Matter can appear as solid, liquid, or gas depending on particle motion and intermolecular forces.

1. Kinetic Theory of Matter

Main ideas:

  • Matter is made of particles.
  • Particles are always moving.
  • Temperature is related to average kinetic energy.
  • Intermolecular forces and particle distance determine the state.

2. States of Matter

PropertySolidLiquidGas
Particle distanceVery smallSmall-mediumLarge
Intermolecular forceStrongMediumVery weak
ShapeDefiniteTakes container shapeFills container
VolumeDefiniteDefiniteVariable
CompressibilityVery lowLowHigh

3. Density

Density links mass and volume:

$$ \rho = \frac{m}{V} $$

Useful rearrangements:

$$ m = \rho V $$
$$ V = \frac{m}{\rho} $$

Typical units:

  • $\mathrm{kg/m^3}$
  • $\mathrm{g/cm^3}$
  • $\mathrm{kg/L}$

4. Changes of State

  • Melting: solid $\to$ liquid
  • Freezing: liquid $\to$ solid
  • Vaporization (evaporation/boiling): liquid $\to$ gas
  • Condensation: gas $\to$ liquid
  • Sublimation: solid $\to$ gas
  • Deposition: gas $\to$ solid

During a phase change, temperature stays constant while energy is used to break or form intermolecular interactions.

5. Heating Curve

In a heating curve:

  • Rising segments: temperature increases in one state.
  • Flat segments: phase change at constant temperature.

Two important temperatures:

  • Melting point
  • Boiling point

6. Gas Laws (qualitative and quantitative)

Gas behavior depends on pressure $P$, volume $V$, and temperature $T$ (in kelvin).

Boyle law (constant temperature)

$$ P_1V_1 = P_2V_2 $$

Charles law (constant pressure)

$$ \frac{V_1}{T_1} = \frac{V_2}{T_2} $$

Gay-Lussac law (constant volume)

$$ \frac{P_1}{T_1} = \frac{P_2}{T_2} $$

Combined gas law

$$ \frac{P_1V_1}{T_1} = \frac{P_2V_2}{T_2} $$

Remember temperature conversion:

$$ T(\mathrm{K}) = T(^\circ\mathrm{C}) + 273.15 $$

7. Everyday Examples

  • A perfume smell spreads because gas particles move and diffuse.
  • A pressure cooker increases pressure, raising boiling temperature.
  • Clothes dry below boiling point by evaporation from the surface.