Fluid Mechanics
PromiseClassify hydrostatic vs flow in 15 seconds; one free-body or streamline equation plus a consistency check finishes most stems under 90 seconds.
01. Hydrostatics is force balance on a fluid element or immersed body: ΔP=ρgh along a vertical, and Pascal transmits pressure change undiminished in a confined incompressible liquid.
02. Buoyancy equals the weight of displaced fluid (Archimedes). Apparent weight and floating equilibrium are static free-body statements, not flow formulas.
03. For steady ideal flow along a streamline, continuity (A₁v₁=A₂v₂ for incompressible) and Bernoulli (P+½ρv²+ρgh=const) are energy/mass bookkeeping—not universal laws for every pipe.
How Advanced asks this
- Manometer / hydraulic-press / force on a gate with Pascal and ρgh
- Floating or fully submerged body: apparent weight, fraction immersed, two-liquid layers
- Venturi, Torricelli, siphon or tank-hole speed from Bernoulli + continuity
- Horizontal/vertical U-tube oscillation or pressure difference from height of liquid columns
- Sphere falling in viscous liquid: terminal velocity, viscosity from timing, Stokes vs buoyancy
- Multi-correct statements mixing streamline assumptions with viscosity or turbulence cues
Traps that leak marks
- Using Bernoulli on a Stokes/viscous terminal-velocity stem
- Confusing gauge and absolute pressure in manometers
- Taking buoyancy with body density instead of fluid density
- Applying A₁v₁=A₂v₂ to compressible or unsteady jets without care
- Forgetting buoyancy when writing terminal-velocity force balance
- Bernoulli on a Stokes/viscous terminal-velocity stem
- Buoyancy with body density instead of fluid density
- Confusing gauge and absolute pressure in manometers
Must cover (this topic)
- Bernoulli applications
- Stokes + terminal velocity
60–90s process
- 0–15s — Decide: hydrostatic pressure/Pascal, buoyancy free-body, ideal streamline flow, or Stokes/terminal.
- 15–35s — Draw free surface, datum, streamlines or FBD; write ΔP=ρgh, F_B=ρVg, continuity, Bernoulli, or ΣF=0 for terminal.
- 35–75s — Solve with consistent gauge/absolute choice and one density per fluid layer; cancel ρg when only height ratios matter.
- 75–90s — Check direction of pressure change with depth, floating fraction ≤1, and that Bernoulli was not used on a Stokes stem.
Methods that change the score
Hydrostatics FBDs and Bernoulli-with-stated-assumptions cover the high-yield fluid asks.
Method 01 · Column-by-column pressure walk
Manometer puzzles become arithmetic instead of memorised shapes.
Do this: Start from a known free surface or shared level and add/subtract ρgh for each vertical segment.
Method 02 · Displaced-volume free body
Floating and apparent-weight stems are pure statics once V_displaced is identified.
Do this: Write mg, F_B and any tensions/normal forces; never invent a Bernoulli term on a static body.
Method 03 · Streamline energy ledger
Venturi and Torricelli reduce to one algebraic difference of P, v and h.
Do this: Pick two points on one streamline; write Bernoulli once; insert continuity if areas change.
Method 04 · Terminal force triangle
Separates density difference from viscosity cleanly and blocks Poiseuille misuse.
Do this: At v_t set weight = buoyancy + Stokes drag (directions clear for rising bubble vs falling sphere).
Quick formulas
- Hydrostatic gradient: ΔP=ρgh (vertical); P=P₀+ρgh below free surface — Incompressible liquid columns and manometers
- Pascal: ΔP transmitted undiminished; F₁/A₁=F₂/A₂ (ideal hydraulic press) — Confined liquid force multiplication
- Archimedes: F_B=ρ_fluid V_displaced g; W_app=W−F_B — Immersed or floating bodies
- Floating: mg=ρ_fluid V_immersed g ⇒ V_imm/V=ρ_body/ρ_fluid — Equilibrium float in one fluid
- Continuity: A₁v₁=A₂v₂ (incompressible, steady) — Same volume flux through sections
- Bernoulli: P+½ρv²+ρgh=const along streamline (ideal, steady, incompressible) — Venturi, Torricelli, siphon
- Torricelli: v=√(2gh) from free surface to hole (ideal) — Tank orifice with negligible surface speed
- Stokes / terminal: F_d=6πηrv; at terminal: 6πηrv_t=(ρ−σ)V g — Small sphere in viscous fluid, Re≪1
Common question families
Hydrostatics and buoyancy
Looks like: Pressure depth, Pascal, floating/submerged
Fast model: P = P₀+ρgh; buoyant force = weight of displaced fluid.
Bernoulli + continuity
Looks like: Venturi, tank efflux, or streamline speed/pressure
Fast model: A₁v₁=A₂v₂ and P+ρgh+½ρv² constant along streamline.
Viscosity and terminal velocity
Looks like: Stokes drag, sphere in fluid
Fast model: At terminal speed, weight = buoyancy + drag.
Surface tension and capillarity
Looks like: Drop/bubble excess pressure, capillary rise
Fast model: ΔP = 2σ/r (drop) or 4σ/r (soap bubble); h=2σcosθ/(ρgr).
Sample preview · Hydrostatics and buoyancy
A wooden cube of relative density 0.8 floats in water. Find the fraction submerged.
Answer: 0.8
Floating balance equates weights of body and displaced liquid.