Highlights

Shear joy of watching paint dry

R. C. Hurd, N. B. Speirs, J. Belden, Z. Pan, B. Lovett, W. Robinson, M. A. Zamora, S. I. Sharker, M. M. Mansoor, A. Merritt, and T. T. Truscott

Phys. Rev. Fluids 2, 090503 (2017) - Published 29 September, 2017

Sweeping jet from a fluidic oscillator in crossflow

Florian Ostermann, Philipp Godbersen, Rene Woszidlo, C. Navid Nayeri, and C. Oliver Paschereit

Phys. Rev. Fluids 2, 090512 (2017) - Published 29 September, 2017

On the rules for aquatic locomotion

M. Saadat, F. E. Fish, A. G. Domel, V. Di Santo, G. V. Lauder, and H. Haj-Hariri

Phys. Rev. Fluids 2, 083102 (2017) - Published 18 August, 2017

Why do most fish swim with a relatively constant tail-beat amplitude of approximately 20% of their body length while their speed is linearly correlated with their tail-beat flapping frequency? Scaling analysis and experiments show that this behavior is rooted in minimizing input power for swimming.

Prediction of blood back spatter from a gunshot in bloodstain pattern analysis

P. M. Comiskey, A. L. Yarin, S. Kim, and D. Attinger

Phys. Rev. Fluids 1, 043201 (2016) - Published 2 August, 2016

Theorists propose a model for predicting and interpreting blood spatter patterns resulting from gunshot wounds. The atomization process, the trajectories of the backspatter drops of blood from the wound to the ground, the impact angle and the impact Weber number on the ground, as well as the distribution and location of blood stains and their shape and sizes are predicted.

Spreading of miscible liquids

Daniel J. Walls, Simon J. Haward, Amy Q. Shen, and Gerald G. Fuller

Phys. Rev. Fluids 1, 013904 (2016) - Published 31 May, 2016

The spreading of sessile drops in miscible environments have distinctly different shape evolution and power law dynamics than sessile drops that spread in immiscible environments.

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.

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