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Vapour is taught in the note for Vapour and Humidity. Read it below and look for the section on this topic.

Vapour and Humidity

10 min read

Vapour

A gas can be liquefied by pressure at any temperature below its critical temperature. A gas below its critical temperature is called a vapour. Evaporation is the escape of the fastest particles from the surface of a liquid at any temperature. Boiling takes place at a fixed temperature throughout the liquid, when bubbles of vapour form inside it.

EvaporationBoiling
TemperatureAt any temperatureAt the boiling point only
WhereAt the surface onlyThroughout the liquid
SpeedSlowFast
Rate depends onTemperature, surface area, wind, humidityHeat supply

A vapour in contact with its own liquid is saturated when the number of particles leaving the liquid equals the number returning. Its pressure, the saturated vapour pressure (SVP), depends only on the temperature: it rises rapidly as the temperature rises. A liquid boils when its saturated vapour pressure equals the external pressure. That is why water boils at a lower temperature on a mountain (lower pressure) and at a higher temperature in a pressure cooker.

Water boils when its saturated vapour pressure reaches the atmospheric pressure of about 101 kPa, at 100 °C.

Humidity

Humidity is the amount of water vapour in the air. Absolute humidity is the mass of water vapour in each cubic metre of air. Relative humidity compares the amount of vapour present with the greatest amount the air could hold at that temperature.

When the air is saturated, relative humidity is 100%. Warm air can hold more vapour than cold air.
Try itRelative humidity

Choose the actual vapour pressure and the saturated vapour pressure at the air temperature. Find the relative humidity.

Dew point and hygrometers

If air is cooled, its saturated vapour pressure falls until it equals the vapour pressure present. This temperature is the dew point. Below it vapour condenses as dew, mist or fog. A hygrometer measures humidity. In a wet and dry bulb hygrometer, evaporation cools the wet bulb, so it reads lower than the dry bulb. The drier the air, the bigger the difference.

Wet and dry bulb hygrometerTwo thermometers side by side. The dry bulb reads the air temperature. The wet bulb is wrapped in damp cloth, and evaporation cools it so it reads lower. The drier the air, the faster the evaporation and the bigger the difference between the two readings; a table converts the difference into relative humidity.dry bulb 28 °Cwet bulb 22 °Cdifference 6 °C → relative humidity about 60%damp cloth
EffectExplanation
Wet clothes dry faster on a windy dayWind carries away water vapour so evaporation continues
Sweat feels sticky in humid weatherAir that is almost saturated takes little more vapour, so sweat evaporates slowly
Dew forms on grass at nightThe grass cools below the dew point
Clouds and rainRising warm air cools to its dew point and the vapour condenses into droplets
Check yourself The dew point is the temperature at which…
Check yourself Water boils at a lower temperature on a high mountain because…
Check yourself The air has a vapour pressure of 1.2 kPa and the saturated value is 2.4 kPa. The relative humidity is…

Key terms

Saturated vapour pressure
The pressure of a vapour in equilibrium with its liquid at a given temperature.
Relative humidity
The ratio of the vapour pressure present to the saturated vapour pressure, as a percentage.
Dew point
The temperature at which air becomes saturated.
Hygrometer
An instrument for measuring humidity.

Summary

  • Evaporation occurs at any temperature at the surface; boiling at a fixed temperature throughout.
  • Saturated vapour pressure depends on temperature; boiling occurs when SVP equals external pressure.
  • Relative humidity = vapour pressure ÷ SVP × 100.
  • Dew point is the temperature at which air is saturated.