Fluid mechanics Study Guide
Study Guide
📖 Core Concepts
Fluid Mechanics – study of liquids, gases, plasmas and the forces acting on them; split into fluid statics (at rest) and fluid dynamics (in motion).
Continuum Assumption – treat fluid as continuous matter; properties (ρ, p, T, u) defined at infinitesimal volumes large compared with molecular scales.
Conservation Laws – mass, momentum, and energy are conserved inside any control volume.
Knudsen Number $Kn=\lambda/L$ – measures molecular mean‑free‑path ($\lambda$) vs characteristic length ($L$); $Kn<0.1$ ⇒ continuum valid.
Reynolds Number $Re=\rho UL/\mu$ – ratio of inertial to viscous forces; determines laminar vs turbulent regime.
Viscosity – internal friction; zero for an inviscid fluid, linear with shear rate for a Newtonian fluid ($\tau=\mu\dot\gamma$).
Navier–Stokes Equations – momentum balance for a viscous fluid; reduce to Euler equations when $\mu=0$.
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📌 Must Remember
Archimedes’ principle: upward force = weight of displaced fluid.
Pascal’s law: pressure change applied to an incompressible fluid is transmitted undiminished throughout.
Continuum validity: $Kn<0.1$.
Reynolds number thresholds (order of magnitude):
$Re\lesssim 2000$ → laminar (steady, smooth).
$Re\gtrsim 4000$ → turbulent (chaotic).
Newtonian fluid stress: $\tau = \mu \dot\gamma$.
Navier–Stokes (incompressible):
$$\rho\left(\frac{\partial \mathbf{u}}{\partial t}+ \mathbf{u}\cdot\nabla\mathbf{u}\right)= -\nabla p + \mu\nabla^{2}\mathbf{u}+ \rho\mathbf{g}$$
Euler equations: same as above with $\mu=0$.
Boundary‑layer no‑slip: fluid velocity equals solid surface velocity at the wall.
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🔄 Key Processes
Applying Conservation of Mass (Continuity):
For incompressible flow: $\nabla\cdot\mathbf{u}=0$.
For control volume: $\displaystyle \frac{d}{dt}\int{CV}\rho\,dV = -\int{CS}\rho\mathbf{u}\cdot d\mathbf{A}$.
Evaluating Flow Regime:
Compute $Re=\rho UL/\mu$.
Compare to laminar/turbulent limits → choose analytical (laminar) or CFD/turbulence model (turbulent).
Deriving Pressure Variation with Depth (Hydrostatics):
$dp = -\rho g\,dz$ → $p(z)=p0+\rho g h$.
Setting Up Navier–Stokes for a Problem:
Identify control volume, assume incompressible/steady if justified.
Write momentum equations, apply boundary conditions (no‑slip, pressure inlet/outlet).
Simplify (e.g., neglect $\mu\nabla^2\mathbf{u}$ for high‑Re inviscid flow).
CFD Workflow (high‑level):
Geometry → Mesh → Governing equations (NS) → Solver settings (turbulence model) → Convergence check → Post‑process results.
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🔍 Key Comparisons
Inviscid vs Viscous
Inviscid: $\mu=0$, no shear stress, Euler equations, only good away from walls.
Viscous: $\mu>0$, shear stress present, Navier–Stokes, essential in boundary layers.
Newtonian vs Non‑Newtonian
Newtonian: $\tau \propto \dot\gamma$ (linear).
Non‑Newtonian: $\tau$–$\dot\gamma$ relation non‑linear (shear‑thinning, shear‑thickening, yield stress).
Ideal vs Real Fluid
Ideal: non‑viscous and incompressible (theoretical tool).
Real: has viscosity, may be compressible; only approximated as ideal when viscous effects negligible.
Laminar vs Turbulent Flow
Laminar: smooth streamlines, $Re$ low, analytical solutions often possible.
Turbulent: chaotic eddies, $Re$ high, requires statistical models or CFD.
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⚠️ Common Misunderstandings
“Zero viscosity = no drag.” Real fluids always have some viscosity; only superfluids approach $\mu=0$.
“High Reynolds number always means turbulent.” Transitional ranges exist (≈2000–4000); geometry and disturbances also matter.
“Euler equations work near walls.” They ignore the no‑slip condition; boundary layers must be treated with Navier–Stokes or boundary‑layer theory.
“All fluids are Newtonian.” Many biological or industrial fluids (blood, polymer melts) are non‑Newtonian.
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🧠 Mental Models / Intuition
Fluid parcels as “tiny ships”: they carry mass, momentum, and energy; forces act on them just like on a small boat.
Reynolds number as “inertia vs friction”: imagine pushing a sled (low $Re$ – friction dominates) vs a race car (high $Re$ – inertia dominates).
Boundary layer as “traffic jam”: fluid right at the wall slows to zero (no‑slip), creating a thin region where velocity changes rapidly.
Continuum ≈ “smooth road”: if your car’s wheels (molecules) are much smaller than the road’s bumps (system length), you can treat the road as smooth.
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🚩 Exceptions & Edge Cases
$Kn \ge 0.1$ (rarefied gases): continuum equations break down; need Boltzmann equation or DSMC methods.
Superfluid helium: behaves as an inviscid fluid but exhibits quantum effects; not covered by classical NS.
Highly compressible flows (Mach > 0.3): density variations become significant; incompressible assumption fails.
Non‑Newtonian shear‑thickening fluids: apparent viscosity increases with shear rate, opposite of many polymer solutions.
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📍 When to Use Which
Inviscid (Euler) analysis:
Flow away from solid surfaces, $Re \gg 1$, and viscous forces negligible.
Viscous (Navier–Stokes) analysis:
Near walls, low‑$Re$ devices, or any situation where shear stress matters.
Laminar analytical solution:
Simple geometry, $Re$ low, steady state (e.g., Hagen–Poiseuille flow).
Turbulent CFD:
$Re$ high, complex geometry, or unsteady flow where analytical methods fail.
Newtonian model:
Water, air, most gases under standard conditions.
Non‑Newtonian model:
Blood, polymer melts, ketchup, paints – use power‑law or Bingham models.
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👀 Patterns to Recognize
Linear pressure gradient → Poiseuille (parabolic) velocity profile in straight pipes.
$p$ decreasing linearly with depth → hydrostatic balance.
Separation of variables in NS → possible only for low‑$Re$, simple geometries.
Sharp rise in drag coefficient near critical $Re$ → transition to turbulence.
Boundary‑layer thickness $\delta \sim \sqrt{\nu x/U}$ for laminar flat‑plate flow.
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🗂️ Exam Traps
Choosing Euler instead of Navier–Stokes for a problem that mentions a solid wall → you’ll miss the no‑slip condition.
Using $Re$ formula with wrong characteristic length (e.g., pipe diameter vs hydraulic radius) → answer off by a factor.
Assuming incompressibility for high‑speed gas flows (Mach > 0.3) → density changes invalidate the simplification.
Mixing up pressure drop signs: $dp = -\rho g\,dz$; forgetting the negative leads to pressure increasing with depth incorrectly.
Treating a non‑Newtonian fluid as Newtonian when the problem states “shear‑thickening” or “yield stress.”
Neglecting the Knudsen number for micro‑scale flows (MEMS); continuum equations give non‑physical results.
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