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Unit · year 3

PU-307 · Fluid Dynamics

Threads force · energy · matter · waves · symmetry · fields · chance28 lectures18 derivations

Starting from the continuum hypothesis and conservation laws, the unit builds the Navier-Stokes equations as the governing dynamics of a deforming material and then explores their structure through the two great limits that make fluids tractable: inviscid, high-Reynolds-number flow (Euler, Bernoulli, vorticity, potential flow) and viscous-dominated, low-Reynolds-number flow (Stokes drag). It closes by confronting where clean theory breaks down — boundary layers, waves, instability, and turbulence — showing how dimensional reasoning and scaling recover predictive power when exact solutions fail.

PREREQUISITES

PU-101, PU-104, PU-201, PU-202

Lectures

L01
The Continuum Hypothesis and the Fluid Description
L02
Kinematics: Material Derivative, Streamlines, and Deformation
L03
The Reynolds Transport Theorem
L04
Conservation of Mass: The Continuity Equation
L05
Stress in a Continuum: The Cauchy Stress Tensor
L06
Cauchy's Momentum Equation
L07
Constitutive Relations and the Navier-Stokes Equations
L08
Boundary Conditions and the No-Slip Condition
L09
Exact Solutions: Couette and Poiseuille Flow
L10
Energy, Dissipation, and the First Law for Fluids
L11
The Inviscid Limit: Euler's Equations
L12
Bernoulli's Theorem and Its Applications
L13
Vorticity and Its Transport
L14
Kelvin's Circulation Theorem
L15
Helmholtz Vortex Theorems and Vortex Dynamics
L16
Potential Flow and Laplace's Equation
L17
Complex Potentials and Flow Past a Cylinder
L18
D'Alembert's Paradox
L19
Lift, Circulation, and the Kutta-Joukowski Theorem
L20
Dimensional Analysis and the Reynolds Number
L21
Creeping Flow and Stokes Drag
L22
High Reynolds Number: Prandtl's Boundary Layer
L23
Boundary-Layer Separation and Form Drag
L24
Compressible Flow and Sound Waves
L25
Surface Gravity Waves
L26
Hydrodynamic Instability: Kelvin-Helmholtz and Rayleigh-Taylor
L27
Introduction to Turbulence: The Energy Cascade
L28
Kolmogorov's Theory and the Four-Fifths Law

Derivations homed in this unit

D-314

Reynolds Transport Theorem

Derives the rate of change of an extensive quantity over a moving material volume by applying the Leibniz rule to a control volume with a moving boundary.

D-315

The Continuity Equation

Derives the local mass-conservation law ∂ρ/∂t + ∇·(ρu) = 0 by applying the Reynolds transport theorem to total mass.

D-316

Existence of the Cauchy Stress Tensor

Proves via the tetrahedron argument that the surface traction depends linearly on the outward normal, establishing the second-rank stress tensor.

D-317

Cauchy's Momentum Equation

Derives the differential momentum balance ρ Du/Dt = ∇·σ + ρf from the transport theorem plus the divergence of the stress tensor.

D-318

Navier-Stokes from the Newtonian Constitutive Law

Closes Cauchy's equation by positing a linear, isotropic stress–strain-rate relation, yielding the incompressible Navier-Stokes equations.

D-319

Euler's Equations as the Inviscid Limit

Recovers the inviscid Euler equations by taking viscosity to zero and discusses the singular nature of that limit near boundaries.

D-320

Bernoulli's Theorem, Steady and Unsteady

Integrates Euler's equation along streamlines for steady flow and over the whole field for irrotational flow to obtain the two Bernoulli relations.

D-321

The Vorticity Transport Equation

Takes the curl of Navier-Stokes to obtain the evolution of vorticity with its stretching, tilting, and diffusion terms.

D-322

Kelvin's Circulation Theorem

Proves that circulation around a material loop is conserved in barotropic, inviscid flow with conservative body forces.

D-323

Potential Flow and Laplace's Equation

Shows that incompressible irrotational flow admits a velocity potential satisfying Laplace's equation, linearising the problem.

D-324

D'Alembert's Paradox

Demonstrates that steady potential flow past a body produces zero net drag, exposing the need for viscosity and boundary layers.

D-325

Stokes Drag on a Sphere

Solves the creeping-flow (Stokes) equations around a sphere to obtain the drag force F = 6πμaU.

D-326

The Reynolds Number from Nondimensionalisation

Nondimensionalises Navier-Stokes to reveal the Reynolds number as the sole governing parameter and grounds dynamic similarity via the Buckingham Pi theorem.

D-327

Energy Balance and Viscous Dissipation

Derives the mechanical-energy equation and identifies the positive-definite viscous dissipation function as the rate of irreversible heating.

D-328

The Acoustic Wave Equation and Speed of Sound

Linearises the compressible Euler and continuity equations about a rest state to obtain the wave equation with c² = (∂p/∂ρ)_s.

D-329

Prandtl's Boundary-Layer Equations

Uses matched scaling of Navier-Stokes at high Reynolds number to reduce the near-wall dynamics to the boundary-layer equations.

D-330

Dispersion of Surface Gravity Waves

Solves potential flow with linearised free-surface conditions to obtain ω² = gk tanh(kh) and its deep- and shallow-water limits.

D-331

Kolmogorov's Four-Fifths Law

Derives the exact -4/5 scaling of the third-order longitudinal velocity structure function from the Kármán-Howarth equation under homogeneous isotropic turbulence.