villermaux

Phys. Rev. Fluids 1, 014201 (2016) - Published 18 May, 2016

Researchers demonstrate that the lifetime of an individual droplet embedded in a dense spray lamellae is much longer than that of a single drop evaporating in quiescent air, as described by the d2 law. An analogy is made with the way mixing times are understood for passive scalars in order to describe the lifetime of dense spray lamellae stretched in a dry environment.

Surfing on a herringbone

Dan Soto, Guillaume Lagubeau, Christophe Clanet, and David Quéré

Phys. Rev. Fluids 1, 013902 (2016) - Published 12 May, 2016

Evaporation of liquid on a hot solid causes droplets to levitate and self-propel, drawn by the underlying flow of vapor. Forcing an anisotropic flow of vapor using a herringbone pattern on a solid surface provides a simple geometry, allowing clarification of the underlying propulsion mechanism.

Adhesion and detachment of a capsule in axisymmetric flow

M. P. Keh and L. G. Leal

Phys. Rev. Fluids 1, 013201 (2016) - Published 9 May, 2016

The dynamics of adhesion and detachment of capsules is studied using scaling theories and a simulation technique that couples the nonhydrodynamic surface forces, membrane mechanics, and Stokes flow, and the results are contrasted against vesicles’ behavior.

Internal wave transmission through a thermohaline staircase

Bruce R. Sutherland

Phys. Rev. Fluids 1, 013701 (2016) - Published 9 May, 2016

A theoretical study indicates that large-scale waves within the ocean can travel through “staircases” of water density, a motion that could enhance ice melting at the surface.

Division of Fluid Dynamics Support of Physical Review Fluids

Ellen Longmire

Phys. Rev. Fluids 1, 010002 (2016) - Published 6 May, 2016

Editorial: Introducing Physical Review Fluids

Phys. Rev. Fluids 1, 010001 (2016) - Published 2 May, 2016

Clear salt water above sediment-laden fresh water: Interfacial instabilities

B. Schulte, N. Konopliv, and E. Meiburg

Phys. Rev. Fluids 1, 012301(R) (2016) - Published 2 May, 2016

Direct numerical simulations of the evolution of an interface separating less dense, clear salt water above from more dense, sediment-laden fresh water below, reveal that the destabilizing effects of double-diffusion and particle settling amplify each other above the diffusive interface, and tend to cancel each other below it.

Pressure evolution in the shear layer of forming vortex rings

Kristy Schlueter-Kuck and John O. Dabiri

Phys. Rev. Fluids 1, 012501(R) (2016) - Published 2 May, 2016

The phenomenon of vortex ring pinch-off is quantified by the formation number and its connection to the pressure in the shear layer feeding the vortex ring as it develops. Researchers find that the formation of a high-pressure region behind the vortex ring is a necessary but not sufficient condition for pinch-off, and they offer a method for estimating pinch-off by tracking the development of this high-pressure region.

Stress in a dilute suspension of spheres in a dilute polymer solution subject to simple shear flow at finite Deborah numbers

Donald L. Koch, Eric F. Lee, and Ibrahim Mustafa

Phys. Rev. Fluids 1, 013301 (2016) - Published 2 May, 2016

A theoretical analysis shows that polymers interacting with particles in a shear flow experience enhanced streamwise stretch that grows in amplitude and spatial extent with increasing Deborah number. This results in shear thickening of the viscosity and first normal stress coefficient of a particle suspension in a Boger fluid.

Drop impact of shear thickening liquids

François Boyer, Enrique Sandoval-Nava, Jacco H. Snoeijer, J. Frits Dijksman, and Detlef Lohse

Phys. Rev. Fluids 1, 013901 (2016) - Published 2 May, 2016

An investigation of the droplet impact of a non-Newtonian, shear-thickening liquid such as a cornstarch suspension reveals a freezing-like behavior at impact, following by a gentle and slow spreading, very different behavior from a Newtonian liquid. Identifying the dissipative mechanisms in such a droplet allows this counterintuitive behavior to be modeled and understood.

Internal wave pressure, velocity, and energy flux from density perturbations

Michael R. Allshouse, Frank M. Lee, Philip J. Morrison, and Harry L. Swinney

Phys. Rev. Fluids 1, 014301 (2016) - Published 2 May, 2016

A Green’s-function-based method for computing the instantaneous velocity, pressure, and baroclinic energy flux strictly from measurements of the density perturbation field represents an important improvement with respect to existing techniques. Energy flux measurements are vital to interpreting the contribution of internal waves to the ocean’s energy budget.

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