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Class 9–10 · Physics

States of matter and pressure

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States of matter and pressure

Fbmg
In floating equilibrium, buoyancy balances weight.
Lessons in this chapter
  1. Particles and states
  2. Elasticity and Hooke's law
  3. Density and relative density
  4. Pressure on a surface
  5. Liquid and atmospheric pressure
  6. Pascal's principle
  7. Buoyancy and Archimedes' principle
  8. Floating and sinking
  9. Surface tension, viscosity and diffusion

Lessons

1

Particles and states

Fbmg
In floating equilibrium, buoyancy balances weight.

Solid particles vibrate near fixed positions; liquid particles move past neighbours; gas particles are widely separated. This explains shape, volume and compressibility. Heating usually increases average microscopic kinetic energy.

Key relationship

solid: fixed shape and volume; liquid: fixed volume; gas: neither

Worked example

Air in a closed syringe compresses much more readily than water.

2

Elasticity and Hooke's law

Fbmg
In floating equilibrium, buoyancy balances weight.

Elastic materials recover their shape after force is removed. Within its linear range, a spring's extension is proportional to force. Stress is force per area and strain is fractional extension. Beyond limits, permanent deformation may occur.

Key relationship

F = kx; stress = F/A; strain = ΔL/L

Worked example

k = 200 N/m, x = 0.03 m ⇒ F = 6 N

3

Density and relative density

Fbmg
In floating equilibrium, buoyancy balances weight.

Density is mass per volume. Relative density compares it with a reference, commonly water at a specified temperature for solids and liquids. The ratio has no unit. Consider both mass and volume when comparing objects.

Key relationship

ρ = m/V; relative density = ρobject/ρreference

Worked example

540 g / 200 cm³ = 2.7 g/cm³ = 2700 kg/m³

4

Pressure on a surface

Fbmg
In floating equilibrium, buoyancy balances weight.

Pressure is perpendicular force divided by area. The same force over a smaller area produces higher pressure. A sharp blade concentrates force, while a wide strap spreads it.

Key relationship

p = F⊥/A; 1 Pa = 1 N/m²

Worked example

100 N / 0.02 m² = 5000 Pa

5

Liquid and atmospheric pressure

Fbmg
In floating equilibrium, buoyancy balances weight.

Hydrostatic pressure increases with depth and density, independent of container shape. At equal depth in one connected stationary liquid, pressure is equal. Absolute pressure adds surface pressure to the liquid's gauge pressure. A barometer measures atmospheric pressure.

Key relationship

gauge p = ρgh; absolute p = p₀+ρgh

Worked example

Water at 2 m: 1000 × 9.8 × 2 = 19600 Pa gauge

6

Pascal's principle

Fbmg
In floating equilibrium, buoyancy balances weight.

A pressure change applied to confined fluid is transmitted throughout it. A larger output piston gives greater force, but travels less far. An ideal hydraulic machine conserves work rather than creating energy.

Key relationship

F₁/A₁ = F₂/A₂; A₁s₁ = A₂s₂

Worked example

A₂ = 10A₁; F₁ = 50 N ⇒ F₂ = 500 N; 10 cm input travel ⇒ 1 cm output

7

Buoyancy and Archimedes' principle

Fbmg
In floating equilibrium, buoyancy balances weight.

Greater pressure below an immersed object produces an upward resultant. Buoyant force equals the weight of displaced fluid. Apparent weight is true weight minus buoyancy. The principle also applies in gases.

Key relationship

Fb = ρfluid g Vimmersed; apparent weight = mg−Fb

Worked example

Water, immersed volume 0.002 m³ ⇒ Fb = 19.6 N

8

Floating and sinking

Fbmg
In floating equilibrium, buoyancy balances weight.

A freely floating object displaces fluid of equal weight. Its average density includes hollow spaces, explaining steel ships. Moving it to denser fluid reduces the immersed volume needed for equilibrium.

Key relationship

floating: Vimmersed/Vtotal = ρobject/ρfluid

Worked example

Wood 600 kg/m³ in water 1000 kg/m³ ⇒ 60% of volume immersed

9

Surface tension, viscosity and diffusion

Fbmg
In floating equilibrium, buoyancy balances weight.

Surface tension resists increasing liquid surface area. Viscosity resists relative motion between fluid layers. Diffusion is net spreading from higher to lower concentration through random particle motion. These are distinct from density and pressure.

Key relationship

surface tension unit N/m

Worked example

A carefully placed needle may be supported by water's surface; honey flows slowly because of high viscosity.

Check your understanding

Try answering first, then open the question to compare your reasoning.

1. Same force, half area: pressure?

p = F/A ⇒ double

2. Twice the depth in one liquid: gauge pressure?

p = ρgh ⇒ double

3. Buoyancy in floating equilibrium equals what?

Fb = weight = mg

4. Output piston area is five times input: ideal force ratio?

F₂/F₁ = A₂/A₁ = 5

5. Fraction submerged for 800 kg/m³ wood in water?

800/1000 = 0.8 = 80%

Sources and scope

Original GetReady teaching notes. The 13 core chapters follow the existing site sequence. Physics to save life is an explicitly labelled older-edition supplement. Check your current book and board instructions for examination scope. Illustrations are schematic. Unless stated otherwise, use g = 9.8 m/s². A physics teacher should review content and edition coverage before it is relied on.