By the end of this chapter you'll be able to…

  • 1State the composition of air: Nitrogen ~78%, Oxygen ~21%, Argon ~0.9%, CO₂ ~0.04%, water vapour and other gases ~0.06%
  • 2Demonstrate properties of air: occupies space (inverted glass experiment), has weight (inflated vs deflated balloon), exerts pressure (crushing can experiment — steam condenses, creating vacuum, atmospheric pressure crushes the can)
  • 3Explain that warm air rises (candle pinwheel experiment) — this is convection, the principle behind hot air balloons and sea breezes
  • 4Identify causes of air pollution (vehicles, factories, crackers, burning waste, crop stubble burning) and their effects (global warming — CO₂; acid rain — SO₂ and NO₂; respiratory diseases — PM2.5 and PM10)
  • 5Explain global warming: increased CO₂ and other greenhouse gases trap heat in the atmosphere → Earth's average temperature rises → melting glaciers, rising sea levels, extreme weather
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Why this chapter matters
Air in Class 5 is the final primary school chapter on the atmosphere. Children revisit the composition of air with greater precision, study the properties of air through experiments, and connect air to real-world phenomena — why a bicycle pump gets hot (compression), why a straw works (air pressure), why aeroplanes fly (Bernoulli's principle in simple terms). The chapter also covers air pollution in depth, linking to global warming and climate change — topics that will dominate their middle and high school science. For a generation growing up in a warming world, understanding air is not just science — it is survival.

Before you start — revise these

A 5-minute refresher here will save you 30 minutes of confusion below.

Air — Class 5 Science (Samacheer Kalvi)

TN State Board (Samacheer Kalvi) Class 5 Science. What air is made of, what it can do, and how we are changing it.


1. What air is made of

Air is not a single gas but a mixture.

GasShareRole
Nitrogenabout 78%Dilutes the oxygen; plants need it for proteins
Oxygenabout 21%Needed for breathing and burning
Argonabout 0.9%An unreactive gas
Carbon dioxideabout 0.04%Used by plants to make food
Water vapour and other gasesabout 0.06%Includes neon, helium and methane

Oxygen is the gas we cannot live without, but nitrogen is the most abundant. That is fortunate. Nitrogen dilutes the oxygen, so fires stay controllable.

2. Air occupies space

Invert an empty glass and push it straight down into water. The water does not rise inside, because air already occupies that space.

Blow into a balloon and it swells for the same reason.

3. Air has weight

Weigh a deflated balloon on a sensitive balance, then inflate it and weigh it again. The inflated one is heavier. Air is not nothing — a cubic metre of it weighs roughly 1.2 kg at sea level.

4. Air exerts pressure

Because air has weight, the column of air above us presses down. This is atmospheric pressure, and it acts in every direction.

The crushing can experiment shows it dramatically. Boil a little water in a tin can so steam drives the air out, then seal it and cool it suddenly. The steam condenses into a few drops of water, leaving almost a vacuum inside. With nothing pushing back, the atmosphere outside crushes the can flat.

Nothing was added or removed from outside. The air pressure had been there all along; the experiment simply took away the pressure that had been balancing it.

5. Warm air rises: convection

Heat air and its particles move faster and spread apart. The air becomes less dense, and so it rises. Cooler, denser air rushes in to take its place.

That movement of air is wind.

You can see it with a paper pinwheel held above a candle. The rising warm air spins it, though nobody is blowing.

The same idea explains why hot air balloons float, why smoke goes up a chimney, and why the upstairs of a house is warmer than the ground floor.

6. Weather and climate are not the same

Weather is what the air is doing now or over a few days — sunny, rainy, windy.

Climate is the average pattern of weather over many years in a place.

So a cold day in summer is weather, not evidence against a warming climate. One day proves nothing about a long-term trend.

7. The greenhouse effect and global warming

Sunlight passes through the atmosphere and warms the Earth. The warmed Earth then radiates heat back out.

Certain gases — carbon dioxide, methane, water vapour — trap part of that outgoing heat instead of letting it escape. These are greenhouse gases, and the trapping is the greenhouse effect.

Some greenhouse effect is essential; without it the Earth would be frozen. The problem is that burning fuels has added far more of these gases than before, so more heat is trapped and the average temperature rises. This is global warming.

Global warming is not the same as the ozone hole. They are two different problems. The ozone hole is the thinning of the ozone layer, which shields us from harmful ultraviolet rays. Global warming is the trapping of heat. Do not mix them up.

8. Worked examples

Example 1. Which gas is most abundant in air?

Solution: Nitrogen, at about 78%.

Example 2. How would you show that air occupies space?

Solution: Invert an empty glass into water. The water cannot enter, because air fills the glass.

Example 3. Why does the can collapse in the crushing can experiment?

Solution: The steam condenses, leaving near vacuum inside. With no pressure pushing outward, atmospheric pressure outside crushes the can.

Example 4. Why does warm air rise?

Solution: Heating makes its particles spread apart, so the air becomes less dense than the cooler air around it.

Example 5. What causes wind?

Solution: Warm air rising and cooler, denser air rushing in to take its place.

Example 6. Is a cold day in summer evidence against global warming?

Solution: No. That is weather, a short-term change. Global warming is a long-term change in climate.

9. Practice

  1. Name the four main gases in air with their approximate percentages.
  2. Why is it fortunate that air is mostly nitrogen rather than oxygen?
  3. Describe an experiment showing that air has weight.
  4. What is atmospheric pressure?
  5. Explain the difference between weather and climate.
  6. Name three greenhouse gases.
  7. What is the greenhouse effect?
  8. How does the ozone hole differ from global warming?

10. Answers

  1. Nitrogen about 78%, oxygen about 21%, argon about 0.9%, carbon dioxide about 0.04%.
  2. Oxygen supports burning, so an atmosphere of mostly oxygen would let fires blaze uncontrollably.
  3. Weigh a deflated balloon, then inflate it and weigh it again; the inflated balloon is heavier.
  4. The pressure exerted by the weight of the column of air above us, acting in all directions.
  5. Weather is the short-term state of the air; climate is the average pattern over many years.
  6. Carbon dioxide, methane and water vapour.
  7. Greenhouse gases trapping part of the heat the Earth radiates back out, keeping the planet warmer.
  8. The ozone hole is thinning of the ozone layer that blocks ultraviolet rays; global warming is heat being trapped by greenhouse gases.

11. Summary

  • Air is a mixture: about 78% nitrogen, 21% oxygen, 0.9% argon and 0.04% carbon dioxide.
  • Nitrogen is the most abundant gas and dilutes the oxygen so fires stay controllable.
  • Air occupies space, has weight, and exerts pressure in all directions.
  • The crushing can experiment shows atmospheric pressure by removing the pressure inside.
  • Heated air becomes less dense and rises; cooler air rushing in makes wind.
  • Weather is short term; climate is the long-term average.
  • Greenhouse gases trap outgoing heat, and burning fuels has increased them, causing global warming.
  • The ozone hole and global warming are two different problems.

Key formulas & results

Everything you need to memorise, in one card. Screenshot this for revision.

Properties of air (with experiments)
Air occupies space → invert an empty glass into water — water does not enter because air occupies the space. Blow into a balloon → it expands because air occupies space. Air has weight → weigh a deflated balloon, then inflate and weigh again — the inflated balloon is heavier. Air exerts pressure → fill a can with a little water, heat until steam comes out, quickly invert into cold water — the can crushes! Steam condenses creating vacuum inside; outside atmospheric pressure (14.7 pounds per square inch) crushes the can.
The crushing can experiment is dramatic and memorable. It demonstrates that air pressure is not 'nothing' — it is a force of about 1 kg per square centimetre, pushing on everything from all directions.
Global warming and the Greenhouse Effect
Sunlight (short wave radiation) passes through the atmosphere and warms the Earth. The Earth re-radiates heat as long-wave (infrared) radiation. Greenhouse gases (CO₂, methane, water vapour, CFCs) in the atmosphere TRAP some of this heat, keeping Earth warm enough for life. This is the natural greenhouse effect — without it, Earth's average temperature would be −18°C instead of +15°C. PROBLEM: Human activities have increased CO₂ by ~50% since the industrial revolution (burning fossil fuels, deforestation). This ENHANCED greenhouse effect is causing global temperatures to rise — global warming.
The last 10 years (2016-2026) have been the hottest decade on record. Tamil Nadu has experienced more frequent heatwaves, irregular monsoons, and coastal erosion — all linked to climate change.
Convection — warm air rises
When air is heated, its molecules move faster and spread apart → the air becomes less dense (lighter) → it RISES. Cooler, denser air rushes in to take its place → this movement creates WIND. This is why: hot air balloons rise, chimney smoke goes up, sea breeze blows from sea to land during the day (land heats faster → air rises → cooler sea air rushes in), land breeze blows from land to sea at night (land cools faster → sea is warmer → air rises over sea → cooler land air rushes out).
Chennai's famous sea breeze in the evening is convection in action. After a hot day, the land cools while the Bay of Bengal retains warmth — creating the pleasant evening breeze that makes Marina Beach so popular.
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Common mistakes & fixes

These are the exact errors that cost students marks in board exams. Read them once, save yourself the trouble.

WATCH OUT
✗ Confusing weather (short-term) and climate (long-term)
✓ A cold day in summer is WEATHER — a temporary change. Global warming is CLIMATE — the long-term average temperature trend. One cold winter does not disprove global warming, just as one hot day does not prove it.
WATCH OUT
✗ Thinking the ozone hole and global warming are the same thing
✓ They are DIFFERENT problems. Ozone hole = depletion of the ozone layer (O₃) by CFCs, allowing harmful UV radiation to reach Earth. This causes skin cancer. Global warming = trapping of heat by greenhouse gases (CO₂, methane), causing Earth to warm. The ozone hole is being fixed (Montreal Protocol banned CFCs). Global warming is still getting worse.

Practice problems

Work through this chapter's problems as a readiness check — reveal each solution, mark yourself honestly, and get your gap report at the end.

Readiness check

Are you exam-ready for Air?

11 problems from this chapter. Try each one, reveal the worked solution, mark yourself honestly — get your gap report at the end.

11 questions~8 min worth ~8 marks in Tamil Nadu (TNBSE) exams

Tamil Nadu (TNBSE) marks blueprint

Where the marks come from in this chapter — so you can plan your prep.

Typical chapter weightage: 6-8 marks in TN Class 5 Science exams

Question typeMarks eachTypical countWhat it tests
Composition1-2The gases of air and their proportions
Properties2Air occupies space, has weight and exerts pressure
Convection1-2Warm air rising and the formation of wind
Weather and climate1-2Distinguishing short-term weather from long-term climate
Greenhouse2The greenhouse effect, global warming and the ozone hole
Verified by the tuition.in editorial team
Last reviewed on 3 June 2026. Written and reviewed by subject-matter experts — read about our process.
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