1. Pressure in a Fluid

Pressure is defined as the normal force per unit area exerted by a fluid:

P=FA

SI unit: Pascal (Pa) = N/m². Other units: 1 atm=1.013×105 Pa; 1 bar=105 Pa; 1 mmHg=133.3 Pa.

Pressure at a Depth in a Static Fluid

For a fluid of uniform density ρ at rest, the pressure at depth h below the free surface is:

P=P0+ρgh

where P0 is the atmospheric pressure at the surface. Key properties:

  • Pressure depends only on depth, not on the shape or cross-section of the container (Hydrostatic Paradox).
  • Pressure acts equally in all directions at any point in a static fluid (Pascal's Law basis).
  • All points at the same horizontal level in a connected static fluid have the same pressure.

Gauge Pressure and Absolute Pressure

Type Definition Formula
Absolute Pressure Total pressure including atmosphere Pabs=P0+ρgh
Gauge Pressure Pressure above atmospheric Pgauge=PabsP0=ρgh
Vacuum Pressure Pressure below atmospheric Pvac=P0Pabs

2. Pascal's Law and Its Applications

Pascal's Law: A change in pressure applied to an enclosed fluid is transmitted undiminished to every point of the fluid and to the walls of the container.

F1A1=F2A2         F2=F1A2A1

  • Hydraulic Lift / Press: A small force F1 on a small piston of area A1 generates a large force F2 at a large piston of area A2. This is the working principle of hydraulic brakes, hydraulic jacks, and car lifts.
  • Work done is conserved: F1d1=F2d2, so the smaller piston moves a larger distance.
  • Hydraulic Brakes: Pressure applied at the brake pedal is transmitted equally to all four wheel cylinders, applying equal braking force at all wheels.

3. Buoyancy and Archimedes' Principle

When a body is partially or fully submerged in a fluid, the fluid exerts an upward force on it called the buoyant force or upthrust.

Archimedes' Principle

The buoyant force on a submerged (or floating) body equals the weight of the fluid displaced by the body:

Fb=ρfluidVdisplacedg

The buoyant force acts upward through the centre of buoyancy — the centroid of the displaced fluid volume.

Conditions for Floating, Sinking, and Neutral Buoyancy

Condition Relation Result
ρbody<ρfluid Fb>W Body floats (partially submerged)
ρbody=ρfluid Fb=W Neutral buoyancy (suspended anywhere)
ρbody>ρfluid Fb<W Body sinks

Law of Flotation

For a freely floating body, weight of body = weight of fluid displaced:

ρbodyVbodyg=ρfluidVsubmergedg

VsubmergedVbody=ρbodyρfluid

This ratio gives the fraction of the body submerged. For example, ice (ρ=917 kg/m³) in water (ρ=1000 kg/m³): fraction submerged =9171000=0.917, i.e., about 91.7% of an iceberg is below water.

Apparent Weight

When a body of density ρb is fully submerged in a fluid of density ρf:

Wapparent=WactualFb=mg(1ρfρb)

4. Fluid Dynamics — Equation of Continuity

For a fluid in motion, we assume it is ideal (incompressible, non-viscous, irrotational, streamline flow) unless stated otherwise.

Streamlines and Laminar Flow

  • A streamline is a curve whose tangent at any point gives the direction of fluid velocity at that point. Streamlines never cross each other.
  • Laminar (streamline) flow: Orderly flow where layers of fluid slide past each other without mixing. Occurs at low speeds.
  • Turbulent flow: Irregular, chaotic flow with eddies and vortices. Occurs above a critical speed.

Equation of Continuity

For an incompressible fluid flowing through a pipe of varying cross-section, the mass flow rate is constant:

A1v1=A2v2=constant    (Volume flow rate Q)

where A is the cross-sectional area and v is the fluid speed. This means:

  • Where the pipe is narrower (A smaller), fluid flows faster (v larger).
  • Where the pipe is wider (A larger), fluid flows slower (v smaller).

5. Bernoulli's Theorem

For an ideal fluid in steady flow, the total mechanical energy per unit volume remains constant along a streamline:

P+12ρv2+ρgh=constant

This is essentially the conservation of energy applied to fluid flow. The three terms represent:

  • P — pressure energy per unit volume
  • 12ρv2 — kinetic energy per unit volume
  • ρgh — potential energy per unit volume

Between any two points 1 and 2 along a streamline:

P1+12ρv12+ρgh1=P2+12ρv22+ρgh2

Applications of Bernoulli's Theorem

(i) Venturimeter

A device to measure the flow speed of a fluid in a pipe. It has a constriction (throat) where velocity increases and pressure drops. The flow speed is:

v1=A22(P1P2)ρ(A12A22)

(ii) Torricelli's Theorem — Speed of Efflux

For a liquid in a large open tank with a small orifice at depth h below the free surface:

v=2gh

This is the same as the speed of a body falling freely from height h. The liquid behaves like a projectile after leaving the orifice — it follows a parabolic path.

Range of the liquid jet on the ground (orifice at height H above ground, depth h below surface):

x=2h(Hh)

Maximum range occurs when h=H/2, i.e., the orifice is at the midpoint of the tank height.

(iii) Dynamic Lift — Aerofoil and Magnus Effect

  • Aerofoil (Aircraft Wing): The wing is shaped so that air flows faster over the curved upper surface than the flat lower surface. By Bernoulli's theorem, pressure above is lower, creating a net upward lift force.
  • Magnus Effect: A spinning ball curves in flight because spin creates unequal air speeds on two sides, leading to a pressure difference and a sideways force (used in cricket, tennis, football).

6. Viscosity

Viscosity is the property of a fluid by virtue of which it opposes relative motion between its adjacent layers. It is the fluid equivalent of friction in solids.

Newton's Law of Viscosity

The viscous force between two adjacent fluid layers is:

F=ηAdvdx

where η is the coefficient of viscosity (dynamic viscosity), A is the area of the layer, and dvdx is the velocity gradient (rate of shear). SI unit of η: Pa·s (or Poise in CGS: 1 Pa·s=10 Poise).

Effect of Temperature on Viscosity

Fluid Type Effect of Increasing Temperature on η Reason
Liquids η decreases Intermolecular cohesive forces weaken
Gases η increases Molecular momentum transfer increases

Stokes' Law and Terminal Velocity

When a small sphere of radius r moves through a viscous fluid with velocity v, the viscous drag force is:

Fdrag=6πηrv    (Stokes' Law)

A body falling through a viscous fluid accelerates until the net downward force is zero. At this point it reaches terminal velocity vT:

W=Fb+Fdrag

mg=ρfVg+6πηrvT

vT=2r2(ρbρf)g9η

  • vTr2 — larger droplets fall faster (important in rainfall and cloud physics).
  • vT(ρbρf) — if ρb<ρf, terminal velocity is upward (bubble rising in liquid).
  • vT1η — more viscous fluids give lower terminal velocity.

7. Surface Tension

Surface tension (T or S) is the property of a liquid surface that makes it behave like a stretched elastic membrane. It arises due to the net inward cohesive force on surface molecules.

T=Fl    (force per unit length)

SI unit: N/m. It can also be expressed as surface energy per unit area: J/m².

Excess Pressure Inside Curved Surfaces

Surface Excess Pressure (ΔP) Reason
Liquid drop (1 surface) ΔP=2TR One liquid-air interface
Soap bubble (2 surfaces) ΔP=4TR Two soap-air interfaces (inner & outer)
Air bubble in liquid (1 surface) ΔP=2TR One liquid-air interface

Capillarity — Capillary Rise and Fall

When a capillary tube of radius r is dipped in a liquid of surface tension T, density ρ, and contact angle θ:

h=2Tcosθρgr

  • If θ<90° (e.g., water in glass): liquid rises — meniscus is concave.
  • If θ>90° (e.g., mercury in glass): liquid falls — meniscus is convex.
  • Capillary rise is independent of the shape of the tube — depends only on radius at the meniscus.
  • h1r — narrower tubes show greater rise.

Effect of Temperature on Surface Tension

Surface tension decreases with increasing temperature and becomes zero at the critical temperature (boiling point for most liquids). This is why hot water cleans better than cold water.

8. Reynolds Number

The Reynolds number (Re) is a dimensionless quantity that predicts whether fluid flow will be laminar or turbulent:

Re=ρvdη

where ρ = fluid density, v = flow speed, d = diameter of pipe, η = coefficient of viscosity.

Reynolds Number Type of Flow
Re<1000 Laminar (streamline) flow
1000<Re<2000 Unstable / transitional flow
Re>2000 Turbulent flow