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Internal hydraulic jump in plane Poiseuille two-layer flow: theoretical, numerical and experimental study

Published online by Cambridge University Press:  16 February 2021

Mrinmoy Dhar
Affiliation:
Department of Mechanical Engineering, Indian Institute of Technology, Kharagpur 721302, India
Subhabrata Ray
Affiliation:
Department of Chemical Engineering, Indian Institute of Technology, Kharagpur 721302, India
Gargi Das*
Affiliation:
Department of Chemical Engineering, Indian Institute of Technology, Kharagpur 721302, India
Prasanta Kumar Das
Affiliation:
Department of Mechanical Engineering, Indian Institute of Technology, Kharagpur 721302, India
*
† Email address for correspondence: gargi@che.iitkgp.ernet.in

Abstract

This paper discusses a hitherto unexplored flow phenomenon, namely the internal hydraulic jump in thin films during co-current and counter-current two-layer flow between parallel plates. The problem corresponds to a special case of plane Poiseuille flow where the velocity profile changes continuously in the streamwise distance. Since an exact solution of Navier–Stokes equations is not possible, we reformulate the approximate shallow water theory, conventionally adopted to analyse viscous jumps in single-layer laminar flow. The standalone theory has been extensively validated with experimental data for coflow of the two phases and numerical simulations for both co- and counter-current flow. In the limit of zero viscosity ratio, the theoretical results reduce to the expression proposed by Dhar et al. (J. Fluid Mech., vol. 884, no. A11, 2020, pp. 1–26) for single-layer viscous jumps. For a holistic understanding, numerical simulations are used to unravel the physics at the jump, where the analysis displays singularity. The theory in conjunction with simulation reveals recirculation zones even in co-current laminar flow and delineates wavy, smooth and submerged jumps, displayed as a phase diagram. We thus demonstrate the efficacy of shallow water theory which, despite the approximations involved, can be used as a reliable tool for a priori prediction of viscous jumps in two-layer flow with much less effort and resources compared to numerical simulations. Use of an approximate analysis to obtain multifaceted results for a complex flow phenomenon has rarely been explored previously. This paper is also the first study reporting experiments on viscous jumps for two-layer flow in a shallow water analogue.

Information

Type
JFM Papers
Copyright
© The Author(s), 2021. Published by Cambridge University Press
Figure 0

Figure 1.Problem domain (a) and the experimental analogue (b) of viscous shear induced hydraulic jump in air–water stratified flow. The liquid film of depth ${h_{l,in}}$ is introduced in the conduit of height H. At streamwise position (x), the film of thickness $h(x)$ flows beneath a gas layer of thickness $[H - h(x)]$. Here, $u(x,z)$ and $w(x,z)$ are the respective streamwise (x) and vertical (z) velocity components for each fluid (of density $\rho$, dynamic viscosity $\mu$ and kinematic viscosity $\nu ( = \mu /\rho )$) flowing at volumetric flow rate q per unit conduit width; P(x) is the pressure at distance x from the entry and g is acceleration due to gravity. Subscripts l and g associated with each notation refer to the liquid and gas phases, respectively, and subscript i denotes the interface. The hydraulic jump confined within control surfaces 1 and 2 is at a distance x1 from the entry.

Figure 1

Table 1.Values of ${({h^\ast }/{L^\ast })^2}$ for the two phases under different flow conditions.

Figure 2

Figure 2.Typical plot of (a) f(h) versus h and (b) ES versus h indicating singularity at h ≈ 1 for qr = 0 (only liquid flow).

Figure 3

Figure 3.Typical plot of (a) f(h) versus h and (b) ES versus h indicating singularity at h ≈ 1 for qr = 25 (co-current flow).

Figure 4

Figure 4.Typical plot of (a) f(h) versus h and (b) ES versus h indicating singularity at h ≈ 1 for qr = −25 (counter-current flow).

Figure 5

Figure 5.Co-current flow: observed (data points) and theoretical (solid curves) interface profile and jump location for hl,in = 0.5 mm and H = 5 mm. In each figure, vertical dotted lines depict the theoretically predicted jump location.

Figure 6

Figure 6.Co-current and counter-current interface profiles from SWT (solid curves) and CFD simulation (dashed-dotted curves) for hl,in = 0.25 mm and H = 3 mm. The vertical dotted lines depict the SWT predicted jump location (−ve flow rate is for counter-current flow).

Figure 7

Figure 7.Validation of theoretical and numerical predictions against experimental data for no air flow. The discrete points represent experimental data and dashed-dotted and solid curves correspond to numerical simulation and analytical prediction respectively for ${q_l} = 8.75 \times {10^{ - 5}}\;{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$ and Lc = 90 mm. The dotted vertical line indicates the analytically predicted jump location under the specified flow condition.

Figure 8

Figure 8.Power law dependence of jump location on ${q_l}$ with ${q_g}$ as parameter (−ve flow rates are for counter-current flow).

Figure 9

Figure 9.Influence of ${q_g}$ and ${q_l}$ on (a) jump location and (b) strength (−ve flow rates are for counter-current flow).

Figure 10

Figure 10.Streamwise variation of (a) interface height and (b) Froude number for co-current, counter-current and no flow condition of gas. The W and S marked in (a) denote wavy and smooth jumps, respectively. The inset in figure (b) shows that there is a transition from Fr > 1 to Fr < 1 (i.e. jump) even at high values of co-current gas flow rate.

Figure 11

Figure 11.Typical streamline patterns, interface profiles and streamwise evolution of velocity profiles at ${q_l} = 1.25\;\textrm{c}{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$ and ${\pm} {q_g} = 2.75\;\textrm{c}{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$ for (a) parallel and (b) opposite flow. Suffixes 1, 2 and 3 display streamwise velocity distribution upstream of jump, at jump and downstream of jump. Markers (hollow circles) in each figure denote interface position. Scaled ordinates non-dimensionalised with inlet liquid velocity ul,in and height hl,in to facilitate a comparative study.

Figure 12

Figure 12.Streamline patterns and interface profiles at ${q_l} = 1.25\;\textrm{c}{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$ and ${q_g} = (a)\;2.75$ and (b) 5.5 cm2 s−1.

Figure 13

Figure 13.Streamwise velocity profiles for (a) co-current and (b) counter-current gas–liquid flow for the gas flow rates used in figure 11 (${q_l} = 1.25\;\textrm{c}{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$ and ${\pm} {q_g} = 2.75\;\textrm{c}{\textrm{m}^2}\;{\textrm{s}^{ - 1}}$). Suffixes 1 and 2 correspond to upstream of jump at x/hl,in = 40 and downstream of jump at x/hl,in = 300 respectively. The markers (hollow circles) in the respective velocity profiles denote the interface position.

Figure 14

Figure 14.Phase diagram for jump type as a function of gas and liquid flow rates.