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L-9: Properties of Fluids

Physics — Class 12 · NIOS Code 312 · Module 2 · Source: 312_Physics_Eng_Lesson9.pdf

Fluids All Around — Why This Lesson Matters

Fluids (liquids and gases) flow when conditions permit. Unlike solids, fluids cannot sustain shearing stress — they exert forces normal to surfaces. This lesson explains why dam walls thicken at the base, hydraulic jacks lift cars, mosquitoes walk on water, honey flows slowly, and cricket balls swing in air.

NIOS objectives: hydrostatic pressure; buoyancy and Archimedes' principle; Pascal's law and hydraulic devices; surface tension and surface energy; capillary rise; streamline vs turbulent flow; Reynolds number; viscosity; Bernoulli's principle and applications.

9.1 Hydrostatic Pressure

Pressure is thrust (normal force) per unit area — the same force has greater effect on a smaller area (sharp pin vs blunt rod).

P = F / A
P = Pressure (pascal, Pa = N·m⁻²)
F = Normal force / thrust (N)
A = Area (m²)
SI unit named after Blaise Pascal.
Fig 9.1 & 9.3 — Dam & Pressure vs Depth water surface P ∝ h Wall thicker at base
Fig 9.1/9.3 — Hydrostatic pressure increases with depth → thicker dam walls

Fluids at rest exert hydrostatic pressure. Consider a vertical cylinder of area A and height h in a liquid of density ρ. Equilibrium of the liquid column gives:

P = ρ g h
P = Gauge pressure at depth h (Pa)
ρ = Liquid density (kg·m⁻³)
g = 9.8 m·s⁻²
h = Depth below free surface (m)
Pressure increases linearly with depth — dam walls thicker at base.

At the open surface, add atmospheric pressure:

P = P_atm + ρ g h
Absolute pressure at depth h.
P_atm ≈ 1.01×10⁵ Pa (76 cm Hg barometer — Torricelli).
Pressure at given depth is independent of container shape (Fig. 9.5).

Example 9.1: Dam depth 100 m, ρ = 10³ kg/m³ → P = 9.8×10⁵ Pa. If 1 m wall withstands 10⁵ Pa, bottom wall needs ~9.8 m thickness.

Fig 9.6 — Torricelli Barometer 76 cm Hg P_atm = hρg ≈ 1.01×10⁵ Pa
Fig 9.6 — Mercury column 76 cm balances atmospheric pressure

9.1.2 Atmospheric Pressure

Earth's atmosphere extends ~200 km. O. von Guericke showed with evacuated copper hemispheres that 8 horses could barely pull them apart. Standard atmospheric pressure from mercury barometer:

P_atm = h ρ_Hg g ≈ 1.01 × 10⁵ Pa
h = 0.76 m mercury column.
ρ_Hg = 13600 kg·m⁻³
Fig 9.7 — Buoyancy States float B=W sink partial
Fig 9.7 — Floating, sinking, and partial immersion under buoyant force

9.2 Buoyancy and Archimedes' Principle

Lifting an object underwater feels easier because the fluid exerts an upward buoyant force. Archimedes' principle: when a body is submerged wholly or partially, buoyant force equals the weight of displaced fluid.

  • Floating: buoyant force = weight of object; object displaces fluid equal to its own weight.
  • Sinking: object denser than fluid — net downward force.
  • Hot-air balloon: less dense hot air → net upward buoyancy in cold air.
Fig 9.9 — Hydraulic Lift CAR F₁ (small) same P everywhere F₂ = F₁(A₂/A₁)
Fig 9.9 — Small force on narrow piston lifts heavy load on wide piston

9.3 Pascal's Law

When pressure is applied at any point in an enclosed liquid, it is transmitted undiminished to every point and to the container walls. This is the law of transmission of liquid pressure.

         PASCAL'S LAW — HYDRAULIC DEVICES
         =================================
    Small piston (A₁)          Large piston (A₂)
         F₁ applied    ──liquid──►   lifts load F₂
                    |
                    v
         Same pressure P = F₁/A₁ = F₂/A₂
                    |
                    v
         F₂ = F₁ × (A₂/A₁)   →  force multiplication
F₂ = F₁ × (A₂/A₁)
Applications: hydraulic press, balance, jack, brakes.
Driver's small force on brake pedal → large force on all four wheel cylinders simultaneously.

Intext check: Boy 25 kg on 0.05 m² vs elephant 5000 kg on 10 m² — ratio A₂/A₁ = 200, so boy can balance 25×200 = 5000 kg!

9.4 Surface Tension

Liquid drops are spherical; soap bubbles form easily but pure water bubbles do not — due to surface tension. Surface molecules experience net inward force (fewer neighbours above); work is needed to expand the surface → surface energy.

T = F / L = W / A
T = Surface tension (N·m⁻¹), dimensions [MT⁻²]
F = Force normal to line L on surface
W = Work to increase area by A
Surface acts like a stretched elastic membrane; decreases with temperature.

Cohesive forces — same substance. Adhesive forces — different substances (glue, water on glass). Water wets glass; mercury does not (strong cohesion).

Excess Pressure on Curved Surfaces

Drop / air bubble: P = 2T/r
Single liquid surface (outer for drop, inner for bubble in water).
Soap bubble in air: P = 4T/r
Two surfaces (inner + outer) → twice the excess pressure of a drop.

Example 9.3: r = 1 mm — soap bubble P = 100 Pa; water drop and air bubble in water P ≈ 144 Pa.

Fig 9.17 — Mosquito on Water Surface 2πrT cosθ = mg surface tension supports weight
Fig 9.17 — Surface tension vertical component balances mosquito's weight

Applications: mosquitoes on water (2πrT cos θ balances mg); detergents lower T for cleaning; camphor-under-duck random motion.

9.5 Angle of Contact

The angle between the liquid surface tangent and container wall (measured inside the liquid) is the angle of contact θ.

  • Acute θ → concave meniscus (water in glass).
  • Obtuse θ → convex meniscus (mercury in glass, water in paraffin).

Determined by balance of cohesive (F_c) and adhesive (F_a) forces at the boundary.

Fig 9.23 — Capillary Rise h h = 2T cosθ / rρg
Fig 9.23 — Concave meniscus; liquid rises until hρg = 2T/r

9.6 Capillary Action

Rise or fall of liquid in a narrow tube due to surface tension is capillarity. Water rises in blotting paper, plant stems, and fine glass tubes; mercury is depressed.

h = 2T cos θ / (r ρ g)
h = Capillary rise (m)
T = Surface tension
θ = Angle of contact
r = Radius of capillary tube
ρ = Liquid density
Fine bore → greater rise. θ = 0° (water in clean glass) maximises rise.

Pressure deficit under concave meniscus (2T/R) drives liquid up until hρg = 2T/R with R = r/cos θ.

9.7 Viscosity

Adjacent fluid layers exert tangential drag opposing relative motion — viscosity. Water stirs differently near walls vs centre; glycerin flows slower than water.

F = −η A (dv/dx)
F = Viscous force (N)
η = Coefficient of viscosity (N·s·m⁻²)
A = Layer area
dv/dx = Velocity gradient
Negative sign: opposes motion. 1 poise = 0.1 N·s·m⁻².

Viscosity of liquids decreases with temperature; gases show opposite trend. Wall layer of pipe assumed stationary; velocity maximum at centre (parabolic profile for laminar flow).

9.8 Types of Liquid Flow

9.8.1 Streamline (Laminar) vs Turbulent

Line of flow: path of a fluid particle. Streamline: curve whose tangent gives velocity direction. Streamlines never cross (unique velocity at a point).

  • Laminar: velocity < critical velocity v_c — layers slide over each other smoothly.
  • Turbulent: v > v_c — mixing, zig-zag paths (flood river vs city water pipe).
Fig 9.28 — Equation of Continuity v₁ slow v₂ fast A₁v₁ = A₂v₂
Fig 9.28 — Narrow pipe → faster flow; A₁v₁ = A₂v₂

9.8.2 Equation of Continuity

A₁ v₁ = A₂ v₂
Incompressible fluid, streamline flow.
Mass entering per second = mass leaving.
Narrow section → higher speed.

9.8.3 Critical Velocity and Reynolds Number

v_c = R η / (ρ d)
R = Reynolds number (dimensionless)
R < 1000 → laminar
1000–2000 → unsteady
R > 2000 → turbulent
Also R = ρ v d / η

9.9 Stokes' Law and Terminal Velocity

For a smooth sphere radius r moving at speed v in viscous fluid:

F = 6π η r v
Stokes' law (empirical, K = 6π).
Derived via dimensional analysis: F ∝ η r v.

A sphere falling in viscous liquid reaches terminal velocity when weight = buoyancy + viscous drag:

v₀ = 2r²g(ρ − σ) / (9η)
ρ = Density of sphere
σ = Density of fluid
r = Radius
Applications: parachutes, raindrop size limit.

9.10 Bernoulli's Principle

Where fluid velocity is high, pressure is low; where velocity is low, pressure is high. Governs chimneys, burrows, convertible tops bulging, umbrella lifting in storms.

Flowing fluid has three energy forms: kinetic (½ρv²), gravitational potential (ρgh), and pressure energy (P).

P + ½ρv² + ρgh = constant
Bernoulli's equation (ideal fluid assumptions):
1. Incompressible (constant ρ)
2. Non-viscous (no friction losses)
3. Streamline (steady) flow
Along a tube of flow between two points.
         BERNOULLI APPLICATIONS MAP
         ==========================
    High v  →  Low P  →  Lift / suction
                    |
    +-------+-------+-------+-------+
    |       |       |       |       |
 Venturi  Aerofoil Atomizer Cricket  Efflux
 meter   (plane)  /spray   swing   √(2gH)
    |       |       |       |       |
 Flow     Wing    Paint    Spin    Tank
 rate     lift    gun      curve   hole
Fig 9.32 & 9.37 — Venturi & Aerofoil low P high P → Venturimeter fast air slow air Lift ↑
Fig 9.32/9.37 — Narrow section = low pressure; aerofoil lift from pressure difference

Key Applications

  • Torricelli efflux: v = √(2gH) — speed of water leaving hole at depth H (from Bernoulli, P_atm at surface and jet).
  • Venturimeter: narrow section → higher v → lower P; measures flow rate V ∝ √(ΔP).
  • Aerofoil: crowded streamlines above → lower pressure → lift.
  • Atomizer / spray gun / Bunsen burner / carburetor: fast air → low P → sucks liquid/fuel.
  • Cricket swing: spin makes air speed asymmetric above/below ball → pressure difference → curved path.
  • Pressed hose: constriction increases v, decreases P — jet travels farther.

Example: Tank height 2.5 m → v = √(2×9.8×2.5) = 7 m/s.

Quick Revision

  • Pressure: P = F/A; hydrostatic P = ρgh; absolute = P_atm + ρgh.
  • Archimedes: buoyancy = weight of displaced fluid.
  • Pascal: F₂ = F₁(A₂/A₁) — hydraulic machines.
  • Surface tension: T = F/L; drop P = 2T/r; soap bubble P = 4T/r.
  • Capillary: h = 2T cos θ/(rρg).
  • Viscosity: F = −ηA(dv/dx); Stokes: F = 6πηrv.
  • Continuity: A₁v₁ = A₂v₂; Reynolds number classifies flow.
  • Bernoulli: P + ½ρv² + ρgh = constant; high v → low P.
20 cards · click any card to flip
Pressure
P = Thrust/Area = F/A. SI unit pascal (Pa) = N·m⁻². Effect of force per unit area.
Hydrostatic pressure
P = ρgh at depth h below free surface. Increases linearly with depth — thicker dam walls at base.
Absolute pressure
P_abs = P_atm + ρgh. Pressure at depth includes atmospheric pressure on the free surface.
Atmospheric pressure
P_atm ≈ 1.01×10⁵ Pa. Torricelli barometer: 76 cm Hg column. Guericke hemispheres experiment.
Archimedes' principle
Buoyant force on submerged body = weight of fluid displaced. Explains floating, hot-air balloons, easier lifting in water.
Pascal's law
Pressure applied anywhere in enclosed liquid transmitted undiminished to all parts and walls. Basis of hydraulic devices.
Hydraulic lift
F₂ = F₁(A₂/A₁). Small force on small piston lifts large load on big piston — car jacks, hydraulic brakes.
Surface tension
T = F/L. Force per unit length tangential to liquid surface. T = W/A = surface energy per unit area. Unit N·m⁻¹.
Cohesive vs adhesive
Cohesive: attraction between same molecules. Adhesive: between different substances. Determines wetting and meniscus shape.
Excess pressure — drop
Spherical liquid drop (one surface): P_i − P_o = 2T/r. Air bubble in water: same 2T/r.
Excess pressure — soap bubble
Soap bubble (two surfaces): P = 4T/r — twice that of a drop of same radius.
Angle of contact
Angle between liquid surface tangent and container wall, measured inside liquid. Acute → concave meniscus; obtuse → convex.
Capillary rise
h = 2T cos θ / (r ρ g). Liquid rises in narrow tube when adhesion > cohesion. Mercury depresses (θ > 90°).
Viscosity
Property opposing relative motion between adjacent fluid layers. Honey more viscous than water. F = −ηA(dv/dx).
Coefficient of viscosity η
SI unit N·s·m⁻². 1 poise = 0.1 N·s·m⁻². Dimensions [ML⁻¹T⁻¹]. Decreases with temperature for liquids.
Equation of continuity
A₁v₁ = A₂v₂ for incompressible streamline flow. Narrow tube → higher speed.
Reynolds number
R = ρvd/η. R < 1000 laminar; 1000–2000 unsteady; R > 2000 turbulent. v_c = Rη/(ρd).
Stokes' law
Viscous drag on sphere: F = 6πηrv. Terminal velocity v₀ = 2r²g(ρ−σ)/(9η). Raindrops, parachutes.
Bernoulli's principle
In streamline flow of ideal fluid: high velocity → low pressure; low velocity → high pressure.
Bernoulli's equation
P + ½ρv² + ρgh = constant along a streamline. Sum of pressure, kinetic, and potential energy per unit volume.

Q1. The SI unit of pressure is:

Q2. Hydrostatic pressure at depth h in a liquid of density ρ is:

Q3. According to Archimedes' principle, buoyant force equals:

Q4. Pascal's law states that pressure in an enclosed fluid:

Q5. Excess pressure inside a soap bubble of radius r is:

Q6. Capillary rise h is inversely proportional to:

Q7. Coefficient of viscosity has SI unit:

Q8. For streamline (laminar) flow, Reynolds number R should be:

Q9. According to Bernoulli's principle, where fluid velocity is high:

Q10. Torricelli's law for efflux speed from a tank at depth H is:

P = F / A
P = ρ g h
P = P_atm + ρ g h
P_atm = h ρ_Hg g ≈ 1.01×10⁵ Pa
F_B = ρ_liquid V_displaced g
F₂ = F₁ × (A₂/A₁)
T = F / L = W / A
P_excess = 2T / r
P_excess = 4T / r
h = 2T cos θ / (r ρ g)
F = −η A (dv/dx)
A₁ v₁ = A₂ v₂
R = ρ v d / η
v_c = R η / (ρ d)
F = 6π η r v
v₀ = 2r²g(ρ − σ) / (9η)
P + ½ρv² + ρgh = constant
v = √(2gH)

1. Formulas & Definitions

Full Ch 9 study guide — pressure, buoyancy, Pascal, surface tension, viscosity, continuity, and Bernoulli.

P = F / A

Definition: Pressure is normal thrust (force) per unit area.

Derivation

P = F/A from definition; fluids exert forces normal to surfaces only.

Variables

P (Pa = N·m⁻²) · F (N) · A (m²)

Why it works

Same force hurts more on a pin point than a blunt rod — area matters.

Historical context

SI unit pascal named after Blaise Pascal (17th century fluid studies).

Deep understanding

Scalar quantity. Fluids at rest cannot sustain shear — only normal pressure.

2. Diagrams & Visuals

P = F / A F↓ smaller A → larger P

Color-coded visual · step-by-step breakdown below

  1. Identify normal force F in N
  2. Area A in m² (perpendicular to F)
  3. P = F/A
  4. State unit: pascal (Pa)

3. Solved Examples

Basic

Q: 100 N on 0.5 m².

Solution: P=100/0.5

Answer: 200 Pa

Intermediate

Q: Thrust 490 N, area 0.01 m².

Solution: P=49000

Answer: 49 kPa

Advanced

Q: Why sharp knife cuts better?

Solution: Smaller A → higher P

Answer: Same F, less area

Exam

Q: SI unit of pressure?

Solution: Pascal (Pa)

Answer: N·m⁻²

P = ρ g h

Definition: Hydrostatic gauge pressure at depth h in a liquid of density ρ.

Derivation

Equilibrium of liquid column height h, area A: P = (ρAhg)/A = ρgh.

Variables

P (Pa) · ρ (kg·m⁻³) · g ≈ 9.8 m/s² · h (m)

Why it works

Pressure grows linearly with depth — dam walls must be thicker at the base.

Historical context

Pascal and Torricelli extended hydrostatic ideas to engineering and barometry.

Deep understanding

Independent of container shape (Fig 9.5). Gauge pressure — add P_atm for absolute.

2. Diagrams & Visuals

h P = ρgh

Color-coded visual · step-by-step breakdown below

  1. ρ of liquid in kg/m³
  2. Depth h below free surface
  3. P = ρgh
  4. Add P_atm if absolute pressure needed

3. Solved Examples

Basic

Q: Water ρ=1000, h=2 m.

Solution: P=1000×9.8×2

Answer: 19.6 kPa

Intermediate

Q: Ex 9.1: h=100 m, ρ=10³.

Solution: P=9.8×10⁵ Pa

Answer: ≈ 10⁶ Pa

Advanced

Q: Double depth — pressure?

Solution: P ∝ h

Answer: 2× pressure

Exam

Q: Dam wall thickness at base?

Solution: P ∝ h → thicker base

Answer: Fig 9.1

P = P_atm + ρ g h

Definition: Absolute pressure at depth h below liquid surface open to atmosphere.

Derivation

Surface at atmospheric pressure; add gauge increment ρgh.

Variables

P_atm ≈ 1.01×10⁵ Pa · ρ · g · h

Why it works

Divers and submarines feel total pressure including air above the water.

Historical context

Torricelli's barometer linked atmospheric pressure to mercury column height.

Deep understanding

At depth h in open tank, absolute P = P_atm + ρgh. Closed systems may differ.

2. Diagrams & Visuals

P = P_atm + ρgh absolute = atmospheric + gauge

Color-coded visual · step-by-step breakdown below

  1. Find gauge P = ρgh
  2. Add P_atm (≈10⁵ Pa unless given)
  3. Report absolute pressure

3. Solved Examples

Basic

Q: ρgh=20 kPa at surface open to air.

Solution: P=101+20

Answer: 121 kPa

Intermediate

Q: Lake 10 m deep surface P_atm.

Solution: ρgh=98 kPa; total≈199 kPa

Answer: ≈ 2×10⁵ Pa

Advanced

Q: Gauge vs absolute?

Solution: Gauge excludes P_atm

Answer: Manometer reads gauge often

Exam

Q: Open surface at depth h?

Solution: P = P_atm + ρgh

Answer: Sec 9.1

P_atm = h ρ_Hg g ≈ 1.01×10⁵ Pa

Definition: Standard atmospheric pressure from mercury barometer column.

Derivation

Balance: ρ_Hg g h = P_atm with h = 0.76 m.

Variables

h = 0.76 m · ρ_Hg = 13600 kg·m⁻³ · g = 9.8

Why it works

Defines normal air pressure — weather 'low pressure' means below this.

Historical context

Evangelista Torricelli (1643); von Guericke's hemispheres demonstrated its magnitude.

Deep understanding

Also ≈ 76 cm Hg or 1 bar. Decreases with altitude.

2. Diagrams & Visuals

76 cm Hg ≈ 10⁵ Pa

Color-coded visual · step-by-step breakdown below

  1. h in metres of Hg
  2. ρ_Hg = 13600 kg/m³
  3. P_atm = h ρ_Hg g

3. Solved Examples

Basic

Q: h=0.76 m standard.

Solution: P≈1.01×10⁵

Answer: 1 atm

Intermediate

Q: Convert to kPa.

Solution: ÷1000

Answer: 101 kPa

Advanced

Q: Why mercury not water?

Solution: ρ much larger → shorter column

Answer: ~10 m water needed

Exam

Q: Torricelli barometer fluid?

Solution: Mercury

Answer: Fig 9.6

F_B = ρ_liquid V_displaced g

Definition: Archimedes' principle — buoyant force equals weight of displaced fluid.

Derivation

Equilibrium of submerged fluid parcel; upward force balances weight of displaced volume.

Variables

F_B (N) · ρ_liquid · V_displaced (m³) · g

Why it works

Objects feel lighter in water because fluid pushes up by this amount.

Historical context

Archimedes (3rd century BCE) — 'Eureka' and crown density legend.

Deep understanding

Float: F_B = W_object. Sink: W > F_B. Hot-air balloon: buoyancy in air.

2. Diagrams & Visuals

F_B = W_displaced

Color-coded visual · step-by-step breakdown below

  1. Find volume of fluid displaced V
  2. ρ of surrounding fluid
  3. F_B = ρ V g (upward)
  4. Compare with object weight

3. Solved Examples

Basic

Q: 2 m³ water displaced.

Solution: F_B=1000×2×9.8

Answer: 19.6 kN up

Intermediate

Q: 10 kg block, volume 0.002 m³ in water.

Solution: F_B=19.6 N; W=98 N

Answer: Sinks

Advanced

Q: Ship floats — condition?

Solution: F_B = W at equilibrium

Answer: Displaces own weight

Exam

Q: Archimedes states?

Solution: Buoyancy = weight of displaced fluid

Answer: Sec 9.2

F₂ = F₁ × (A₂/A₁)

Definition: Pascal's law — force multiplication in hydraulic machines.

Derivation

Pressure transmitted equally: P = F₁/A₁ = F₂/A₂ → F₂ = F₁(A₂/A₁).

Variables

F₁, F₂ (N) · A₁, A₂ (m²)

Why it works

Small pedal force lifts a car — area ratio is the mechanical advantage.

Historical context

Blaise Pascal (1653); hydraulic brakes, jacks, and presses use this daily.

Deep understanding

Liquid incompressible and enclosed. Work same both sides: F₁d₁ = F₂d₂.

2. Diagrams & Visuals

load F₂ = F₁(A₂/A₁)

Color-coded visual · step-by-step breakdown below

  1. Same pressure: F₁/A₁ = F₂/A₂
  2. Rearrange for desired force
  3. Area ratio gives multiplication

3. Solved Examples

Basic

Q: F₁=10 N, A₁=0.01, A₂=0.5 m².

Solution: F₂=10×50

Answer: 500 N

Intermediate

Q: Intext: boy 25 kg, A₁=0.05, elephant 5000 kg, A₂=10.

Solution: Ratio 200; 25×200=5000

Answer: Balances!

Advanced

Q: Brake pedal design?

Solution: Small A₁, large A₂ at wheels

Answer: Force multiplication

Exam

Q: PYQ hydraulic: F₂ formula?

Solution: F₁×A₂/A₁

Answer: Pascal's law

T = F / L = W / A

Definition: Surface tension — force per unit length along a liquid surface.

Derivation

Work W to stretch surface area A gives T = W/A; also T = F/L on a line.

Variables

T (N·m⁻¹) · F (N) · L (m) · W (J) · A (m²)

Why it works

Surface behaves like stretched elastic skin — drops are spherical, mosquitoes walk on water.

Historical context

Surface energy concept links molecular cohesion to macroscopic T.

Deep understanding

T decreases with temperature. Cohesive vs adhesive forces explain wetting.

2. Diagrams & Visuals

F T = F/L

Color-coded visual · step-by-step breakdown below

  1. Measure force F normal to length L
  2. T = F/L
  3. Or from work: T = W/A

3. Solved Examples

Basic

Q: F=0.07 N across 0.05 m.

Solution: T=1.4

Answer: 1.4 N/m

Intermediate

Q: Why soap bubbles form?

Solution: Soap lowers T

Answer: Easier to stretch surface

Advanced

Q: Dimensions of T?

Solution: [MT⁻²]

Answer: Same as force/length

Exam

Q: Water vs mercury meniscus?

Solution: Cohesion/adhesion balance

Answer: Sec 9.4–9.5

P_excess = 2T / r

Definition: Excess pressure inside a liquid drop or air bubble in water (one surface).

Derivation

Laplace law for single curved surface: ΔP = 2T/r.

Variables

P_excess (Pa) · T (N·m⁻¹) · r (m)

Why it works

Small drops have higher internal pressure — explains droplet stability.

Historical context

Laplace pressure law connects surface tension to curvature.

Deep understanding

Outer surface for drop; inner surface for bubble in liquid. One interface only.

2. Diagrams & Visuals

P = 2T/r

Color-coded visual · step-by-step breakdown below

  1. Radius r of drop/bubble
  2. Surface tension T
  3. P_excess = 2T/r

3. Solved Examples

Basic

Q: T=0.07, r=1 mm.

Solution: P=0.14/0.001

Answer: 140 Pa

Intermediate

Q: Ex 9.3: r=1 mm air bubble in water.

Solution: P≈144 Pa

Answer: Compare soap bubble

Advanced

Q: Smaller r — pressure?

Solution: P ∝ 1/r

Answer: Higher for tiny drops

Exam

Q: Drop vs soap bubble factor?

Solution: 1 surface → 2T/r; 2 surfaces → 4T/r

Answer: Next formula

P_excess = 4T / r

Definition: Excess pressure inside a soap bubble in air (two surfaces).

Derivation

Inner and outer surfaces each contribute 2T/r → total 4T/r.

Variables

P_excess (Pa) · T · r

Why it works

Soap film has two liquid-air interfaces — double the drop pressure.

Historical context

Classic lecture demonstration comparing water drop, bubble, and soap bubble.

Deep understanding

Ex 9.3: r=1 mm → soap bubble P=100 Pa; water drop ≈144 Pa (different T values).

2. Diagrams & Visuals

4T/r

Color-coded visual · step-by-step breakdown below

  1. Two surfaces for soap film
  2. Each gives 2T/r
  3. Total P = 4T/r

3. Solved Examples

Basic

Q: T=0.025, r=1 mm soap.

Solution: P=4×0.025/0.001

Answer: 100 Pa

Intermediate

Q: Same r, water drop T=0.072.

Solution: 2T/r=144 Pa

Answer: One surface

Advanced

Q: Why two surfaces?

Solution: Film has inside + outside air contact

Answer: Bubble in air only

Exam

Q: Ex 9.3 values?

Solution: Soap 100 Pa; drop/bubble ~144 Pa

Answer: Memorise pattern

h = 2T cos θ / (r ρ g)

Definition: Capillary rise (or depression) in a tube of radius r.

Derivation

Surface tension upward component 2πrT cosθ balances weight of column πr²hρg.

Variables

h (m) · T · θ = contact angle · r · ρ · g

Why it works

Water rises in thin tubes and blotting paper — plants pull water via capillarity.

Historical context

Jurin and Young studied capillary phenomena in 18th–19th centuries.

Deep understanding

θ acute → rise (water/glass); θ obtuse → depression (mercury). Finer bore → higher h.

2. Diagrams & Visuals

h = 2T cosθ/rρg

Color-coded visual · step-by-step breakdown below

  1. T, θ, r, ρ of liquid
  2. h = 2T cosθ/(rρg)
  3. θ=0° maximises rise for water

3. Solved Examples

Basic

Q: T=0.07, θ=0, r=0.5 mm, ρ=1000.

Solution: h=0.14/(0.0005×9800)

Answer: ≈ 2.9 cm

Intermediate

Q: Halve r — h becomes?

Solution: h ∝ 1/r

Answer: 2× rise

Advanced

Q: Mercury in glass?

Solution: θ obtuse → cosθ negative

Answer: Depression not rise

Exam

Q: Fine bore effect?

Solution: h larger for smaller r

Answer: Capillary action

F = −η A (dv/dx)

Definition: Viscous drag between fluid layers (Newton's law of viscosity).

Derivation

Shear stress τ = η(dv/dx); force F = τA.

Variables

F (N) · η (N·s·m⁻²) · A (m²) · dv/dx = velocity gradient

Why it works

Honey flows slowly — strong internal friction between layers.

Historical context

Sir Isaac Newton proposed viscosity law for fluids; 1 poise = 0.1 Pa·s.

Deep understanding

Negative sign: opposes relative motion. η of liquids ↓ with temperature.

2. Diagrams & Visuals

layers slide

Color-coded visual · step-by-step breakdown below

  1. Find velocity gradient dv/dx
  2. Area A of layer
  3. F = ηA(dv/dx) opposing motion

3. Solved Examples

Basic

Q: η=0.1, A=0.01, dv/dx=2.

Solution: F=0.002 N

Answer: 0.002 N

Intermediate

Q: Wall layer of pipe velocity?

Solution: v=0 at wall

Answer: Max at centre

Advanced

Q: Gas vs liquid η vs T?

Solution: Liquid η↓; gas η↑ with T

Answer: NIOS contrast

Exam

Q: Unit of η?

Solution: N·s·m⁻² (Pa·s)

Answer: 1 poise=0.1 Pa·s

A₁ v₁ = A₂ v₂

Definition: Equation of continuity for incompressible streamline flow.

Derivation

Mass flow rate ρA₁v₁ = ρA₂v₂ with constant ρ → A₁v₁ = A₂v₂.

Variables

A (m²) · v (m/s) · subscripts 1, 2 at two sections

Why it works

Garden hose narrows → water speeds up — same volume per second must pass.

Historical context

Continuity is conservation of mass applied to fluid flow (Fig 9.28).

Deep understanding

Streamlines never cross. Narrow tube → higher speed. Basis for Venturi meter.

2. Diagrams & Visuals

v₁ v₂ fast A₁v₁=A₂v₂

Color-coded visual · step-by-step breakdown below

  1. Identify two cross-sections
  2. Measure areas A₁, A₂
  3. A₁v₁ = A₂v₂
  4. Solve for unknown speed

3. Solved Examples

Basic

Q: A₁=0.04, v₁=2, A₂=0.01.

Solution: v₂=0.08/0.01

Answer: v₂ = 8 m/s

Intermediate

Q: Pipe doubles in diameter?

Solution: A ∝ d² → 4× area

Answer: v quarters

Advanced

Q: Compressible gas at high speed?

Solution: ρ not constant

Answer: Continuity modifies

Exam

Q: Fig 9.28 principle?

Solution: Narrow → fast

Answer: Mass conserved

R = ρ v d / η

Definition: Reynolds number — dimensionless ratio for flow type.

Derivation

R = (inertial forces)/(viscous forces) ∝ ρvd/η.

Variables

R (no unit) · ρ · v · d (characteristic size) · η

Why it works

Predicts laminar vs turbulent flow in pipes and around objects.

Historical context

Osborne Reynolds (1883) demonstrated transition in pipe flow.

Deep understanding

R<1000 laminar; 1000–2000 unsteady; R>2000 turbulent. Also v_c = Rη/(ρd).

2. Diagrams & Visuals

R = ρvd/η low R → smooth laminar

Color-coded visual · step-by-step breakdown below

  1. ρ, v, d (pipe diameter)
  2. η of fluid
  3. R = ρvd/η
  4. Classify flow regime

3. Solved Examples

Basic

Q: ρ=1000, v=0.1, d=0.05, η=0.001.

Solution: R=5

Answer: Laminar

Intermediate

Q: Double v — R becomes?

Solution: R ∝ v

Answer: 2× R

Advanced

Q: Turbulent river vs calm pipe?

Solution: High v, large d → high R

Answer: Turbulent flood

Exam

Q: R>2000 means?

Solution: Turbulent flow

Answer: Sec 9.8.3

v_c = R η / (ρ d)

Definition: Critical velocity marking onset of turbulent flow.

Derivation

From Reynolds definition with critical R (≈1000–2000 depending on context).

Variables

v_c (m/s) · R (critical Reynolds) · η · ρ · d

Why it works

Engineers keep pipe flow below v_c to reduce noise and energy loss.

Historical context

Paired with Reynolds number in NIOS Sec 9.8.3.

Deep understanding

Larger d or lower η → lower v_c threshold in formula rearrangement.

2. Diagrams & Visuals

v_c = Rη/(ρd)

Color-coded visual · step-by-step breakdown below

  1. Choose critical R (often given)
  2. η, ρ, d of system
  3. v_c = Rη/(ρd)

3. Solved Examples

Basic

Q: R=1000, η=0.001, ρ=1000, d=0.1.

Solution: v_c=0.01

Answer: 0.01 m/s

Intermediate

Q: Relation to R=ρvd/η?

Solution: Same R at v=v_c

Answer: Equivalent forms

Advanced

Q: Laminar condition?

Solution: v < v_c

Answer: Smooth layers

Exam

Q: Turbulent when?

Solution: v > v_c

Answer: Flood vs city pipe

F = 6π η r v

Definition: Stokes' law — viscous drag on smooth sphere radius r at speed v.

Derivation

Dimensional analysis: F ∝ ηrv; coefficient 6π from full theory.

Variables

F (N) · η · r (m) · v (m/s)

Why it works

Explains slow fall of small raindrops and sedimentation in viscous fluids.

Historical context

George Gabriel Stokes (1851); used in Millikan oil-drop experiment.

Deep understanding

Valid for low Reynolds number (laminar creep flow around sphere).

2. Diagrams & Visuals

v F_drag

Color-coded visual · step-by-step breakdown below

  1. Sphere radius r
  2. Speed v relative to fluid
  3. η of medium
  4. F = 6πηrv

3. Solved Examples

Basic

Q: η=0.1, r=1 mm, v=0.01 m/s.

Solution: F=6π×0.1×0.001×0.01

Answer: ≈ 1.9×10⁻⁵ N

Intermediate

Q: Double r — drag becomes?

Solution: F ∝ r

Answer: 2× drag

Advanced

Q: Double v — drag?

Solution: F ∝ v

Answer: 2× drag

Exam

Q: Stokes coefficient?

Solution:

Answer: Sec 9.9

v₀ = 2r²g(ρ − σ) / (9η)

Definition: Terminal velocity of sphere falling in viscous fluid.

Derivation

At terminal speed: weight = buoyancy + Stokes drag → solve for v₀.

Variables

v₀ (m/s) · r · g · ρ = sphere density · σ = fluid density · η

Why it works

Raindrops don't accelerate forever — drag balances net weight.

Historical context

Parachutes increase drag area to reduce terminal speed safely.

Deep understanding

Larger r → much larger v₀ (r² dependence). Applies to small smooth spheres.

2. Diagrams & Visuals

mg v₀ constant

Color-coded visual · step-by-step breakdown below

  1. ρ and σ densities
  2. Radius r
  3. η of fluid
  4. v₀ = 2r²g(ρ−σ)/(9η)

3. Solved Examples

Basic

Q: ρ=8000, σ=1000, r=0.001, η=0.1.

Solution: v₀=2×10⁻⁶×9.8×7000/0.9

Answer: ≈ 0.15 m/s

Intermediate

Q: Net driving density (ρ−σ)?

Solution: Effective weight per volume

Answer: In numerator

Advanced

Q: Parachute reduces v₀ how?

Solution: Increases effective drag area

Answer: Not Stokes regime

Exam

Q: When is v₀ reached?

Solution: a=0; forces balance

Answer: Sec 9.9

P + ½ρv² + ρgh = constant

Definition: Bernoulli's equation along a streamline (ideal fluid).

Derivation

Energy conservation: pressure energy + kinetic + potential per unit volume.

Variables

P (Pa) · ρ · v (m/s) · g · h (m)

Why it works

Fast flow → low pressure: airplane lift, cricket swing, atomizers, chimneys.

Historical context

Daniel Bernoulli (1738) Hydrodynamica; Euler gave modern form.

Deep understanding

Assumptions: incompressible, non-viscous, steady streamline flow. High v → low P.

2. Diagrams & Visuals

low P, high v high P P + ½ρv² + ρgh = const

Color-coded visual · step-by-step breakdown below

  1. Pick two points on same streamline
  2. Write P, v, h at each
  3. Set P₁+½ρv₁²+ρgh₁ = P₂+½ρv₂²+ρgh₂
  4. Solve unknown

3. Solved Examples

Basic

Q: Horizontal pipe narrows: P₂?

Solution: h same; v up → P down

Answer: Bernoulli trade-off

Intermediate

Q: Venturi: narrow section pressure?

Solution: Lower than wide part

Answer: Flow meter principle

Advanced

Q: Viscous real pipe?

Solution: Energy lost to heat

Answer: Bernoulli approximate

Exam

Q: High speed → pressure?

Solution: Lower P

Answer: Core Bernoulli idea

v = √(2gH)

Definition: Torricelli efflux speed — liquid leaving hole at depth H.

Derivation

Bernoulli between surface (v≈0, P=P_atm) and jet (P=P_atm, h=0): ½ρv²=ρgH.

Variables

v (m/s) · g · H = depth of hole below surface (m)

Why it works

Water jet from tank hole — speed depends only on depth, not hole size (ideal).

Historical context

Torricelli's theorem (1643) — student of Galileo.

Deep understanding

Ex: H=2.5 m → v=√(49)=7 m/s. Same as free fall from height H.

2. Diagrams & Visuals

H v=√(2gH)

Color-coded visual · step-by-step breakdown below

  1. Depth H below free surface
  2. v = √(2gH)
  3. Independent of hole area (ideal)

3. Solved Examples

Basic

Q: H=2 m.

Solution: v=√(19.6)

Answer: ≈ 4.43 m/s

Intermediate

Q: Ex: H=2.5 m.

Solution: v=√(49)

Answer: 7 m/s

Advanced

Q: Double H — speed?

Solution: v ∝ √H

Answer: √2 × speed

Exam

Q: Efflux from tank hole?

Solution: v = √(2gH)

Answer: Bernoulli application

5. Special Features & Extras

Complete study guide for Properties of Fluids.

Exam Tips & Tricks

  • Hydrostatic: P = ρgh for gauge; add P_atm for absolute.
  • Pascal: F₂ = F₁(A₂/A₁) — area ratio is force multiplier (PYQ favourite).
  • Surface tension: drop 2T/r; soap bubble 4T/r (two surfaces).
  • Capillary: h ∝ 1/r — finer tube rises higher.
  • Bernoulli: high v → low P — lift, swing, atomizer.
  • Continuity + Bernoulli together solve pipe and Venturi problems.

Common Student Mistakes

  • Confusing gauge and absolute pressure
  • Using 2T/r for soap bubble (needs 4T/r)
  • Forgetting cos θ in capillary formula
  • Applying Bernoulli when viscosity losses matter
  • Mixing up ρ (sphere) and σ (fluid) in terminal velocity
  • Assuming larger hole → faster efflux (v = √(2gH) only)

Memory Aids & Mnemonics

Pressure ladder: F/A → ρgh → P_atm+ρgh
Bubble rule: "One skin 2T, two skins 4T" over r
Bernoulli: "Fast = thin pressure" — velocity up, pressure down
Stokes terminal: "2 r squared g delta-rho over 9 eta"

Which Formula When?

  • Force on area? → P = F/A
  • Depth in liquid? → P = ρgh
  • Floating/sinking? → Archimedes F_B = ρVg
  • Hydraulic jack? → F₂ = F₁(A₂/A₁)
  • Drop/bubble pressure? → 2T/r or 4T/r
  • Rise in tube? → h = 2T cosθ/(rρg)
  • Pipe narrows? → A₁v₁ = A₂v₂ then Bernoulli
  • Tank hole speed? → v = √(2gH)

QUICK REFERENCE — Ch 9 Properties of Fluids

P = F / AP = ρ g hP = P_atm + ρ g hP_atm = h ρ_Hg g ≈ 1.01×10⁵ PaF_B = ρ_liquid V_displaced gF₂ = F₁ × (A₂/A₁)T = F / L = W / AP_excess = 2T / rP_excess = 4T / rh = 2T cos θ / (r ρ g)F = −η A (dv/dx)A₁ v₁ = A₂ v₂R = ρ v d / ηv_c = R η / (ρ d)F = 6π η r vv₀ = 2r²g(ρ − σ) / (9η)P + ½ρv² + ρgh = constantv = √(2gH)

Units: Pa = N·m⁻² · T in N·m⁻¹ · η in Pa·s · R (Reynolds) dimensionless

Tip: Draw the diagram (dam, hydraulic lift, capillary, Venturi) before picking the formula.

PYQ — Previous Year Questions

Extracted from NIOS Physics (312) board exam papers in your PDF. Chapter L9 — Properties of Fluids only. Use Model Answer for marking points; Explanation for concept clarity.

Chapter 9 — Properties of Fluids (L9)

20 questions · Section A (MCQ & objective) + Section B (short/long) · Sources: 312/TUS/104A, 312/MAY/204A–C, 68/ESS/1-312-A, Marking Scheme

Section A — Multiple Choice (1 mark)

PYQ1. Pressure due to a liquid column does not depend on — (A) its density   (B) its viscosity   (C) its height   (D) acceleration due to gravity

1 mark · Section A Q1 · 312/TUS/104A

Model Answer

Answer: (B) its viscosity

Hydrostatic pressure P = hρg depends on height, density and g — not on viscosity.

Explanation

Viscosity matters for flowing fluids (drag, Poiseuille flow). In a static column at rest, pressure at depth h is P = hρg (L9 §9.1).

PYQ2. Two solid spheres of the same metal (masses M and 8M) fall together in a viscous liquid. If terminal velocities are v and nv, then n is — (A) 2   (B) 4   (C) 8   (D) 16

1 mark · Section A Q12 · 312/TUS/104A

Model Answer

Answer: (B) 4

Stokes: v_t ∝ r². Same metal ⇒ m ∝ r³ ⇒ r ∝ m^(1/3). Hence v_t ∝ m^(2/3). For 8M: n = 8^(2/3) = 4.

Explanation

v₀ = 2r²g(ρ−σ)/(9η). Radius doubles when mass is 8× (volume ×8). Speed scales as r² → factor 4.

PYQ3. Two spherical drops of the same liquid have volumes in ratio 1 : 8. The ratio of excess pressures inside them is — (A) 8 : 1   (B) 2 : 1   (C) 1 : 1   (D) 1 : 2

1 mark · Section A Q12 (OR) · 312/TUS/104A

Model Answer

Answer: (B) 2 : 1

V ∝ r³ ⇒ volume ratio 1:8 gives r ratio 1:2. ΔP = 2T/r ⇒ smaller drop (r₁) has higher pressure: P₁/P₂ = r₂/r₁ = 2 : 1.

Explanation

Liquid drop (one surface): ΔP = 2T/r. Smaller radius ⇒ larger excess pressure. r₂/r₁ = 2 ⇒ P₁/P₂ = 2.

PYQ4. Capillarity is due to — (A) Cohesion only   (B) Adhesion only   (C) Cohesion and adhesion both   (D) Neither

1 mark · Section A Q4 · Marking Scheme

Model Answer

Answer: (C) Cohesion and adhesion both

Explanation

Cohesion (liquid–liquid) and adhesion (liquid–wall) together fix the contact angle and capillary rise/fall: h = 2T cos θ/(rρg).

PYQ5. For non-viscous incompressible steady flow, if pipe area is halved, velocity becomes — (A) 4×   (B) 3×   (C) 2×   (D) unchanged

1 mark · Section A Q4 (OR) · Marking Scheme

Model Answer

Answer: (C) Doubled

Equation of continuity: A₁v₁ = A₂v₂. If A₂ = A₁/2, then v₂ = 2v₁.

Explanation

Mass conservation for incompressible flow. Narrower tube ⇒ faster flow — basis of Bernoulli applications (L9 §9.10).

PYQ6. Excess pressure inside two soap bubbles of diameters in ratio 4 : 1 is — (A) 1 : 4   (B) 2 : 1   (C) 1 : 2   (D) 4 : 1

1 mark · Section A Q5 · Marking Scheme

Model Answer

Answer: (A) 1 : 4

Soap bubble: ΔP = 4T/r. Pressure ∝ 1/r. Diameter ratio 4:1 ⇒ radius ratio 4:1 ⇒ pressure ratio 1:4.

Explanation

Bubble has two surfaces → P = 4T/r (L9). Larger bubble has smaller excess pressure.

PYQ7. Match device with principle (any two): (a) Barometer — ?   (b) Hydraulic brake — ?   Options: (i) Upthrust = weight of displaced fluid   (ii) P = hdg   (iii) F₁/A₁ = F₂/A₂   (iv) F = 6πηrv

2 marks (1×2) · Section A Q26 · 312/TUS/104A

Model Answer

(a) Barometer ↔ (ii) P = hdg

(b) Hydraulic brake ↔ (iii) F₁/A₁ = F₂/A₂ (Pascal's law)

(i) ↔ Archimedes  ·  (iv) ↔ Stokes' law

Explanation

Barometer measures atmospheric pressure from mercury column height. Hydraulic systems transmit pressure equally — small piston force amplified on large piston.

PYQ8. True or False (any two): (a) Kerosene rises in a lantern wick due to surface tension   (b) Raindrop hits ground at terminal velocity   (c) Time to reach terminal velocity in air depends on air density   (d) Excess pressure in soap bubble of radius r is 2T/r

2 marks (1×2) · Section A Q21 · 312/TUS/104A

Model Answer

  • (a) True — capillary action driven by surface tension
  • (b) True — viscous drag balances weight at terminal speed
  • (c) True — drag depends on fluid density
  • (d) False — soap bubble has two surfaces: ΔP = 4T/r

Explanation

2T/r is for a liquid drop with one free surface. A bubble in air has inner and outer surfaces → factor of 2 extra.

PYQ9. Passage — Bernoulli spray gun: In P + ½ρv² + ρgh = const, for unit volume A, B, C are — ?   If piston speed 5 mm/s (r=20 mm), nozzle air speed (r=1 mm) is — ?

2 marks (1×2) · Section A Q19 · Marking Scheme: (i)(c), (ii)(c) → 2 m/s

Model Answer

(i) (c) pressure energy, kinetic energy, potential energy (per unit volume: P, ½ρv², ρgh)

(ii) (c) 2 m·s⁻¹

Continuity: π(20)²×5 = π(1)²×v₂ ⇒ v₂ = 2000 mm/s = 2 m/s

Explanation

Bernoulli + continuity explain spray guns: fast air at nozzle lowers pressure, sucking liquid up the tube (L9 application).

PYQ10. Match: (i) SI unit of coefficient of viscosity — ?   (ii) CGS unit — ?   Options: P. N·s·m⁻²   Q. poise   R. N·m⁻²

2 marks (1×2) · Section A Q28 · Marking Scheme

Model Answer

(i) ↔ P. N·s·m⁻² (pascal-second)

(ii) ↔ Q. poise   (1 poise = 0.1 N·s·m⁻²)

Explanation

From F = −ηA(dv/dx). SI unit of η is N·s·m⁻². CGS uses poise (dyne·s·cm⁻²).

PYQ11. What is Reynolds number? How does it help decide the nature of flow?

2 marks · Section B Q32 · 312/MAY/204A/B/C

Model Answer

Reynolds number: R = ρvd/η — dimensionless ratio of inertial to viscous forces in fluid flow.

Significance: R < 1000 → laminar (streamline); 1000–2000 → transition; R > 2000 → turbulent. Predicts whether flow stays orderly or becomes chaotic.

Explanation

Critical velocity v_c = Rη/(ρd). Same as L9 §9.8.3 — used in pipe design, aircraft, blood flow.

PYQ12. What is terminal velocity? Write the expression for a sphere of radius r and density ρ falling in a fluid of viscosity η and density σ.

2 marks · Section B Q32 (OR) · 312/MAY/204A/B/C

Model Answer

Terminal velocity: Constant maximum speed when weight equals viscous drag (net force zero).

Expression: v₀ = 2r²g(ρ − σ) / (9η)

Set weight = Stokes drag: (4/3)πr³ρg = 6πηrv₀.

Explanation

Valid for small spheres in viscous fluid at low R. Raindrops, Millikan oil-drop experiment use same idea.

PYQ13. What is Reynolds number? What is its significance? (Raynold's number)

2 marks · Section B Q29 · 68/ESS/1-312-A

Model Answer

Same as PYQ11: R = ρvd/η. Low R → viscous forces dominate (laminar); high R → inertia dominates (turbulent). Engineers use it to avoid turbulent losses or ensure mixing.

Explanation

Alternate spelling "Raynold" in paper — same dimensionless number named after Osborne Reynolds.

PYQ14. Give in brief the principle of working of a parachute.

2 marks · Section B Q32 · 68/ESS/1-312-A

Model Answer

Large canopy increases cross-sectional area → air resistance (viscous + pressure drag) increases sharply. When drag = weight, acceleration becomes zero and descent continues at safe terminal velocity.

Explanation

Fluid drag on bluff bodies depends on area and speed. Parachute trades fast fall for survivable terminal speed — viscosity/air resistance application.

PYQ15. Water flows in a horizontal pipe of non-uniform cross-section. At v = 0.2 m·s⁻¹, pressure = 20 mm of Hg. Find pressure where v = 1.5 m·s⁻¹. (ρ_water = 10³ kg·m⁻³)

3 marks · Section B Q41 · 312/MAY/204A/B/C

Model Answer

Bernoulli (horizontal): P₁ + ½ρv₁² = P₂ + ½ρv₂²

P₁ − P₂ = ½ρ(v₂² − v₁²) = 500 × (2.25 − 0.04) = 1105 Pa

P₁ = 20 mm Hg ≈ 2666 Pa ⇒ P₂ ≈ 1561 Pa ≈ 11.7 mm Hg

Explanation

Faster flow → lower pressure (Bernoulli). Use 1 mm Hg ≈ 133 Pa. Assumes ideal fluid, no height change.

PYQ16. Calculate capillary rise of liquid (ρ = 1000 kg·m⁻³) in tube l = 0.05 m, r = 0.2×10⁻³ m. (T = 7.27×10⁻² N·m⁻¹, g = 10 m·s⁻², θ ≈ 0°)

3 marks · Section B Q41 (OR) · 312/MAY/204A/B/C

Model Answer

h = 2T cos θ / (rρg) = 2 × 7.27×10⁻² × 1 / (0.2×10⁻³ × 1000 × 10)

= 0.1454 / 2 = 0.0727 m ≈ 7.3 cm (< 5 cm tube length — rise is physically limited by tube length in real setup).

Explanation

Jurin's law. Narrower tube (smaller r) gives greater rise — explains water creeping up wick/paper.

PYQ17. A 50 kg body stands on the small piston (A = 0.1 m²) of a hydraulic lift. Large piston A = 10 m². Find the weight of the car that can be lifted.

2 marks · Section B Q37 · 68/ESS/1-312-A

Model Answer

Pascal: F₁/A₁ = F₂/A₂

F₁ = mg = 500 N

F₂ = F₁ × A₂/A₁ = 500 × 10/0.1 = 50 000 N

Mass lifted = 50 000/10 = 5000 kg (5 tonne)

Explanation

Pressure transmitted undiminished through fluid. Area ratio 100 ⇒ force multiplied by 100 — hydraulic jack/lift principle (L9 §9.3).

PYQ18. Excess pressure inside a soap bubble of radius 4 cm. (T = 25×10⁻³ N·m⁻¹)

2 marks · Section B Q37 (OR) · 68/ESS/1-312-A

Model Answer

ΔP = 4T/r = 4 × 25×10⁻³ / 0.04 = 2.5 Pa

Explanation

Soap film has two surfaces (inner + outer) → twice the drop formula 2T/r. Excess pressure makes bubble slightly higher pressure than atmosphere.

PYQ19. Using Bernoulli's theorem, explain how a spray gun sucks liquid from a container when air is pushed through a narrow nozzle (piston r = 20 mm, nozzle r = 1 mm).

3 marks · Section A Q19 (passage) · Marking Scheme

Model Answer

Fast air at narrow nozzle (v ≈ 2 m·s⁻¹ by continuity) ⇒ low pressure (Bernoulli). Pressure at liquid surface = atmospheric; pressure in tube at nozzle < atmospheric ⇒ liquid is pushed up the tube and atomised in the fast air stream.

Explanation

P + ½ρv² + ρgh = constant. High v at throat ⇒ reduced P. Same principle as perfume sprayers and carburettors.

PYQ20. State Pascal's law. A hydraulic lift has pistons 0.1 m² and 10 m². If 500 N is applied on the small piston, what force is available on the large piston?

3 marks · Section B Q37 · 68/ESS/1-312-A (Pascal application)

Model Answer

Pascal's law: Pressure applied to enclosed fluid is transmitted undiminished in all directions.

F₂ = F₁ × A₂/A₁ = 500 × 10/0.1 = 50 000 N

Explanation

Same calculation as PYQ17 (50 kg person). Force multiplication equals area ratio — hydraulic press, brake, and lift designs.

Problem Solving — L9 Properties of Fluids

Six problems spanning this chapter’s NIOS syllabus. Every question is built from the notes and formula sheet: solve with equations first, then read the formal textbook-style write-up, the easy explanation, and the topic in depth (formulas, meaning, exam tips). Explanations open by default.

Question 1 of 6Pressure

Find pressure due to a 5.0 m column of water (ρ = 10³ kg·m⁻³, g = 10) at the bottom. What is gauge pressure and absolute pressure if atmospheric pressure is 10⁵ Pa?

P = F/A
P = hρg

Solution — step by step with formulas

  1. P_gauge = hρg = 5×1000×10 = 5.0×10⁴ Pa.
  2. P_abs = P_atm + P_gauge = 1.5×10⁵ Pa.

Final answer: Gauge 5×10⁴ Pa; absolute 1.5×10⁵ Pa

Formulas used in this problem

P = F/A
P = hρg

Textbook formal language

Hydrostatic pressure at depth h in an incompressible fluid of density ρ is hρg (gauge). Absolute pressure adds atmospheric pressure.

Working formula set for this problem: P = F/A; P = hρg. In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Deeper water presses harder: 5 m of water adds 50 kPa. Total push including air is 150 kPa.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Fluid pressure

Pressure acts equally in all directions at a point (Pascal). Same depth ⇒ same pressure regardless of container shape (hydrostatic paradox).

Link to chapter notes (L9 — Fluid pressure): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: P = F/A; P = hρg. In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write P = F/A; P = hρg before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).
Question 2 of 6Pascal

In a hydraulic lift, small piston area 0.01 m², large 0.20 m². What force on small piston lifts a 2000 N load on the large piston?

F₁/A₁ = F₂/A₂

Solution — step by step with formulas

  1. F₁ = F₂ (A₁/A₂) = 2000×(0.01/0.20) = 100 N.

Final answer: F₁ = 100 N

Formulas used in this problem

F₁/A₁ = F₂/A₂

Textbook formal language

Pascal’s law: pressure applied to an enclosed fluid is transmitted undiminished. Hence F/A is equal on both pistons.

Working formula set for this problem: F₁/A₁ = F₂/A₂. In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Same pressure, bigger pad multiplies force. Area ratio 20 ⇒ force ratio 20; 2000 N needs only 100 N on the small side.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Pascal’s law / hydraulic lift

Ideal hydraulic machines ignore friction and fluid compressibility.

Link to chapter notes (L9 — Pascal’s law / hydraulic lift): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: F₁/A₁ = F₂/A₂. In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write F₁/A₁ = F₂/A₂ before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).
Question 3 of 6Archimedes

A 0.5 kg object fully immersed displaces 200 cm³ of water. Find buoyant force (g=10) and apparent weight.

F_B = V_displaced ρ_fluid g

Solution — step by step with formulas

  1. V = 200×10⁻⁶ m³ = 2×10⁻⁴ m³.
  2. F_B = 2×10⁻⁴×1000×10 = 2.0 N.
  3. True weight = 5.0 N; apparent weight = 5.0 − 2.0 = 3.0 N.

Final answer: F_B = 2 N; apparent weight 3 N

Formulas used in this problem

F_B = V_displaced ρ_fluid g

Textbook formal language

Archimedes’ principle: upthrust equals weight of fluid displaced. Apparent weight is true weight minus upthrust when fully immersed.

Working formula set for this problem: F_B = V_displaced ρ_fluid g. In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Water pushes up with the weight of the water kicked aside—here 2 N. Scale reading drops by 2 N.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Buoyancy

Floatation: weight = upthrust ⇒ average density ≤ fluid density.

Link to chapter notes (L9 — Buoyancy): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: F_B = V_displaced ρ_fluid g. In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write F_B = V_displaced ρ_fluid g before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).
Question 4 of 6Bernoulli

State Bernoulli’s equation and explain why airspeed over an aeroplane wing being higher than below can produce lift (qualitative).

P + ½ρv² + ρgh = constant

Solution — step by step with formulas

  1. Along a streamline for steady, incompressible, non-viscous flow: P + ½ρv² + ρgh = const.
  2. Higher v above wing ⇒ lower P above than below ⇒ net upward force (lift).

Final answer: Higher speed → lower pressure above wing → lift

Formulas used in this problem

P + ½ρv² + ρgh = constant

Textbook formal language

Bernoulli’s theorem equates mechanical energy per unit volume along a streamline under ideal-flow assumptions. Pressure and kinetic terms trade off when height is fixed.

Working formula set for this problem: P + ½ρv² + ρgh = constant. In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Fast air means lower push. Wing shape makes air rush over the top, so bottom pressure is higher and the plane is pushed up.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Bernoulli’s principle

Assumptions fail for turbulent or highly viscous flows; real wings also use angle of attack and circulation.

Link to chapter notes (L9 — Bernoulli’s principle): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: P + ½ρv² + ρgh = constant. In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write P + ½ρv² + ρgh = constant before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).
Question 5 of 6Equation of continuity

Water flows in a pipe of area 4.0 cm² at 0.50 m·s⁻¹. Find speed where area narrows to 1.0 cm².

A₁v₁ = A₂v₂

Solution — step by step with formulas

  1. v₂ = v₁(A₁/A₂) = 0.50×4 = 2.0 m·s⁻¹.

Final answer: v₂ = 2.0 m·s⁻¹

Formulas used in this problem

A₁v₁ = A₂v₂

Textbook formal language

For incompressible steady flow, volume flux is conserved: Av = constant.

Working formula set for this problem: A₁v₁ = A₂v₂. In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Same amount of water each second must go through. Narrower pipe ⇒ faster flow.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Continuity equation

Combine with Bernoulli for Venturi effect: narrow region has higher speed, lower pressure.

Link to chapter notes (L9 — Continuity equation): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: A₁v₁ = A₂v₂. In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write A₁v₁ = A₂v₂ before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).
Question 6 of 6Viscosity / Stokes

Explain terminal velocity of a raindrop falling in air qualitatively using force balance.

F_d = 6πηrv (Stokes)
mg = 6πηrv_t + buoyancy (terminal)

Solution — step by step with formulas

  1. Initially gravity dominates ⇒ acceleration.
  2. Viscous drag (and buoyancy) grow with speed until net force ≈ 0 ⇒ constant terminal speed.

Final answer: v_t when weight = drag + buoyancy

Formulas used in this problem

F_d = 6πηrv (Stokes)
mg = 6πηrv_t + buoyancy (terminal)

Textbook formal language

At terminal velocity, downward gravitational force is balanced by upward buoyant force and viscous drag; net force and acceleration vanish.

Working formula set for this problem: F_d = 6πηrv (Stokes); mg = 6πηrv_t + buoyancy (terminal). In the NIOS presentation, physical quantities must be expressed in SI units and the relevant law or definition stated before substitution. Vector quantities require an explicit choice of positive direction; scalar work and energy require attention to sign conventions of the textbook.

Easy language (same idea, plain words)

Drop falls faster until air resistance catches up with weight; then it stops speeding up and falls at steady speed.

Read the question once for the story, once for the numbers. Write the formula, plug in values with units, then simplify. If a result looks huge or tiny, re-check powers of ten and whether you used sin/cos of the correct angle.

Topic in depth — Viscous drag and terminal speed

Stokes’ law applies to small spheres at low Reynolds number; larger drops deform and use different drag laws.

Link to chapter notes (L9 — Viscous drag and terminal speed): this idea sits with the definitions and worked examples in the detailed notes and formula sheet. Memorise: F_d = 6πηrv (Stokes); mg = 6πηrv_t + buoyancy (terminal). In multi-step questions, keep a free-body diagram or energy flow sketch before algebra; most errors are missing forces or wrong signs, not hard maths.

Exam tip

Quote the law in one line, then write F_d = 6πηrv (Stokes); mg = 6πηrv_t + buoyancy (terminal) before numbers. Box the final answer with unit. For numericals, keep at least three significant figures until the last step unless the data are coarse.

Common mistakes

  • Mixing up scalar and vector quantities (e.g. treating momentum as unsigned).
  • Using the wrong sign convention for work/heat/force direction.
  • Forgetting to convert units (g↔kg, cm↔m, minutes↔seconds).
  • Applying a formula outside its assumptions (e.g. F = ma when mass is not constant).