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23-Chem-B1 Transport Phenomena · May 2014

Question 1 of 6: A1 — Laminar flow of water between parallel plates

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format: National Exams, May 2014 — 04-CHEM-B1 Transport Phenomena; 3 hours, open book. Six problems in three sections (A Fluid Mechanics, B Heat Transfer, C Mass Transfer); candidates attempt one from each section plus a fourth from any section (four of six marked, 25 marks each). The worked solutions below cover all six problems. A summary of the conservation equations (continuity, Navier–Stokes, energy, species) is provided as Appendix A in the paper and is used throughout.

Reference texts: R. S. Brodkey & H. C. Hershey, Transport Phenomena — A Unified Approach (McGraw-Hill) — the paper’s own reference and source of the appended conservation-equation tables; R. B. Bird, W. E. Stewart & E. N. Lightfoot, Transport Phenomena (2nd ed., Wiley) — equations of change and the differential momentum / energy / species balances; J. R. Welty, C. E. Wicks, R. E. Wilson & G. L. Rorrer, Fundamentals of Momentum, Heat and Mass Transfer (Wiley) — differential balances and diffusion with reaction; F. P. Incropera & D. P. DeWitt, Fundamentals of Heat and Mass Transfer (Wiley) — conduction with generation, composite walls, combined convection–radiation.

Question 1: A1 — Laminar flow of water between parallel plates

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. Fully-developed, steady laminar flow of water (constant $\rho$, $\mu$) between infinite parallel plates a distance $2\delta$ apart; $y$ measured from the mid-plane, so the walls are at $y=\pm\delta$. Flow is driven along $x$ by a constant pressure gradient $dP/dx$. For part (b), inlet temperature $T_{in}$, wall temperature $T_s$.

Find. (a) the velocity profile $u(y)$; (b) the governing PDE for $T$ together with its boundary conditions.

upper plate: y = +δ, wall temperature Ts lower plate: y = −δ, wall temperature Ts y=+δ y=−δ y=0 x umax parabolic profile u(y)
Fig. A1: Fully-developed laminar flow between parallel plates spaced $2\delta$ apart. The pressure gradient drives a symmetric parabolic velocity profile, zero at each wall and maximum on the mid-plane $y=0$.

Part (a) — velocity profile

  1. Reduce the Navier–Stokes equation. For steady, fully-developed unidirectional flow, $\vec{u}=u(y)\,\hat{\imath}$ with $u_y=u_z=0$; continuity then gives $\partial u/\partial x=0$ automatically. The $x$-momentum equation (Table A.2) loses its transient, inertial and $z$-terms, leaving a balance of pressure and viscous stress: $$0=-\frac{1}{\rho}\frac{\partial P}{\partial x}+\nu\frac{\partial^2 u}{\partial y^2}\;\Longrightarrow\;\mu\frac{d^2u}{dy^2}=\frac{dP}{dx}.$$
  2. Integrate twice. With $dP/dx$ constant across the gap, $\dfrac{du}{dy}=\dfrac{1}{\mu}\dfrac{dP}{dx}\,y+C_1$ and $u=\dfrac{1}{2\mu}\dfrac{dP}{dx}\,y^2+C_1 y+C_2.$
  3. Apply symmetry and no-slip. Symmetry about the mid-plane requires $du/dy=0$ at $y=0$, so $C_1=0$. No-slip at either wall, $u(\pm\delta)=0$, gives $C_2=-\dfrac{1}{2\mu}\dfrac{dP}{dx}\,\delta^2.$
  4. Assemble the profile. Substituting the constants, $$u(y)=-\frac{1}{2\mu}\frac{dP}{dx}\left(\delta^2-y^2\right)=-\frac{\delta^2}{2\mu}\frac{dP}{dx}\left(1-\left(\frac{y}{\delta}\right)^2\right).$$ The centre-line value $u(0)=-\dfrac{\delta^2}{2\mu}\dfrac{dP}{dx}$ is by definition $u_{max}$ (positive, since a driving flow has $dP/dx<0$), giving the required result. $\boxed{\,u=u_{max}\left(1-\left(\dfrac{y}{\delta}\right)^2\right)\,}$

Part (b) — temperature-profile equation

The flow is now thermally developing: the fluid enters at $T_{in}$ and is heated (or cooled) toward the wall value $T_s$ as it moves downstream, so $T=T(x,y)$. Applying the energy equation for an incompressible medium (Table A.3) in rectangular coordinates and discarding the terms that vanish gives the governing PDE.

  1. Reduce the energy equation. Steady state removes $\partial T/\partial t$; with $u_y=u_z=0$ only the axial convection term $u_x\,\partial T/\partial x$ survives on the left. On the right, axial conduction $\partial^2T/\partial x^2$ is negligible next to transverse conduction $\partial^2T/\partial y^2$ (large Péclet number), and there is no volumetric generation. With constant $k$: $$\rho\hat{C}_P\,u(y)\,\frac{\partial T}{\partial x}=k\,\frac{\partial^2 T}{\partial y^2}.$$
  2. Insert the known velocity profile. Substituting $u(y)=u_{max}\!\left(1-(y/\delta)^2\right)$ from part (a) gives the differential equation describing the temperature field: $$\boxed{\;\rho\hat{C}_P\,u_{max}\!\left(1-\left(\frac{y}{\delta}\right)^2\right)\frac{\partial T}{\partial x}=k\,\frac{\partial^2 T}{\partial y^2}\;}$$ This is the classic Graetz (thermal-entry) problem; as instructed we stop here without solving.
  3. Boundary and inlet conditions. Three conditions close the second-order-in-$y$, first-order-in-$x$ equation:
    • Inlet: $T(0,y)=T_{in}$ for all $y$.
    • Both walls isothermal: $T(x,+\delta)=T(x,-\delta)=T_s$.
    • Equivalently, by symmetry the centre-line has zero transverse gradient: $\left.\dfrac{\partial T}{\partial y}\right|_{y=0}=0$ (may replace one wall condition).
Check — modelling assumptions

Viscous dissipation is neglected (water at ordinary shear rates: the Brinkman number is very small), axial conduction is dropped relative to axial convection (high Péclet number), and properties are taken constant. If dissipation were retained, a source term $+\mu(du/dy)^2$ would be added to the right-hand side.

PartResult
(a) Velocity profile$u=u_{max}\!\left(1-(y/\delta)^2\right)$,  $u_{max}=-\dfrac{\delta^2}{2\mu}\dfrac{dP}{dx}$
(b) Temperature PDE$\rho\hat{C}_P u_{max}\!\left(1-(y/\delta)^2\right)\dfrac{\partial T}{\partial x}=k\dfrac{\partial^2 T}{\partial y^2}$
(b) Conditions$T(0,y)=T_{in}$; $T(x,\pm\delta)=T_s$; $\partial T/\partial y|_{y=0}=0$
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