States of Matter & Vapor Pressure

20min Part 2 / Ch3 / Lesson 4
Prerequisites: 2-3-1

Objectives

  • Explain the three states of matter and phase changes using particle models
  • Understand the relationship between vapor pressure and boiling point
  • Read and interpret phase diagrams

Three States of Matter

Matter exists in three states — solid, liquid, gas — determined by temperature and pressure.

ChangeNameEnergy
Solid → LiquidMeltingEndothermic
Liquid → GasVaporizationEndothermic
Solid → GasSublimationEndothermic
Gas → LiquidCondensationExothermic
Liquid → SolidFreezingExothermic
Gas → SolidDepositionExothermic

Heating curve: When a pure substance is heated at a constant rate, the temperature plateaus at the melting and boiling points (latent heat is being absorbed).

Heating time →Temp (°C)Ice0°C (melting)Water100°C (boiling)Steam
Heating curve of water

Vapor Pressure

In a closed container, liquid evaporates until the rate of evaporation = rate of condensation — this is liquid-vapor equilibrium.

The pressure exerted by the vapor at this point is the saturated vapor pressure (vapor pressure).

  • Vapor pressure increases with temperature
  • Boiling point = temperature at which vapor pressure equals external pressure
  • At high altitude (lower atmospheric pressure), the boiling point is lower

Phase Diagrams

Temperature →Pressure →Triple pointSolidLiquidGas1 atm
Phase diagram of water (schematic)

In a phase diagram:

  • Triple point: all three phases coexist
  • Critical point: beyond this temperature, liquid and gas become indistinguishable
  • Lines = boundaries where two phases coexist
  • Water’s anomaly: the solid-liquid boundary slopes to the left (ice is less dense than water)

Check Your Understanding

Q1 The boiling point is the temperature at which vapor pressure equals...

Q2 What does a plateau on a heating curve indicate?

Q3 What is the triple point on a phase diagram?


Exercises

Q1. Explain why water boils below 100°C at the summit of Mt. Fuji (atmospheric pressure ≈ 0.63 atm).

Solution

Boiling occurs when the vapor pressure equals the external (atmospheric) pressure.

At the summit of Mt. Fuji, atmospheric pressure is only 0.63 atm, so the vapor pressure reaches 0.63 atm at a lower temperature (~87°C), and boiling begins there.

In other words, when external pressure is lower, a lower temperature is enough for vapor pressure to match it, resulting in a lower boiling point.