22-Mec-B6 Advanced Fluid Mechanics · December 2014
Question 3 of 5: Gravity-driven laminar flow in a vertical annulus with one shear-free wall
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
Paper format. National Exams, December 2014 —
07-Mec-B6 Advanced Fluid Mechanics. Three hours, OPEN BOOK, any non-communicating
calculator permitted. Five questions are printed; candidates answer any four and all
questions are equally weighted, so each question carries 25 of the 100 marks. A four-page
aid sheet (compressible flow, boundary-layer integral relations, the Navier–Stokes
equations in Cartesian and cylindrical-polar form, and potential-flow building blocks) is
bound into the paper; every relation used below is taken from it. All five questions
are solved here.
Reference texts. Solutions follow the conventions of the texts the
EGBC syllabus recommends for this subject:
F. M. White, Fluid Mechanics, 8th ed. — potential flow and images (§8.3–8.5),
turbulent flat-plate layers (§7.4), turbomachinery similarity (§11.3–11.5).
F. M. White, Viscous Fluid Flow, 3rd ed. — exact solutions of the
Navier–Stokes equations in annular geometry (§3.2–3.3).
J. D. Anderson, Modern Compressible Flow, 3rd ed. — quasi-one-dimensional
nozzle flow and normal shocks (Ch. 3 and Ch. 5).
P. K. Kundu, I. M. Cohen & D. R. Dowling, Fluid Mechanics, 6th ed. —
complex potential, Blasius theorem and image forces (Ch. 6).
R. W. Fox et al., Introduction to Fluid Mechanics, 10th ed. —
entrance-region and duct-flow treatment (Ch. 8).
SI units throughout; air and water properties are those printed in the question, and
Canadian practice (SI, absolute pressures stated explicitly) is followed.
Question 3: Gravity-driven laminar flow in a vertical annulus with one shear-free wall (25 marks)
Find. ur(r), uz(r), and the magnitude and direction of the
force per unit length that the water exerts on the inner rod.
Figure 3.1 — Left: the annular gap, driven by gravity alone because both ends are open to atmosphere. Right: the axial velocity profile, a parabola plus a logarithm; the zero-shear (Teflon) wall is the free-surface-like edge where the profile is flat.
Approach. Continuity plus the non-porous walls kills the radial component
outright; the z-momentum equation from the cylindrical-polar aid sheet then collapses to an
ordinary differential equation in r driven by gravity alone, whose two constants are set by the
zero-shear condition at the Teflon wall and the no-slip condition at the rod. The rod force is
the wall shear times its circumference, and a global force balance on the annulus checks it.
Part (a) — eliminate the radial velocity from continuity. For a steady,
axisymmetric, incompressible flow the aid-sheet continuity equation reduces to
$$\frac{1}{r}\frac{\partial}{\partial r}\left(r\,u_r\right)+\frac{\partial u_z}{\partial z}=0$$
Fully developed flow in a long pipe means $ \partial u_z/\partial z = 0 $, so
$ \partial(r u_r)/\partial r = 0 $ and therefore $ r\,u_r = C $, a constant across the gap.
Applying the non-porous condition at either wall — $ u_r(b)=0 $ — forces C = 0, and
since $ r \geq b > 0 $ everywhere in the annulus,
$$\boxed{\;u_r(r)=0\quad\text{throughout the gap}\;}$$
The streamlines are exactly parallel to the axis; nothing crosses between radii.
Part (b) — reduce the axial momentum equation. With
$ u_r = u_\theta = 0 $, $ \partial/\partial\theta = 0 $, $ \partial u_z/\partial z = 0 $ and
steady flow, every convective term in the aid-sheet z-momentum equation vanishes and it leaves
a balance between pressure, gravity and viscous diffusion:
$$0=-\frac{dP}{dz}+\rho g+\frac{\mu}{r}\frac{d}{dr}\left(r\frac{du_z}{dr}\right)$$
The inlet and outlet are both open to the same atmosphere, so the static pressure does not
change along the pipe: $ dP/dz = 0 $. Gravity is therefore unbalanced and is the only
thing driving the flow — the pipe is running as a gravity drain, not as a pressure line:
$$\frac{1}{r}\frac{d}{dr}\left(r\frac{du_z}{dr}\right)=-\frac{\rho g}{\mu}$$
Integrate twice. Multiplying by r and integrating,
$ r\,du_z/dr = -\rho g r^{2}/(2\mu)+C_1 $, and integrating again
$$u_z(r)=-\frac{\rho g\,r^{2}}{4\mu}+C_1\ln r+C_2$$
The logarithm is the signature of the annular geometry; a plain circular pipe would reject it
because the velocity must stay finite on the axis, but here the axis is occupied by the rod.
Apply the Teflon condition at r = R. A non-wetting wall carries no shear, so
$ du_z/dr = 0 $ there:
$$-\frac{\rho g R}{2\mu}+\frac{C_1}{R}=0\quad\Longrightarrow\quad C_1=\frac{\rho g R^{2}}{2\mu}$$
This is the mathematical statement that the outer wall behaves like a free surface: the profile
arrives at it flat.
Apply no slip at the rod, r = b = R/4. Setting $ u_z(b)=0 $,
$ C_2=\rho g b^{2}/(4\mu)-C_1\ln b $, and substituting both constants gives the profile
$$\boxed{\;u_z(r)=\frac{\rho g}{4\mu}\left(b^{2}-r^{2}\right)
+\frac{\rho g R^{2}}{2\mu}\,\ln\!\frac{r}{b},\qquad b=\frac{R}{4}\;}$$
which is a Poiseuille parabola bent upward by a logarithm. It is positive everywhere in
$ b < r \leq R $ (the parabolic term is negative there, but the logarithm dominates), and it
rises monotonically from zero at the rod to its maximum at the shear-free outer wall:
$$u_{z,\max}=u_z(R)=\frac{\rho g R^{2}}{\mu}\left[\frac{1}{4}\left(\frac{1}{16}-1\right)
+\frac{1}{2}\ln 4\right]=0.4588\,\frac{\rho g R^{2}}{\mu}$$
Part (c) — evaluate the shear stress the water applies to the rod.
Differentiating the profile,
$$\begin{aligned}
\frac{du_z}{dr}&=-\frac{\rho g r}{2\mu}+\frac{\rho g R^{2}}{2\mu\,r}\
\frac{du_z}{dr}\bigg|_{r=b}&=-\frac{\rho g R}{8\mu}+\frac{2\rho g R}{\mu}
=\frac{15}{8}\frac{\rho g R}{\mu}
\end{aligned}$$
The traction the fluid exerts on the rod surface is
$ \tau_{rz}(b)=\mu\,du_z/dr|_b=\tfrac{15}{8}\rho g R $, acting in the +z direction, i.e.
with the flow.
Multiply by the wetted perimeter to get force per unit length. The rod
presents a circumference $ 2\pi b=2\pi R/4 $, so
$$F' = \tau_{rz}(b)\,(2\pi b)=\frac{15}{8}\rho g R\cdot\frac{\pi R}{2}
=\frac{15}{16}\pi\rho g R^{2}$$
$$\boxed{\;F'=\frac{15}{16}\pi\rho g R^{2}\approx 2.945\,\rho g R^{2}\ \text{N per metre,
directed downward (with the flow)}\;}$$
Audit the answer with a global force balance. Take the whole annular column
of fluid, per unit length, as a free body. Its weight is
$ \rho g\,\pi(R^{2}-b^{2})=\rho g\pi R^{2}(1-\tfrac{1}{16})=\tfrac{15}{16}\pi\rho g R^{2} $;
the pressure forces on the two ends cancel because the pressures are equal; the Teflon wall
transmits no shear at all. The rod is therefore the only thing holding the water up,
and it must carry the entire weight — which is exactly the number obtained in step 7.
Any slip in the algebra would break this identity immediately, so it is worth writing down.
Put representative numbers on the result. Water at laboratory scale would be
turbulent here, so take a light lubricating oil,
$ \rho = 900 $ kg/m³, $ \mu = 0.50 $ Pa·s, in a pipe of $ R = 10 $ mm with a 2.5 mm
rod. Then $ u_{z,\max}=0.4588(900)(9.81)(0.010)^{2}/0.50=0.810 $ m/s, the mean velocity is
0.657 m/s, the hydraulic diameter is $ 2(R-b)=15 $ mm and
$ Re = \rho \bar{u} D_h/\mu = 17.7 $ — comfortably laminar, as assumed. The rod then carries
$ F' = \tfrac{15}{16}\pi(900)(9.81)(0.010)^{2}=2.60 $ N per metre, identical to the weight of the
0.265 kg of oil each metre of annulus contains.
Check: the direction of z and the laminar assumption.
z is taken positive downward, along the flow and along gravity, matching Fig. Q3; with z upward
every sign flips but the magnitude of the rod force is unchanged. The laminar premise is the
question's, and it is restrictive: for water (μ = 1.0 × 10−3 Pa·s)
the same geometry at R = 10 mm would give a mean velocity of order 300 m/s and
Re ≈ 5 × 106, so a real water column of this size would be fully turbulent
and the profile above would not apply. The analysis is valid for viscous liquids, for very small
radii, or for the low-gravity/microchannel limit — state that assumption rather than
presenting the parabola-plus-logarithm as a general answer.
Part
Result
(a) Radial velocity
ur(r) ≡ 0 — forced by continuity plus non-porous walls