shear flows
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2022 ◽  
Vol 64 ◽  
pp. 103446
Author(s):  
Paolo Falsaperla ◽  
Giuseppe Mulone ◽  
Carla Perrone
Keyword(s):  

2022 ◽  
Vol 7 (1) ◽  
Author(s):  
Kahlil F. E. Cui ◽  
Gordon G. D. Zhou ◽  
Lu Jing

2022 ◽  
Vol 128 (2) ◽  
Author(s):  
Martin Oberlack ◽  
Sergio Hoyas ◽  
Stefanie V. Kraheberger ◽  
Francisco Alcántara-Ávila ◽  
Jonathan Laux

2022 ◽  
Vol 128 (1) ◽  
Author(s):  
Lukasz Klotz ◽  
Grégoire Lemoult ◽  
Kerstin Avila ◽  
Björn Hof

2022 ◽  
Author(s):  
Casey Broslawski ◽  
Bryan Morreale ◽  
Rodney D. Bowersox ◽  
Gary Nicholson ◽  
Lian Duan

2022 ◽  
Author(s):  
Lu Zhao ◽  
Saeed Farokhi ◽  
Ray Taghavi

Soft Matter ◽  
2022 ◽  
Author(s):  
Qiang Zhu ◽  
Xiaobo Bi

By combining a multiscale structural model of erythrocyte with a fluid-cell interaction model based on the boundary-integral method, we numerically investigate the dynamic response of erythrocytes in oscillatory shear flows...


2021 ◽  
Vol 3 (4) ◽  
Author(s):  
Zhiyuan Zhao ◽  
Boyi Wang ◽  
Shigeyuki Komura ◽  
Mingcheng Yang ◽  
Fangfu Ye ◽  
...  
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2021 ◽  
Vol 104 (6) ◽  
Author(s):  
Meng Liu ◽  
Christoph R. Müller

2021 ◽  
Vol 932 ◽  
Author(s):  
Philip Hall

A strongly nonlinear theory describing the effect of small amplitude boundary forcing in the form of waves on high Reynolds number shear flows is given. The interaction leads to an $O(1)$ change in the unperturbed flow and is relevant to a number of forcing mechanisms. The cases of the shear flow being bounded or unbounded are both considered and the results for the unbounded case apply to quite arbitrary flows. The instability criterion for unbounded flows is expressed in terms of the wall forcing and the friction Reynolds number. As particular examples we investigate wall transpiration or surface undulations as sources of the forcing and both propagating and stationary waves are considered. Results are given for propagating waves with crests perpendicular to the flow direction and for stationary waves with crests no longer perpendicular to the flow direction. In the first of those situations we find the instability induced by transpiration waves is independent of the propagation speed. For wavy walls downstream propagation completely stabilises the flow at a critical speed whereas upstream propagation greatly destabilises the flow. For stationary oblique waves we find that the instability is enhanced and a much wider range of unstable wavenumbers exists. For the bounded case with a wall of fixed wavelength we identify a critical wavelength where the most dangerous mode switches from the aligned to the oblique configuration. For the transpiration problem in the oblique configuration a strong resonance occurs when the vortex wavelength coincides with the spanwise wavelength of the forcing.


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