Three-Dimensional Low Reynolds Number Flows near Biological Filtering and Protective Layers

• Published in: Fluids (Basel) Vol. 2; no. 4; p. 62
• Main Authors: Strickland, Christopher, Miller, Laura, Santhanakrishnan, Arvind, Hamlet, Christina, Battista, Nicholas, Pasour, Virginia
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.12.2017
• Subjects: Arrays; Blood; Blood flow; Boundary layer; Brinkman model; Computational fluid dynamics; Computer simulation; Cylinders; Endothelial cells; filtering layers; Filtration; Flow profiles; Fluid flow; Fluids; Free flow; Gases; glycocalyx; Heat exchange; Heat transfer; immersed boundary method; leakiness; Mathematical models; Mathematics; Organisms; porous flow; Porous media; Proteins; Reynolds number; Shear stress; Surface layers; Three dimensional flow; trichomes; Wind speed; United States > US
• ISSN: 2311-5521; 2311-5521
• DOI: 10.3390/fluids2040062

Mesoscale filtering and protective layers are replete throughout the natural world. Within the body, arrays of extracellular proteins, microvilli, and cilia can act as both protective layers and mechanosensors. For example, blood flow profiles through the endothelial surface layer determine the amount of shear stress felt by the endothelial cells and may alter the rates at which molecules enter and exit the cells. Characterizing the flow profiles through such layers is therefore critical towards understanding the function of such arrays in cell signaling and molecular filtering. External filtering layers are also important to many animals and plants. Trichomes (the hairs or fine outgrowths on plants) can drastically alter both the average wind speed and profile near the leaf’s surface, affecting the rates of nutrient and heat exchange. In this paper, dynamically scaled physical models are used to study the flow profiles outside of arrays of cylinders that represent such filtering and protective layers. In addition, numerical simulations using the Immersed Boundary Method are used to resolve the three-dimensional flows within the layers. The experimental and computational results are compared to analytical results obtained by modeling the layer as a homogeneous porous medium with free flow above the layer. The experimental results show that the bulk flow is well described by simple analytical models. The numerical results show that the spatially averaged flow within the layer is well described by the Brinkman model. The numerical results also demonstrate, however, that the flow can be highly three-dimensional with fluid moving into and out of the layer. These effects are not described by the Brinkman model and may be significant for biologically relevant volume fractions. The results of this paper can be used to understand how variations in density and height of such structures can alter shear stresses and bulk flows.