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AQA GCSE Chemistry (8462) · 4.9 Chemistry of the atmosphere
Mini-Lesson

Chemistry of the Atmosphere

This mini-lesson walks you through the whole of AQA Topic 4.9: what's in the air today, how Earth's atmosphere evolved over 4.6 billion years, the greenhouse gases and how the greenhouse effect works, global climate change, the carbon footprint, and the pollutants that combustion releases.

early air mostly CO₂ air today N₂ + O₂ ~4.6 billion years oceans, photosynthesis, rocks

Work through each screen, answer the questions as you go (some recall facts, some match a cause to its effect) and collect ⭐ stars. Press Start when you're ready.

Today's atmosphere · 4.9.1.1

What's in the air now?

For about 200 million years the proportions of gases in the atmosphere have been roughly the same as today:

N₂ ~78% O₂ ~21% Nitrogen — about ⅘ (~80%) Oxygen — about ⅕ (~20%) Small amounts of: • carbon dioxide • water vapour • noble gases
Roughly four-fifths nitrogen and one-fifth oxygen, with small amounts of other gases.

Exact figures: AQA says "about four-fifths (~80%) nitrogen" and "about one-fifth (~20%) oxygen." The fuller numbers ~78% N₂ and ~21% O₂ are also accepted — the remaining ~1% is argon, carbon dioxide and water vapour.

Quick check

Reading the air

?Which gas makes up about one-fifth (~20%) of today's atmosphere?
The early atmosphere · 4.9.1.2

Where the air came from

Evidence for the early atmosphere is limited because of the time scale of 4.6 billion years, so theories have changed and developed over time. One leading theory:

  • During Earth's first billion years, intense volcanic activity released gases that formed the early atmosphere.
  • It was likely mainly carbon dioxide, with little or no oxygen — much like Mars and Venus today.
  • Volcanoes also released water vapour, which condensed to form the oceans, plus nitrogen (which built up), and small proportions of methane and ammonia.
🌋 CO₂ — mainly carbon dioxide 💧 water vapour → condenses → oceans N₂ + small amounts of CH₄ & NH₃
When oceans formed, CO₂ dissolved in the water and carbonates precipitated as sediments — lowering atmospheric CO₂.
Oxygen up, CO₂ down · 4.9.1.3–4

How the air changed

Oxygen increased. About 2.7 billion years ago, algae first produced oxygen by photosynthesis; later plants evolved and the oxygen level gradually rose enough for animals to evolve:

6CO₂ + 6H₂O → C₆H₁₂O₆ + 6O₂carbon dioxide + water → glucose + oxygen (light energy, in algae & plants)

Carbon dioxide decreased in several ways:

  • Dissolving in the oceans (then locked away as carbonate sediments).
  • Photosynthesis by algae and plants.
  • Carbon being locked into sedimentary rocks (e.g. limestone) and into fossil fuels — coal, crude oil and natural gas.
oceans CO₂ dissolves; carbonates form photosynthesis algae & plants take in CO₂ locked in carbon sedimentary rocks & fossil fuels
Sort it

Order the events

Tap the event that came next in the story of Earth's atmosphere.

Quick check

Which process?

?Which process was the main reason the amount of oxygen in the atmosphere increased?
Greenhouse gases · 4.9.2.1

The greenhouse effect

Greenhouse gases keep Earth warm enough to support life. The three you must know are:

  • Carbon dioxide (CO₂)
  • Methane (CH₄)
  • Water vapour (H₂O)
☀️ short-wavelength sunlight in greenhouse gas layer long-wavelength IR absorbed & re-radiated warm Earth's surface
Short-wavelength radiation comes in; the warmed Earth re-radiates long-wavelength (infrared) radiation, which greenhouse gases absorb and re-radiate — some back to the surface.

Common misconception: the greenhouse effect itself is natural and essential — without it Earth would be too cold for life. The concern is the enhanced effect from extra greenhouse gases, which raises average temperatures.

Quick check

How it traps heat

?Which radiation do greenhouse gases mainly absorb and re-radiate to warm the lower atmosphere?
Human activities · 4.9.2.2

Adding more greenhouse gases

Some human activities increase the amount of greenhouse gases in the air:

  • Burning fossil fuels → more carbon dioxide.
  • Deforestation → fewer trees to remove CO₂ by photosynthesis, so more CO₂ stays in the air.
  • Agriculture / livestock (e.g. cattle and rice paddy fields) → more methane.
  • Landfill → decomposing waste releases methane.

Exam tip: AQA wants two human activities for each gas. CO₂: burning fossil fuels & deforestation. Methane: livestock farming & landfill (also rice growing).

Based on peer-reviewed evidence, many scientists believe these extra gases will raise the temperature of the Earth's atmosphere at the surface, causing global climate change.

Match it

Activity → gas released

Tap an activity on the left, then tap the greenhouse gas it mainly increases.

Human activity
Gas increased
Evidence & uncertainty · 4.9.2.2

How sure are scientists?

Global climate is a hugely complex system with many variables, so scientists use simplified models. This means parts of the evidence can be uncertain, and media reports may be simplified, speculative or biased if they use only part of the evidence.

  • Peer review — other scientists check results before publication, which improves reliability.
  • You should be able to evaluate the quality of evidence in a climate report and describe the uncertainties in it.
  • Results should be communicated to a wide range of audiences.

Balanced view: there is a correlation between rising greenhouse gases and rising average global temperature, and most scientists link the two. Models simplify reality, so exact predictions carry uncertainty — that's normal in science, not a reason to dismiss the evidence.

Global climate change · 4.9.2.3

Potential effects

An increase in average global temperature is a major cause of climate change. You should be able to describe four potential effects and discuss their scale, risk and environmental implications:

  • Sea levels rise (melting ice and expanding water) → coastal flooding.
  • More frequent or severe extreme weather (storms, droughts, floods).
  • Changes to where species can live and to migration patterns (loss of habitats/biodiversity).
  • Changes to rainfall patterns affecting food production and water supply.

Stay measured: these are potential effects whose scale and timing carry uncertainty. The exam wants you to discuss risk and implications factually, not to exaggerate.

Carbon footprint · 4.9.2.4

Carbon footprint & reducing it

The carbon footprint is the total amount of carbon dioxide and other greenhouse gases emitted over the full life cycle of a product, service or event.

It can be reduced by cutting emissions of carbon dioxide and methane, for example:

  • Using renewable energy or more efficient processes instead of fossil fuels.
  • Carbon capture and storage; planting trees.
  • Government taxes / caps on emissions; reducing waste sent to landfill.

Why actions may be limited: cost, the need for global agreement, lack of public/political will, incomplete technology, and the difficulty of changing lifestyles can all hold back reductions.

Quick check

Lowering the footprint

?The carbon footprint of a product is the total greenhouse gas emitted over its full life cycle. Which action would reduce it?
Pollutants from fuels · 4.9.3.1

What burning fuels releases

Most fuels (including coal) contain carbon and/or hydrogen, and may contain some sulfur. Burning them is a major source of atmospheric pollutants:

  • Complete combustion (plenty of oxygen) → carbon dioxide + water vapour.
  • Incomplete combustion (not enough oxygen) → carbon monoxide (CO), soot (carbon particles) and unburned hydrocarbons.
  • The sulfur in the fuel burns to form sulfur dioxide (SO₂).
  • At high temperatures, nitrogen and oxygen in the air react to form oxides of nitrogen (NOₓ).
incomplete combustion → carbon monoxide → soot (particulates) → unburned HCs sulfur in fuel → sulfur dioxide SO₂ (plus NOₓ from the hot air) complete combustion → carbon dioxide → water vapour (needs plenty of O₂)

Misconception watch: complete combustion gives CO₂; incomplete combustion (too little oxygen) is what produces the toxic CO and soot.

Effects of pollutants · 4.9.3.2

Why each pollutant matters

  • Carbon monoxide (CO) — a toxic gas; colourless and odourless, so not easily detected.
  • Soot / particulates — cause global dimming and respiratory (health) problems.
  • Sulfur dioxide (SO₂) and oxides of nitrogen (NOₓ) — cause respiratory problems and acid rain.
CO toxic (colourless, odourless) particulates global dimming + breathing problems SO₂ & NOₓ acid rain + breathing problems
Quick check

Complete or incomplete?

?A faulty heater burns gas in a poor supply of oxygen. Which toxic gas is most likely to be produced?
Match it

Pollutant → effect

Tap a pollutant on the left, then tap its main effect on the right.

Pollutant
Main effect
Recap

The facts to know

Air today: ~78% N₂, ~21% O₂, small amounts of CO₂, water vapour & noble gases.

Early air: volcanoes → mainly CO₂; water vapour → oceans; little/no O₂.

O₂ up: photosynthesis (algae then plants). CO₂ down: oceans, photosynthesis, sedimentary rocks & fossil fuels.

Greenhouse gases: CO₂, methane, water vapour — absorb & re-radiate long-wavelength (IR) radiation.

More gases from: burning fossil fuels, deforestation (CO₂); livestock, landfill (methane).

Carbon footprint: total greenhouse gas over a full life cycle — reduce by cutting CO₂ & CH₄.

Pollutants: CO (toxic), particulates (global dimming + breathing), SO₂ & NOₓ (acid rain + breathing).

You've covered all of AQA 4.9 — composition & evolution, greenhouse gases & climate change, and atmospheric pollutants. Press Finish to see your score.

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You've worked through Chemistry of the Atmosphere for AQA GCSE Chemistry. 🎉

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