FI22                         My Program 


Flow-Induced Instabilities and Non-Newtonian Fluids


Drawing parallels: Small-scale canopy elastic turbulence versus large-scale inertial turbulence


October 15, 2024 (Tuesday) 11:10


Track 5 / Room 405

(Click on name to view author profile)

  1. Lopez de la Cruz, Ricardo A. (Okinawa Institute of Science and Technology Graduate Univers)
  2. Haward, Simon J. (Okinawa Institute of Science and Technology Graduate Univers, Micro,Bio,Nanofluidics Unit)
  3. Shen, Amy Q. (Okinawa Institute of Science and Technology Graduate Univers, Micro,Bio,Nanofluidics Unit)

(in printed abstract book)
Ricardo A. Lopez de la Cruz, Simon J. Haward and Amy Q. Shen
Micro,Bio,Nanofluidics Unit, Okinawa Institute of Science and Technology Graduate Univers, Onna-son, Okinawa 904-0495, Japan


Lopez de la Cruz, Ricardo A.


flow-induced instabilities; non-Newtonian fluids; polymer solutions


Since its discovery nearly two decades ago, elastic turbulence (ET) has been extensively investigated across various systems with diverse geometries, spanning curved and straight channels, as well as porous media. Recognized for its parallels with inertial turbulence and its potential applications in microfluidics, ET has garnered significant interest in elucidating the conditions triggering it, its flow dynamics, and its interplay with inertial turbulence. While progress has been notable in curved geometries, questions persist regarding straight channels and more intricate systems. Here, we investigate the latter scenario, specifically exploring a canopy within a microfluidic device, drawing upon insights gleaned from simpler flows. Our investigation begins with examining the flow characteristics of a viscoelastic fluid at varying Weissenberg numbers, revealing distinct flow regimes dictated by the rheological properties of the fluid and flow conditions. Focusing on the ET regime, we study the mean and fluctuating velocity fields, observing a delineation of the flow into distinct regions reminiscent of porous media within the canopy, a mixing-layer-like flow at the canopy tips, channel flow away from the canopy, and a transitional zone between the mixing layer and channel flow in the presence of ET. Local fitting of the average flow profiles with models corresponding to specific flow types—Brinkman equation, hyperbolic tangent, and Poiseuille profile—illustrates the flow dynamics at each location. Lastly, we assess the robustness of these models under variations in canopy geometry and fluid rheology. Our findings demonstrate that the complex ET flow in such systems can be effectively characterized by leveraging simpler analogues and drawing insights from conventional turbulence, thereby enhancing our understanding of real-world scenarios like cilia in bacteria or within mammalian bodies.