UNIT 3: FLUID MECHANICS – II (Exam-Focused Short Notes)
1. Introduction and Historical Development
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Fluid Mechanics: Study of fluids (liquids & gases) at rest (fluid statics) and in motion (fluid dynamics), and their interaction with solids.
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Key Milestones:
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Archimedes (250 BC): Buoyancy principle.
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Newton (1687): Law of viscosity, fluid resistance.
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Bernoulli (1738): Hydrodynamica, energy principle.
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Euler (1755): Equations of motion for inviscid flow.
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Reynolds (1883): Experiment on laminar/turbulent transition, Reynolds number.
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Prandtl (1904): Boundary layer theory.
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Stokes (1851): Flow past spheres, Stokes' law.
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Exam Focus: Historical questions often ask for contributors and their key laws. Link names to equations (e.g., Bernoulli → energy equation, Reynolds → Re).
2. Fluid Properties and Basic Concepts
Definition of Fluid: A substance that deforms continuously under shear stress, no matter how small.
| Property | Symbol | Unit | Notes |
|---|---|---|---|
| Density | $\rho$ | kg/m³ | Mass per unit volume |
| Specific Weight | $\gamma$ | N/m³ | $$\displaystyle \gamma = \rho g $$ |
| Dynamic Viscosity | $\mu$ | Pa·s (N·s/m²) | Resistance to shear |
| Kinematic Viscosity | $\nu$ | m²/s | $$\displaystyle \nu = \mu / \rho $$ |
Newton’s Law of Viscosity:
$$ \tau = \mu \frac{du}{dy} $$
Significance: Relates shear stress $\tau$ to velocity gradient. Fluids obeying this are Newtonian (water, air); others are non-Newtonian.
Temperature Effects:
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Water: Viscosity decreases with temperature (molecular bonds weaken).
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Air: Viscosity increases with temperature (molecular momentum transfer rises).
Surface Tension & Capillarity:
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Surface Tension ($\sigma$): Force per unit length (N/m). Arises from cohesion.
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Capillary Rise/Fall:
$$ h = \frac{4\sigma \cos\theta}{\rho g d} $$
$\theta$: contact angle; $d$: tube diameter.
- Laplace Equation (droplet/bubble):
$$ \Delta p = \frac{4\sigma}{d} \quad \text{(droplet)} $$
$$ \Delta p = \frac{8\sigma}{d} \quad \text{(soap bubble, two surfaces)} $$
Pascal’s Law:
Pressure change in confined fluid transmits undiminished in all directions.
Proof: Consider equilibrium of fluid element; force balance gives $$\displaystyle dp = \gamma \, dh $$; for horizontal element, $$\displaystyle dp = 0 $$ → pressure same at all points on same horizontal plane.
Pressure Head:
$$ h = \frac{p}{\rho g} $$
Height of liquid column equivalent to pressure $p$.
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Common Pitfalls:
- Capillary rise: $$\displaystyle \cos\theta > 0 $$ for wetting fluids (water-glass), $$\displaystyle \cos\theta < 0 $$ for non-wetting (mercury-glass).
- Laplace for bubble: double surface → factor 8, not 4.
- Pascal’s law applies only to static fluids.
3. Kinematics of Fluid Flow
Flow Classification:
| Type | Basis | Example |
|---|---|---|
| Steady | $$\displaystyle \frac{\partial}{\partial t}(\text{property}) = 0 $$ | Constant flow in pipe |
| Unsteady | Time-dependent | Pump starting/stopping |
| Laminar | Smooth, ordered layers | Re < 2000 (pipe) |
| Turbulent | Chaotic, mixing | Re > 4000 (pipe) |
| Rotational | Vorticity $\omega \neq 0$ | Vortex flow |
| Irrotational | $$\displaystyle \omega = 0 $$ | Ideal flow far from boundaries |
Reynolds Experiment:
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Dye filament in glass tube:
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Low velocity → filament remains distinct (laminar).
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High velocity → filament diffuses (turbulent).
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Critical Reynolds Number:
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Pipe flow: $$\displaystyle Re_{crit} \approx 2000 $$–$2300$.
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Flat plate: $$\displaystyle Re_{crit} \approx 5 \times 10^5 $$ (based on distance from leading edge).
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Eulerian vs Lagrangian:
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Eulerian: Field description; observe fixed points in space. Used in most engineering problems.
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Lagrangian: Track individual fluid particles. Complex, used in particle dynamics.
Continuity Equation (3D Cartesian, compressible):
$$ \frac{\partial \rho}{\partial t} + \frac{\partial (\rho u)}{\partial x} + \frac{\partial (\rho v)}{\partial y} + \frac{\partial (\rho w)}{\partial z} = 0 $$
For incompressible ($$\displaystyle \rho = \text{constant} $$):
$$ \frac{\partial u}{\partial x} + \frac{\partial v}{\partial y} + \frac{\partial w}{\partial z} = 0 $$
Application: Given $u$ and $v$, find $w$: $$\displaystyle w = \int \left( -\frac{\partial u}{\partial x} - \frac{\partial v}{\partial y} \right) dz + f(x,y) $$.
Velocity Potential ($\phi$) & Stream Function ($\psi$):
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$\phi$: For irrotational flow, $$\displaystyle \vec{V} = \nabla \phi $$.
$$\displaystyle u = \frac{\partial \phi}{\partial x},\; v = \frac{\partial \phi}{\partial y} $$.
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$\psi$: For 2D incompressible flow,
$$\displaystyle u = \frac{\partial \psi}{\partial y},\; v = -\frac{\partial \psi}{\partial x} $$.
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Cauchy-Riemann Equations (for $\phi$ & $\psi$ to be conjugate):
$$ \frac{\partial \phi}{\partial x} = \frac{\partial \psi}{\partial y}, \quad \frac{\partial \phi}{\partial y} = -\frac{\partial \psi}{\partial x} $$
- Orthogonal Trajectories: $$\displaystyle \phi = \text{constant} $$ (equipotentials) and $$\displaystyle \psi = \text{constant} $$ (streamlines) intersect at $$\displaystyle 90^\circ $$.
Streamlines, Pathlines, Streaklines:
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Streamline: Instantaneous line tangent to velocity field.
$$\displaystyle \frac{dx}{u} = \frac{dy}{v} = \frac{dz}{w} $$.
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Pathline: Actual trajectory of a fluid particle.
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Streakline: Line joining all particles that passed through a fixed point.
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Steady flow: All three coincide. Unsteady: They differ.
Flow Nets: Grid of orthogonal streamlines and equipotentials. Used in groundwater flow, lubrication problems.
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Exam Tricks:
- Given $\phi$, find $u,v$ by differentiation; then integrate to get $\psi$ using Cauchy-Riemann.
- Continuity for 2D: $$\displaystyle \frac{\partial u}{\partial x} + \frac{\partial v}{\partial y} = 0 $$ is a quick check.
- Orthogonality proof: $$\displaystyle \nabla \phi \cdot \nabla \psi = 0 $$ from Cauchy-Riemann.
4. Dynamics of Inviscid Flow
Forces in Fluids:
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Surface Forces: Pressure (normal), viscous (tangential).
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Body Forces: Gravity, electromagnetic.
Euler’s Equation (along streamline, inviscid, steady):
$$ \frac{dp}{\rho} + g \, dz + V \, dV = 0 $$
Derivation: Apply Newton’s 2nd law to fluid element along streamline; pressure and gravity forces only.
Bernoulli’s Theorem (from Euler integration):
$$ \frac{p}{\rho g} + \frac{V^2}{2g} + z = \text{constant} $$
Assumptions:
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Inviscid ($$\displaystyle \mu = 0 $$)
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Steady flow
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Incompressible ($$\displaystyle \rho = \text{constant} $$)
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Along a streamline (or entire flow if irrotational)
Total Energy Line (TEL) & Hydraulic Gradient Line (HGL):
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TEL: Represents total head ($$\displaystyle \frac{p}{\rho g} + \frac{V^2}{2g} + z $$). Horizontal for ideal flow; slopes downward with losses.
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HGL: Represents pressure head ($$\displaystyle \frac{p}{\rho g} + z $$). Always below TEL by $$\displaystyle \frac{V^2}{2g} $$.
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Difference: TEL – HGL = velocity head.
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Common Errors:
- Bernoulli applies only along streamlines unless flow is irrotational.
- Do not mix units: use consistent (SI: m, kg, s).
- TEL slope = head loss per unit length; HGL slope = pressure gradient.
5. Viscous Flow and Boundary Layer Theory
Laminar Flow in Circular Pipes (Hagen–Poiseuille):
- Velocity Profile (parabolic):
$$ u(r) = u_{max} \left(1 - \frac{r^2}{R^2}\right) $$
where $$\displaystyle u_{max} = \frac{\Delta p \, R^2}{4\mu L} $$.
- Shear Stress:
$$ \tau(r) = \mu \frac{du}{dr} = -\frac{\Delta p}{2L} r $$
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At wall ($$\displaystyle r = R $$): $$\displaystyle \tau_w = \frac{\Delta p \, R}{2L} = \frac{4\mu u_{max}}{R} $$.
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At center ($$\displaystyle r = 0 $$): $$\displaystyle \tau = 0 $$.
Boundary Layer Theory:
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Concept: Thin region near solid surface where velocity from 0 to free-stream $U$ due to viscosity.
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Development over Flat Plate:
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Laminar: $$\displaystyle \delta \approx \frac{5x}{\sqrt{Re_x}} $$ (Blasius solution).
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Turbulent: $$\displaystyle \delta \approx \frac{0.37x}{Re_x^{1/5}} $$.
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Thicknesses:
- Displacement Thickness $$\displaystyle \delta^* $$:
$$ \delta^* = \int_0^\delta \left(1 - \frac{u}{U}\right) dy $$
Represents mass flow deficit.
- Momentum Thickness $\theta$:
$$ \theta = \int_0^\delta \frac{u}{U} \left(1 - \frac{u}{U}\right) dy $$
Used in momentum integral equation.
- Skin Friction Drag (flat plate):
$$ D_f = \tau_w \times \text{area} $$
For laminar: $$\displaystyle \tau_w = 0.332 \rho U^2 / \sqrt{Re_x} $$.
Turbulence:
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Characteristics: Random fluctuations, enhanced mixing, energy cascade.
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Effect on Velocity Profile: Fuller (flatter) than laminar; increased momentum transfer.
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Energy Dissipation: Viscous dissipation of turbulent kinetic energy into heat.
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Key Formulas:
- Pipe flow shear: $$\displaystyle \tau_w = \frac{\Delta p D}{4L} $$.
- Boundary layer thickness: $$\displaystyle \delta \propto x / \sqrt{Re_x} $$ (lam), $$\displaystyle \delta \propto x / Re_x^{1/5} $$ (turb).
- Drag reduction: Delay transition (smooth surface) or use turbulent boundary layer (delayed separation).
6. Flow Measurement and Instrumentation
Pitot–Static Tube:
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Construction: Forward-facing pitot (stagnation) + side static ports.
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Working:
$$\displaystyle p_0 = p + \frac{1}{2}\rho V^2 $$ (stagnation pressure)
$p$ = static pressure.
Velocity:
$$ V = \sqrt{\frac{2(p_0 - p)}{\rho}} = C \sqrt{\frac{2\Delta p}{\rho}} $$
$C$: calibration coefficient (~0.98–1.0).
Manometers:
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Principle: Balance pressure by liquid column height.
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Simple Manometer (U-tube):
$$\displaystyle p_1 - p_2 = (\rho_m - \rho) g h $$ (if one side open to atmosphere).
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Differential Manometer: Measures $$\displaystyle p_1 - p_2 $$ directly with two connections.
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Inclined Manometer: Amplifies deflection for low pressure; $$\displaystyle h = L \sin\theta $$, $$\displaystyle p_1 - p_2 = \rho g L \sin\theta $$.
Capillary Effects in Manometers:
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Error: Meniscus curvature in small-diameter tubes gives false reading.
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Correction:
$$ h_{corr} = \frac{4\sigma \cos\theta}{\rho g d} $$
Subtract from observed $h$ if wetting ($$\displaystyle \theta < 90^\circ $$).
- Max Allowable Diameter for error $$\displaystyle < \epsilon $$:
$$ d > \frac{4\sigma \cos\theta}{\rho g h \epsilon} $$
Other Flow Meters:
- Venturi Meter:
$$ Q = A_1 A_2 \sqrt{\frac{2(p_1 - p_2)}{\rho (A_1^2 - A_2^2)}} $$
(Theoretical, apply discharge coefficient $$\displaystyle C_d $$).
- Orifice Meter: Similar but with higher losses; $$\displaystyle C_d \approx 0.6 $$–$0.7$.
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Pitot Tube: Ensure alignment with flow; use for velocity only.
Manometer: Always write pressure balance equation; include all fluid densities.
Capillary: Correction adds to measured $h$ for wetting fluids (water in glass).
7. Applications of Fluid Mechanics
Reciprocating Pump:
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Components: Cylinder, piston, suction valve, delivery valve, crank.
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Working:
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Suction stroke: piston moves left, suction valve opens, water enters.
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Delivery stroke: piston moves right, suction valve closes, delivery valve opens, water discharged.
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Discharge: $$\displaystyle Q = A \times L \times N \times \eta_v $$ (volumetric efficiency accounts for slip).
Reaction Turbine (e.g., Francis):
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Principle: Both pressure and kinetic energy of water convert to rotational energy.
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Construction: Spiral casing, guide vanes, runner (rotor), draft tube.
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Working: Water enters spiral casing → guide vanes direct onto runner blades at optimal angle → pressure drop occurs both in casing and over blades → runner rotates → water exits via draft tube (recovers kinetic energy).
Biofluid Mechanics:
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Blood Flow: Non-Newtonian (shear-thinning), pulsatile.
Reynolds number in aorta ~ 2000 (transition risk).
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Heart: Acts as pulsatile pump; pressure–volume loop describes cardiac cycle.
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Veins: Valves prevent backflow; flow aided by muscle pump.
Buoyancy & Flotation:
- Archimedes’ Principle:
$$ F_b = \gamma_f V_{sub} = \rho_f g V_{sub} $$
(Buoyant force equals weight of displaced fluid).
- Floating Body:
$$ \rho_{body} = \rho_f \times \frac{V_{sub}}{V_{total}} $$
Weight = Buoyancy: $$\displaystyle \rho_{body} g V_{total} = \rho_f g V_{sub} $$.
Hydrostatic Pressure:
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Barometer: $$\displaystyle p_{atm} = \rho_{Hg} g h $$ (mercury column).
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Pressure at Depth:
$$ p = p_{atm} + \rho g h $$
(Gauge pressure: $$\displaystyle p_{gauge} = \rho g h $$).
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Pump Discharge: Remember slip $$\displaystyle s = \frac{\text{theoretical} - \text{actual}}{\text{theoretical}} $$.
Turbine vs Pump: Turbine extracts energy; pump adds energy.
Buoyancy: For floating, $$\displaystyle V_{sub} $$ adjusts so weight = buoyancy.
Barometer: Use $$\displaystyle \rho_{Hg} = 13600 $$ kg/m³, $$\displaystyle g = 9.81 $$ m/s².
Quick Reference Table: Exam-Favorite Formulas
| Topic | Formula | Notes |
|---|---|---|
| Viscosity (shear stress) | $$\displaystyle \tau = \mu \frac{du}{dy} $$ | Newtonian fluids |
| Capillary rise | $$\displaystyle h = \frac{4\sigma \cos\theta}{\rho g d} $$ | For circular tube |
| Continuity (2D incomp.) | $$\displaystyle \frac{\partial u}{\partial x} + \frac{\partial v}{\partial y} = 0 $$ | |
| Bernoulli | $$\displaystyle \frac{p}{\rho g} + \frac{V^2}{2g} + z = H $$ | $H$ = total head |
| Pipe flow ( Hagen-Poiseuille) | $$\displaystyle Q = \frac{\pi R^4 \Delta p}{8\mu L} $$ | Laminar only |
| Boundary layer (lam.) | $$\displaystyle \delta \approx \frac{5x}{\sqrt{Re_x}} $$ | Blasius solution |
| Pitot velocity | $$\displaystyle V = \sqrt{\frac{2\Delta p}{\rho}} $$ | $$\displaystyle \Delta p = p_0 - p $$ |
| Buoyancy | $$\displaystyle F_b = \rho_f g V_{sub} $$ | |
| Pressure at depth | $$\displaystyle p = p_0 + \rho g h $$ | $$\displaystyle p_0 $$ = surface pressure |
Final Advice:
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Definitions: Memorize exact wording (e.g., fluid, viscosity, Bernoulli assumptions).
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Derivations: Practice continuity, Euler, Bernoulli – they are 7-mark questions.
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Numericals: Focus on pipe flow (shear stress), boundary layer thickness, manometers with capillary correction, buoyancy.
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Diagrams: Sketch Pitot tube, boundary layer development, flow net, reciprocating pump cycle.
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Units: Always check SI consistency (Pa, m, kg, s).
Past Paper Pattern:
- 7-mark: Definitions, explanations, derivations, simple numerics.
- 14-mark: Combined problems (e.g., continuity + potential, Bernoulli + manometer).
- Frequent: Viscosity calculations, Reynolds experiment, Pitot, capillary, boundary layer, buoyancy, Bernoulli applications.