Bulletin of the American Physical Society
73rd Annual Meeting of the APS Division of Fluid Dynamics
Volume 65, Number 13
Sunday–Tuesday, November 22–24, 2020; Virtual, CT (Chicago time)
Session J01: Focus Session: Fluid Dynamics in a Deformable Porous Medium (8:00am  8:45am CST)Interactive On Demand

Hide Abstracts 

J01.00001: Boundary conditions on a hydrogelfluid interface Jimmy Feng, YuanNan Young Hydrogels are an important class of soft material for biological, biomedical and MicroElectroMechanical Systems (MEMS) applications. Hydrogels are often deployed alongside fluids, thus the interfacial dynamics of a gelfluid system becomes an interesting question. Given the wide range in length scales, from the nanometer pore size in the gel to the dimension of a MEMS device (millimeters or more), it seems appropriate to model the hydrogel as a twophase mixture of a (deformable) skeleton and a liquid that permeates the gel. In such a poroelastic framework, the boundary conditions on the gelfluid interface are extremely tedious to derive from first principles of coarsegraining, and must be postulated. In this talk, we describe an energy dissipation formalism that suggests two sets of boundary conditions. We will compare the flow profiles predicted by these conditions with those of published models. [Preview Abstract] 

J01.00002: Viscous Transport in Eroding Porous Media Bryan Quaife, ShangHuan Chiu, Nick Moore In groundwater flow, erosion leads to a deforming porous media. Erosion creates conduits or channels of high porosity, and these are directly related to the transport properties of particulates and concentrations through the eroded geometry. This talk will use highorder simulations of both erosion and transport to analyze the flow through eroded porous media. [Preview Abstract] 

J01.00003: Cell nucleus as a microrheological probe to study the rheology of the cytoskeleton Ehssan Nazockdast, Moslem Moradi Mechanical properties of the cell are important biomarkers for probing its architectural changes caused by cellular processes and/or pathologies. Recent advancements in microfluidic and highspeed imaging technologies have enabled probing the cell cortex deformations in microchannels, while also tracking different intracellular components in highthroughputs. Most previous studies of cell mechanics using microchannels only measure the cell stiffness, and do not disentangle the rheology of different cellular components, including the cortex, the cytoplasm and the nucleus. We present a novel method that utilizes the correlation between the cortical deformations that are induced by external microfluidic flows, and the nucleus displacements, induced by those cortical deformations, to decouple the cell cortex and the cytoplasm mechanics. As a proof of concept, we consider a rigid spherical nucleus centered in a spherical cell. We obtain analytical expressions for the timedependent nucleus velocity vs the cell deformations, when the interior cytoplasm is modeled as a viscous, viscoelastic, porous and poroelastic material, and demonstrate how the nucleus velocity can be used to characterize the linear rheology of the cytoplasm over a wide range of forces and timescales/frequencies. [Preview Abstract] 

J01.00004: Growth of an isotropic cluster of activated fractures in the presence of stress anisotropy Mohammed Alhashim, Donald Koch Hydraulic stimulation of low permeability rocks via hydroshearing of preexisting fractures is widely used in the oil/gas and geothermal industries. Optimization of this process requires deep understanding of the interplay between fluid transport and permeability changes due to the growth of a cluster of activated fractures. The effects of network connectivity, pressuredriven flow of the fracturing fluid, and stress anisotropy on the cluster growth are analyzed. To delineate the effects of the network's connectivity, preexisting fractures are modeled as line segments of uniform length that are randomly oriented. To capture the effects of fluid transport, we use discrete network simulations of the stimulation process. We show that the effects of stress anisotropy, which tend to produce a quasionedimensional network, can be mitigated by fracturing in such a way that the viscous pressure drop required to drive the injected fluid becomes important over a length scale that is comparable with the preexisting fractures' correlation length. This result provides a criterion to increase the ramification of the induced hydraulically conductive flow paths by optimal design of the fracturing process. [Preview Abstract] 

J01.00005: A phasefield model for capillary bulldozing Liam Morrow, Oliver Paulin, Matthew Hennessy, Christopher MacMinn The invasion of nonwetting gas into a horizontal, liquidfilled tube or HeleShaw cell is a classical problem in fluid mechanics that has been studied extensively from a variety of perspectives. However, the addition of a sedimented granular material to the defending liquid phase can fundamentally change the mechanics of the problem by introducing friction, leading to a class of ``multiphase frictional flows'' that remain relatively poorly understood. For example, recent experiments [Dumazer et al., 2016, PRL] show that, in a capillary tube, the motion of the gasliquid interface will bulldoze the granular material, accumulating a pile of grains on the liquid side of the interface that will grow until it forms a plug and clogs the tube. Here, we present a thermodynamically consistent phasefield model for capillary bulldozing. The model involves three phases  gas, liquid, and liquidsolid mixture  and takes the form of a coupled pair of nonlinear conservation laws and a linear elliptic equation for the velocity of liquidsolid mixture. We solve our model numerically for a variety of different scenarios to develop insight into the roles of sliding friction, rearrangement, capillarity, viscosity, and plug formation during capillary bulldozing. [Preview Abstract] 

J01.00006: Catch and release of bubbles in a soft granular medium Christopher MacMinn, Jian Guan, Omid Dorostkar, Sungyon Lee A liquidsaturated packing of soft particles can behave like a complex fluid or like a porous solid, depending on the confining stress. In the fluidlike state, a gas bubble can rise through the packing due to buoyancy with a rise velocity that decreases as the solid fraction increases. In the solidlike state, gas bubbles cannot rise unless their buoyancy overcomes the failure stress of the packing or the capillary entry pressure of the pore space. Here, we use laboratory experiments, discreteelement simulations, and theoretical modelling to study these two states and the transition between them. Specifically, we study the rise velocity of bubbles as a function of bubble size and solid fraction in order to identify the solid fraction at which bubbles are immobilised. We also study the poromechanics of changing the solid fraction by compressing the packing with a fluidpermeable piston. We combine these ingredients to show that active manipulation of the solid fraction can therefore be used for the ondemand catch and release of gas bubbles. [Preview Abstract] 

J01.00007: LargeDeformation Poroelasticity with Friction Tyler Lutz, Larry Wilen, John Wettlaufer Fluid impinging on a soft porous material may cause the material to deform, which alters the behavior of the fluid flow in turn. Flows exhibiting this socalled poroelastic coupling are not generally found in isolation; frictional contacts between the solid phase and any confining boundaries strongly influence the nature of the coupling. For the tractable geometry of uniaxial flow through a cylindrical porous medium, we develop both analytic and numerical models to study the effects of wall friction on the properties of largedeformation poroelastic flows in steady state. The presence of friction leads to a measurable hysteresis in the volume flux, solid deformation, and pore pressure gradient of the flow. Using data from a mechanicallycompressed latex foam to parameterize the frictional input to our theoretical models, we present direct quantitative comparisons between model predictions and experimental measurements of volume flux, deformation, and pressure of the foam subject to flowdriven compression. [Preview Abstract] 

J01.00008: Relaxation of a fluidfilled blister on a porous substrate Danielle L. Chase, ChingYao Lai, Howard A. Stone The relaxation dynamics of a fluidfilled blister between an elastic sheet and a porous substrate are controlled by the deformation of the elastic sheet, the viscous stresses in the pores, and the capillary pressure at the fluidair interface. We present experiments where fluid is injected between a porous substrate and an elastic sheet. First, fluid invades the pores and subsequently, the elastic sheet is peeled and uplifted from the substrate resulting in a fluidfilled blister. Further injection causes both the fluid front in the pores and the fracture front of the blister to propagate radially. After injection is stopped, the fluid continues to advance into the pores as the elastic stresses in the overlying sheet drive drainage of the blister. We conduct experiments and develop a mathematical model to study the effects of blister size, permeability of the porous substrate, and bending stiffness of the elastic sheet on the relaxation dynamics. We find that the bending stiffness of the elastic sheet and the permeability of the substrate largely control the dynamics, but for thin sheets and low permeability substrates, the capillary pressure at the fluidair interface significantly affects the dynamics. [Preview Abstract] 

J01.00009: Law of mass action (LMA) with energetic variational approaches (EnVarA) with applications Chun Liu, Bob Eisenberg, Pei Liu, Yiwei Wang, Tengfei Zhang h $abstract$\backslash $pard In this talk, we will present a derivation to generalize the massaction kinetics of chemical reactions using an energetic variational approach. Our general framework involves the energy dissipation law for a chemical reaction system, which carries all the information about the dynamics. The dynamics of the system is determined through the choice of the free energy, the dissipation (the entropy production), as well as the kinematics (conservation of species). The method enables us to capture the coupling and competition of various mechanisms, including mechanical effects such as diffusion, viscoelasticity in polymeric fluids and muscle contraction, as well as the thermal effects. We will also discuss several applications under this approach, in particular, the modeling of wormlike micellar solutions. This is joint work with Bob Eisenberg, Pei Liu, Yiwei Wang, and Tengfei Zhang.$\backslash $pard/abstract$\backslash $\tex [Preview Abstract] 

J01.00010: Variational Lagrangian Scheme for the Porous Medium Equation and Phasefield models: A Discrete Energetic Variational Approach Yiwei Wang, Chun Liu In this talk, we present a systematic framework of deriving variational schemes for generalized diffusions and gradient flows, by a discrete energetic variational approach, which performs an energetic variational approach (EnVarA) at a semidiscrete level. The resulting semidiscrete equation Inherits the variational structures from the continuous energydissipation law directly. In particular, we apply such an approach to construct variational Lagrangian schemes to the porous medium type generalized diffusion and the AllenCahn type phasefield models. Numerical examples show the advantages of our schemes in capturing singularities, thin diffuse interfaces, and free boundaries.~ This is joint work with Professor Chun Liu (IIT). [Preview Abstract] 

J01.00011: Dynamics of swimmers in fluids with resistance Sarah Olson Microswimmers such as spermatozoa are able to efficiently navigate through viscous fluids that contain a sparse network of fibers or other macromolecules. We utilize the Brinkman equation to capture the fluid dynamics of sparse and stationary obstacles that are represented via a single resistance parameter. The method of regularized Brinkmanlets is utilized to solve for the fluid flow and motion of the swimmer in 2dimensions when assuming the flagellum (tail) propagates a curvature wave. For a single swimmer, we determine that increased swimming speed occurs for smaller cell body radius and smaller fluid resistance. Progression of swimmers exhibits complex dynamics when considering hydrodynamic interactions; attraction of two swimmers is a robust phenomenon for smaller beat amplitude of the tail and smaller fluid resistance. Wall attraction is also observed, with a longer time scale of wall attraction with larger resistance parameter. [Preview Abstract] 

J01.00012: A poroelastoviscoplastic model of the dewatering of a twophase suspension Tom S. Eaves, Daniel T. Paterson, Duncan R. Hewitt, Neil J. Balmforth, D. Mark Martinez A poroelastoviscoplastic model for the consolidation of a twophase suspension is presented, motivated by the compaction and dewatering of woodfibre pulp. For that material, traditional twophase models of particulate porous media based upon plastic yielding of the particle network prove insufficient to capture the observed dynamics. The incorporation of viscous effects stemming from the compaction of the woodfibrenetwork assists the model in reproducing experimental dewatering tests at moderate rates of compaction. However, during more rapid dewatering there is clear emergence of an elastic behaviour in the woodfibre network. We present a poroelastoviscoplastic extension of the model, its calibration for woodpulp using quasistatic cycles of loading and unloading, and demonstrate its improved representation of the rapid dewatering experiments. [Preview Abstract] 

J01.00013: Fluidstructure interactions in a softwalled HeleShaw cell Callum Cuttle, Satyajit Pramanik, Jian Hui Guan, Christopher MacMinn The interaction of viscous and interfacial flows with soft materials has recently attracted substantial interest from a variety of different perspectives. Here, we study these interactions in the context of a model problem: Flow in a deformable HeleShaw cell, where one wall is rigid and the other is soft. Combining experiments with mathematical modelling, we consider the coupling of flow and deformation as viscous fluid is injected into an initially empty cell. We then discuss the implications of these results for hydrodynamic instabilities such as viscous fingering. [Preview Abstract] 

J01.00014: Viscous backflows from elastic reservoirs Zhong Zheng, Emilie Dressaire, Alban Sauret The dynamics of fluid removal from an elastic reservoir is related to the practice of waste water migration following hydraulic fracturing, surface morphology control during geotechnical engineering and skin fluid collection for medical use. We report a series of reducedorder modelling studies and scaling results for the viscous backflow process from elastic reservoirs, including that from a hydraulic fracture and from beneath a stretched membrane or a bending plate. The backflow is generated once the exit of the elastic cavities is exposed to the atmosphere, or a fluid bath with a lower pressure. A couple of firstorder ODEs are derived to describe the time evolution of the length and height of the fracture/cavity. The rate of fluid removal can also be estimated accordingly. The flow dynamics is found to depend on three nonlinear competing terms that correspond to the process of fluid propagation within a fracture or an elastic cavity, the viscous flow in the exiting channel, and the induced flow from the low pressure at the exit. [Preview Abstract] 

J01.00015: Deformationdriven solute transport in soft porous media Matilde Fiori, Satyajit Pramanik, Christopher MacMinn Solute transport plays an important role in many soft porous materials, including the movement of contaminants in soils and the movement of nutrients and waste in living tissues and tissueengineering scaffolds. These systems are also often exposed to large, periodic loading and deformation, which drives nontrivial fluid motion and changes in pore structure. Here, we study the strong coupling between fluid flow and mechanical stimulation during periodic deformations using a 1D continuum model based on largedeformation poroelasticity. We show that these reversible deformations lead to nonreversible spreading and mixing, even in a homogeneous medium. We analyse the three primary mechanisms of solute transport (advection, molecular diffusion, and mechanical dispersion) and study their separate impacts on the solute distribution. We also identify the key dimensionless parameters that govern deformationdriven transport, and we study their qualitative and quantitative impacts on solute spreading and mixing. [Preview Abstract] 

J01.00016: Gasliquid phase separation in a soft porous medium Oliver Paulin, Liam Morrow, Matthew Hennessy, Christopher MacMinn Various biological and chemical processes can lead to the nucleation and growth of gas bubbles within the pore space of an otherwise liquidsaturated granular medium, such as in lake beds and waste ponds. The gas is typically nonwetting and, as the bubbles approach the pore size, it is energetically costly for them to invade narrow pore throats. If the solid skeleton is sufficiently soft, it is favourable for the bubbles to displace the solid grains and form macroscopic cavities. Here, we consider this process through the lens of phase separation, where thermomechanics govern the separation of a gas phase from a gasliquidsolid mixture. We construct a phasefield model informed by largedeformation poromechanics, in which two immiscible fluids interact with a poroelastic solid skeleton. Our model captures the competing effects of elasticity and gasliquidsolid interactions. As a model problem, we consider an initial distribution of gas in the pore space that separates into multiple gas cavities, which then coarsen over time as the smaller cavities collapse and the larger cavities expand. We identify the key parameters that control phase separation, the conditions that favour the formation of gas cavities, and the characteristic size of the resulting gas cavities. [Preview Abstract] 

J01.00017: Deformations of the cell cytoplasm through the lens of poroviscoelastic materials Calina Copos, Robert Guy The cell cytoplasm is the largest part of the cell by volume and its rheological properties dictate the material response of the whole cell. In particular, the cytoskeleton behaves like a porous elastic solid on timescales of seconds, but a viscous fluid on timescales longer than minutes. On intermediate timescales, the actin network behaves like an elastic material that exhibits stress relaxation due to the reorganization of the cytoskeleton. We consider a poroelastic immersed boundary method in which a fluid permeates a porous, elastic structure of negligible volume fraction. Then, we extend this method to describe a poroviscoelastic material in a computationally efficient way, and thus include stress relaxation of the material. Lastly, we demonstrate how this computational method can be used, together with fast cytometry measurements, to infer material properties of the cell. [Preview Abstract] 

J01.00018: Unraveling cytoplasmic streaming using a coarsegrained model of microtubule hydrodynamics David Stein, Gabriele de Canio, Eric Lauga, Michael Shelley, Raymond Goldstein During the development of the fruit fly oocyte, flows with shortranged correlations transition to a dramatic cellspanning vortex, accompanied by coherent deformations in the microtubule cytoskeleton. Using a coarsegrained model for the hydrodynamics of ordered fibers, we show that sufficiently dense microtubule arrays, forced only by molecular motors transporting cargo, undergo a ``swirling transition'' that is fundamentally different than the buckling transition which leads to the flapping motion of isolated filaments. Our model produces streaming velocities consistent with \emph{in vivo} measurements, and allows us to place bounds on the number density of kinesin1 motors transporting cargo within the microtubule array. [Preview Abstract] 
Follow Us 
Engage
Become an APS Member 
My APS
Renew Membership 
Information for 
About APSThe American Physical Society (APS) is a nonprofit membership organization working to advance the knowledge of physics. 
© 2023 American Physical Society
 All rights reserved  Terms of Use
 Contact Us
Headquarters
1 Physics Ellipse, College Park, MD 207403844
(301) 2093200
Editorial Office
1 Research Road, Ridge, NY 119612701
(631) 5914000
Office of Public Affairs
529 14th St NW, Suite 1050, Washington, D.C. 200452001
(202) 6628700