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C9 Atm ChemistryAQA GCSE Chemistry · 8462 (Triple)

Earth's Atmosphere

History and composition of the atmosphere, evolution over time, evidence for changes.

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CognitoEarth's atmosphere — evolution and composition
Key facts & methods

Current composition of the atmosphere — fill in the table

Gas% of atmosphere
Nitrogen (N2)
Oxygen (O2)
Argon (Ar)
Carbon dioxide (CO2)
Water vapour
Noble gases (He, Ne, Kr, Xe)

Evolution of the atmosphere — fill in the table

StageWhat happened
4.6 billion years ago
Volcanic activity
Water vapour condensed
Photosynthesis
Nitrogen

Evidence for atmosphere changes — fill in the table

EvidenceWhat it shows
Carbonate rocks (limestone)
Iron-banded formations
Fossils of early photosynthetic organisms
Gas bubbles in ancient ice cores
Mathematical models

Role of key processes — fill in the table

ProcessEffect
Photosynthesis
Respiration and combustion
Dissolution in oceans
Formation of fossil fuels
Maintaining current balance
Exam questions — 4 questions · 10 marks · AQA 8462 style
⚡ Show all working — the AI marks against the AQA mark scheme. Method marks awarded for correct working even if the final answer is wrong.
1 markAtmosphere compositionAQA 8462 style

Approximately what percentage of the current atmosphere is nitrogen?

A 21%
B 50%
C 78%
D 100%
3 marksEvolution of atmosphereAQA 8462 P1 style

Explain how the level of oxygen in the atmosphere increased over billions of years. (3 marks)

Hint: Start with: early atmosphere had no O2. Explain: photosynthesis by early organisms produced O2. Over billions of years O2 accumulated.
+30 XP
1 markCO2 decreaseAQA 8462 style

Which of the following is NOT a reason why CO2 levels decreased in the early atmosphere?

A CO2 dissolved in oceans
B Photosynthesis removed CO2
C CO2 was converted to oxygen by volcanic activity
D Formation of carbonate rocks (limestone) locked up carbon
3 marksRole of oceansAQA 8462 style

Explain how the formation of oceans helped reduce the level of CO2 in the early atmosphere. (3 marks)

Hint: Chain: water vapour condenses → oceans form → CO2 dissolves in ocean water → carbonate rocks form → CO2 removed from atmosphere.
+30 XP
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