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On the boundary layer structure near a highly permeable porous interface

Published online by Cambridge University Press:  31 May 2016

Mohit P. Dalwadi*
Affiliation:
Synthetic Biology Research Centre, University of Nottingham, University Park, Nottingham NG7 2RD, UK Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
S. Jonathan Chapman
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
Sarah L. Waters
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
James M. Oliver
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
*
†Email address for correspondence: mohit.dalwadi@nottingham.ac.uk

Abstract

The method of matched asymptotic expansions is used to study the canonical problem of steady laminar flow through a narrow two-dimensional channel blocked by a tight-fitting finite-length highly permeable porous obstacle. We investigate the behaviour of the local flow close to the interface between the single-phase and porous regions (governed by the incompressible Navier–Stokes and Darcy flow equations, respectively). We solve for the flow in these inner regions in the limits of low and high Reynolds number, facilitating an understanding of the nature of the transition from Poiseuille to plug to Poiseuille flow in each of these limits. Significant analytical progress is made in the high Reynolds number limit, and we explore in detail the rich boundary layer structure that occurs. We derive general results for the interfacial stress and for the conditions that couple the flow in the outer regions away from the interface. We consider the three-dimensional generalization to unsteady laminar flow through and around a tight-fitting highly permeable cylindrical porous obstacle within a Hele-Shaw cell. For the high Reynolds number limit, we give the coupling conditions and interfacial stress in terms of the outer flow variables, allowing information from a nonlinear three-dimensional problem to be obtained by solving a linear two-dimensional problem. Finally, we illustrate the utility of our analysis by considering the specific example of time-dependent forced far-field flow in a Hele-Shaw cell containing a porous cylinder with a circular cross-section. We determine the internal stress within the porous obstacle, which is key for tissue engineering applications, and the interfacial stress on the boundary of the porous obstacle, which has applications to biofilm erosion. In the high Reynolds number limit, we demonstrate that the fluid inertia can result in the cylinder experiencing a time-independent net force, even when the far-field forcing is periodic with zero mean.

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Papers
Copyright
© 2016 Cambridge University Press 
Figure 0

Figure 1. Schematic of a high aspect ratio vessel bioreactor, containing a porous scaffold (darker region). The bioreactor has a similar shape to a Petri dish turned on its side. (a) Face view. (b) Side view showing the gaps between the scaffold and the bioreactor. Cells are seeded within the scaffold, and the entire bioreactor is filled with a nutrient-rich fluid and rotated around its axis, causing the scaffold to move.

Figure 1

Figure 2. The model geometry for flow within (a) a channel and (b) a Hele-Shaw cell. The light region is the exterior fluid and the dark region is the porous obstacle.

Figure 2

Table 1. Typical dimensional parameter values and the corresponding values of the dimensionless parameters. The absolute upper bound of $1/12\approx 8.3\times 10^{-2}$ for $K$ can be obtained by considering unobstructed Poiseuille flow through a channel. We use the density and viscosity values of water at room temperature for ${\it\rho}$ and ${\it\mu}$, respectively.

Figure 3

Figure 3. The boundary layer structure for $Re=O(1)$. The light region is the exterior fluid and the dark region is the porous obstacle. (a) The different asymptotic regions are indicated and labelled in Roman numerals. (b) A schematic representation of the flow.

Figure 4

Figure 4. The inner inflow problem for $Re=O(1)$. The flow is from left to right.

Figure 5

Figure 5. The inner outflow problem for $Re=O(1)$. The flow is from left to right.

Figure 6

Figure 6. The $O({\it\epsilon})$ normal and shear stresses acting on the interface $X=0$, for $K=0.01$. (a) $\overline{p}_{1}-2\overline{u}_{0X}$, (b) $-(\overline{u}_{0z}+\overline{w}_{0X})$.

Figure 7

Table 2. Asymptotic expansions within boundary layers in the large Reynolds number limit.

Figure 8

Figure 7. Schematic diagram of the inner regions IIa–c within the inflow boundary region II. The light region is the exterior fluid and the dark region is the porous obstacle. The size of the boundary layers has been exaggerated for illustrative purposes.

Figure 9

Figure 8. The streamlines for inflow near the interface. (a) The streamlines for the scaled first-correction velocity $K\overline{\boldsymbol{u}}_{01}$, which is independent of $K$. The fluid moves from the centre of the channel to the channel walls. (b) The streamlines for the full velocity up to first correction $\overline{\boldsymbol{u}}_{00}+{\it\delta}\overline{\boldsymbol{u}}_{01}$ (with a large value of ${\it\delta}/K=1$ taken to emphasise the effect of the correction). The fluid moves from left to right.

Figure 10

Figure 9. The function $(\int _{0}^{1}\overline{p}_{11}\,\text{d}z+12X^{-})K$ for varying $X^{-}$ in region II, which allows us to determine the outer pressure drop for inflow.

Figure 11

Figure 10. The interfacial stress predicted by the inner flows (from (2.60)) at $O({\it\epsilon})$. (a) The normal stress (we plot $K\overline{p}_{11}(0,z)$) and (b) the shear stress (we plot $6z(1-z)K\overline{w}_{01}(0,z)$). As both the normal and shear stress scale with $1/K$ at this order, both plotted terms are independent of $K$.

Figure 12

Figure 11. Schematic diagram of the inner regions for outflow – VIa, VIb, and VIc. The size of the boundary region VIb has been exaggerated for illustrative purposes, is of height $O({\it\epsilon}{\it\delta}^{1/2})$, and grows proportional to the square root of the distance from the porous obstacle. Region VIc lies within region VIb and has height and length $O({\it\epsilon}{\it\delta})$.

Figure 13

Figure 12. Calculating the outflow pressure drop along the channel by plotting $\widetilde{p}_{10}+12\widetilde{X}$. See text for further details.

Figure 14

Figure 13. Plan view of streamlines through and around a general porous obstacle model with a uniform far-field flow. The $z$-axis points out of the page. The Hele-Shaw cell has a depth of length $h$ in the $z$-direction (not shown). We show the unit vectors $\boldsymbol{e}_{x}$ and $\boldsymbol{e}_{y}$ in the $x$- and $y$-directions respectively (for the Cartesian coordinate system), and the curvilinear $(n,s)$-coordinate system for a given point on the boundary of the obstacle.

Figure 15

Figure 14. The spatial variation of the Darcy velocity averaged over one temporal oscillation of the far field, given by the $O({\it\epsilon}\overline{Re}K)$ term in (4.12). This term is proportional to the shear stress experienced within the porous obstacle. We use far-field forcing functions of (a) $G(t)=\cos (t)/\sqrt{{\rm\pi}}$, (b) $G(t)=(\cos t-\cos 2t)/\sqrt{2{\rm\pi}}$. The functions are chosen such that $\int _{0}^{2{\rm\pi}}G^{2}(t)\,\text{d}t=1$. In both figures, we take $K=0.01$, we use contour spacings of $0.05$ and, as there are logarithmic singularities at $(x,y)=(0,\pm 1)$, we do not plot contours of values larger than $0.3$. We see that the symmetry exhibited in (a) is not present in (b). This is due to the effect of fluid inertia.

Figure 16

Figure 15. A contour plot of the function $z(1-z)|\sin 2{\it\theta}|^{1/2}$, showing the shape of erosion in the region $({\it\theta},z)\in [0,{\rm\pi}/2]\times [0,1]$. This shape is repeated in each quadrant of the circular cylinder interface, but the magnitude will vary, as discussed in the text. We use contour spacings of 0.05.