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KS3 Science · National Curriculum · Physics: Matter
Mini-Lesson

Physics — Matter

This mini-lesson builds the particle model of matter: how particles are arranged in solids, liquids and gases, how that explains density and changes of state, the difference between heat and temperature, and the difference between mass and weight.

solid 🧊 liquid 💧 gas 💨 melt boil
Heating adds energy to the particles: a solid can melt to a liquid, and a liquid can boil to a gas.

Work through each screen, answer the questions as you go (some are wordy, some are calculations) and collect ⭐ stars. Press Start when you're ready.

The three states of matter

Solid, liquid and gas

Everything around you is matter — it has mass and takes up space. Most matter you meet is in one of three states:

  • A solid keeps its own shape and can't be squashed much.
  • A liquid flows and takes the shape of its container, but keeps the same volume.
  • A gas spreads out to fill any container completely and can be squashed easily.

Same stuff, different state: ice, water and steam are all H₂O. Changing state doesn't change what the substance is — only how its particles are arranged and moving.

The particle model

Zoom in: the particle model

Imagine zooming in until you can see the tiny particles. Their arrangement, how close they are and how much they move decide the state:

SOLID packed · vibrate in place LIQUID close · slide past each other GAS far apart · move fast, freely
Left to right the particles get further apart and move more. Notice the same number of particles fills far more space in the gas — so a gas is far less dense.

Key idea: the particles themselves stay the same size and mass. Only their spacing, arrangement and movement change between states.

Quick check

Read the particles

?In which state are the particles far apart, arranged randomly, and moving quickly in all directions?
Density

Density: how packed the particles are

Density tells you how much mass is squeezed into a certain volume. It is not the same as "how heavy" — a huge block of foam can weigh more than a tiny steel ball, yet the steel is far more dense.

density = mass ÷ volumedensity (kg/m³ or g/cm³) = mass ÷ volume

Because a solid's particles are packed tightly and a gas's are spread out, most substances are densest as a solid and least dense as a gas.

Worked example

A metal block has a mass of 240 g and a volume of 30 cm³.

density = 240 ÷ 30 = 8 g/cm³

Calculate

Your turn — density

1A block of wood has a mass of 60 g and a volume of 120 cm³. Calculate its density in g/cm³.
g/cm³
Hint: density = mass ÷ volume = 60 ÷ 120.
Common mistake

Dense ≠ heavy

It's tempting to say "steel is heavier than wood" — but a matchstick of steel weighs less than a tree trunk. What we really mean is that steel is more dense: for the same volume, it has more mass because its particles are heavier and more tightly packed.

foam — few particles = same volume steel — many particles
Same-sized cubes: the steel packs in far more mass, so it is more dense and would sink where the foam floats.

Watch out: density is about mass per volume, not just weight. Always compare the same volume when you decide which is denser.

Quick check

Which is more dense?

?You have a 1 cm³ cube of lead and a 1 cm³ cube of cork. The lead cube has much more mass. Which statement is correct?
Changes of state

Changing state (physical changes)

Adding or removing energy can change the state. These are physical changesno new substance is made and they can be reversed:

  • Melting — solid → liquid. Freezing — liquid → solid.
  • Boiling / evaporating — liquid → gas. Condensing — gas → liquid.
  • Sublimation — solid → gas directly (e.g. dry ice).

Conservation of mass: when ice melts into water, or water boils into steam, no mass is lost. The particles are the same particles — just rearranged. Melt 50 g of ice and you get 50 g of water.

Sort it

Physical change or not?

A physical change makes no new substance and can be reversed. Tap the correct label for each.

Conservation of mass

Mass is conserved

In a sealed container, if a solid melts, evaporates or condenses, the total mass stays the same. Nothing is created or destroyed — the particles just spread out or come together.

Worked example

A sealed flask holds 80 g of ice. The ice melts completely.

Mass of water afterwards = 80 g (unchanged).

Why steam looks like it "vanishes": in an open pan the gas escapes into the room, so the pan gets lighter — but the mass isn't lost, it has just spread out into the air.

Calculate

Your turn — conservation of mass

2A sealed test tube contains 45 g of ice. It is warmed until all the ice melts to water. What mass of water is now in the sealed tube?
g
Hint: it's sealed, so no particles escape — mass is conserved.
Heat vs temperature

Heat is not the same as temperature

Temperature tells you how hot something is — really, how fast its particles are moving on average. Heat (or thermal energy) is the total energy transferred, and it always flows from a hotter place to a cooler one.

  • A sparkler is at a very high temperature but carries very little heat energy — it barely warms your hand.
  • A warm bath is at a lower temperature but holds a huge amount of heat energy because there is so much water.

Direction of flow: energy is transferred by heating from hot to cold until both reach the same temperature (thermal equilibrium) — never the other way round on its own.

Quick check

Hot vs a lot of energy

?A tiny spark at 800 °C lands on your arm and barely hurts, while a bath at 45 °C would scald you if it were hotter still. Why can the cooler bath transfer far more energy?
Energy in matter

The heating curve & latent heat

If you heat ice steadily and record its temperature, the graph has flat plateaus. During a change of state the temperature stops rising even though energy is still going in:

temperature → energy added → 0°C 100°C melting boiling solid liquid gas
The flat plateaus are where the substance changes state. The energy going in (latent heat) is used to pull the particles apart, not to raise the temperature.

Latent heat: a change of state needs energy without a temperature change. Melting and boiling absorb this energy to break the forces holding particles together.

Quick check

Reading the plateau

?On the heating curve, the temperature stays flat while ice is melting even though the heater is still on. Where is that energy going?
Heating and expansion

Heating: particles move more, not grow

When you heat a substance, the particles gain energy and move faster, so they push a little further apart. This makes the whole object expand slightly — but the particles themselves do not grow.

cool: packed, slow warm: spread out, fast
Same 8 particles, same size — but when warm they take up more space, so the object expands and becomes slightly less dense.

Watch out: a common wrong idea is that particles "get bigger" when heated. They don't — they just move faster and spread apart.

Evidence for particles

Diffusion & Brownian motion

We can't see particles, but their movement leaves clues:

  • Diffusion — a drop of ink spreads through still water, and the smell of perfume drifts across a room. The particles move about and mix on their own, with no stirring.
  • Brownian motion — tiny smoke or pollen grains seen under a microscope jiggle randomly. They are being knocked about by even smaller, fast-moving particles you can't see.
ink diffuses Brownian: jagged path
Diffusion and Brownian motion are strong evidence that matter is made of small, constantly-moving particles.
Quick check

What does the jiggle show?

?Under a microscope, smoke grains are seen jiggling about in random, jerky paths. What is the best explanation?
Mass and weight

Mass vs weight

Mass is the amount of matter in an object, measured in kilograms (kg). It stays the same wherever you take it. Weight is the pull of gravity on that mass, measured in newtons (N), and it changes with the gravitational field strength:

W = m × gweight (N) = mass (kg) × gravitational field strength (N/kg)

On Earth g ≈ 10 N/kg. On the Moon g is only about 1.6 N/kg, so the same astronaut weighs less on the Moon — but has exactly the same mass.

Worked example

A 6 kg bag on Earth (g = 10 N/kg):

W = 6 × 10 = 60 N

Calculate

Your turn — weight

3A rock has a mass of 8 kg. On Earth the gravitational field strength is 10 N/kg. Calculate the weight of the rock on Earth.
N
Hint: W = m × g = 8 × 10.
Quick check

On the Moon

?An astronaut travels from Earth to the Moon, where gravity is weaker. What happens to her mass and her weight?
Match it

Match the state to its particles

Tap a state on the left, then tap its matching description on the right.

State
Particles & density
Recap

The big ideas to know

Particle model: solid = packed & vibrating; liquid = close & sliding; gas = far apart & fast.

Density: density = mass ÷ volume (how packed, not just how heavy).

Changes of state are physical, reversible and conserve mass.

Heat vs temperature: temperature = average particle speed; heat = total energy, flows hot → cold.

Latent heat: changing state needs energy with no temperature change.

Mass vs weight: W = m × g; mass is fixed, weight changes with gravity.

You've covered the KS3 Physics — Matter ideas: the particle model, density, changes of state, heat vs temperature, and mass vs weight. Press Finish to see your score.

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