Revision notes · Particle model of matter
Changes of state and the particle model
Density of materials4.3.1.1
| Equation | Units |
|---|---|
| ρ = m ÷ V | ρ (density) in kg/m³, m (mass) in kg, V (volume) in m³ |
- •Required practical — regular solid: measure mass on a balance; measure length/width/height with a ruler (or diameter with callipers for a cylinder) and calculate the volume from the shape's formula; density = mass ÷ volume.
- •Required practical — irregular solid: measure mass on a balance; find the volume by displacement — lower the object into a eureka can filled to the spout with water, and the volume of water collected in a measuring cylinder equals the object's volume.
Density depends on how closely packed the particles of a material are. In solids and liquids, particles are closely packed with little space between them, so solids and liquids have similar densities (usually a liquid is slightly less dense than the same substance as a solid, though water is a well-known exception — ice is less dense than liquid water). In a gas, particles are spread much further apart and have much more energy to move around, so gases have a far lower density than solids or liquids of the same substance.
Changes of state4.3.1.2
| Change | From → to |
|---|---|
| Melting | Solid → liquid |
| Freezing | Liquid → solid |
| Evaporating / boiling | Liquid → gas |
| Condensing | Gas → liquid |
| Sublimation | Solid → gas directly (e.g. solid carbon dioxide, 'dry ice') |
Mass is conserved during a change of state — if 20 g of liquid evaporates, the gas produced also has a mass of 20 g. No particles are created or destroyed, they simply rearrange and change how far apart they are.
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