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AQA GCSE Chemistry Smart practice A mixed round aimed at your weak spots
Unit 1
Atomic structure and the periodic table
Unit 2
Bonding, structure, and the properties of matter
Unit 3
Quantitative chemistry
Unit 4
Chemical changes
Unit 5
Energy changes
Unit 6
The rate and extent of chemical change
Unit 7
Organic chemistry
Unit 8
Chemical analysis
Unit 9
Chemistry of the atmosphere
Unit 10
Using resources
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How carbon dioxide decreased

Practise 18 exam-style questions on How carbon dioxide decreased for AQA GCSE Chemistry. Write your answer as you would in the exam and get it marked in seconds against the mark scheme, point by point, with an AI tutor on hand if you get stuck.

  • 18 questions
  • 1–6 marks each
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18 questions, marked as you go

Sample questions with model answers

Here are 4 of the questions in this topic, each with a model answer, an explanation of why it earns the marks and the mark scheme an examiner would use.

Question 1

2 marks

Scientists think that the Earth's early atmosphere was mainly carbon dioxide. Today the atmosphere contains only about 0.04% carbon dioxide.

Give two reasons why the percentage of carbon dioxide in the atmosphere decreased.

Model answer

Algae and plants removed carbon dioxide from the atmosphere by photosynthesis. Carbon dioxide also dissolved in the oceans, where carbonates were precipitated and formed sedimentary rocks such as limestone.

Explanation

Several processes worked together: photosynthesis by algae and plants, dissolving in the oceans, the formation of carbonate sediments and rocks, and the burial of carbon in fossil fuels. Any two of these earn the marks. Animals breathing does not remove carbon dioxide - respiration releases it.

Mark scheme
  1. 1 mark

    photosynthesis by algae and plants

    max 2; allow 'used by plants to make glucose'

  2. 1 mark

    carbon dioxide dissolved in the oceans

    allow 'absorbed by the sea'

  3. 1 mark

    formation of sedimentary rocks / carbonates were precipitated to form sediments / limestone formed

    allow locked up in shells and skeletons of marine organisms

  4. 1 mark

    formation of fossil fuels (coal, crude oil, natural gas) that contain carbon

    ignore 'used by animals'; ignore 'reacted with oxygen'

Question 2

2 marks

Burning fossil fuels today is sometimes described as 'returning ancient carbon dioxide to the atmosphere'.

Explain why.

Model answer

The carbon in coal, crude oil and natural gas came from carbon dioxide that ancient plants and plankton removed from the atmosphere millions of years ago. When the fuels burn, the carbon combines with oxygen and is released into the atmosphere as carbon dioxide again.

Explanation

Fossil fuels are a store of carbon taken out of the atmosphere long ago. Combustion reverses that storage in a very short time, adding carbon dioxide to the atmosphere much faster than it was removed.

Mark scheme
  1. 1 mark

    the carbon in fossil fuels came from carbon dioxide removed from the atmosphere millions of years ago

    allow by photosynthesis of ancient plants / algae / plankton

  2. 1 mark

    combustion converts the carbon in the fuel back into carbon dioxide (which is released into the atmosphere)

    allow burning releases carbon dioxide

Question 3

3 marks

Coral reefs are built by tiny marine animals that make hard skeletons from calcium carbonate. Over millions of years, the remains of old reefs can become limestone.

Explain how the growth of coral reefs removes carbon dioxide from the atmosphere.

Model answer

Carbon dioxide from the atmosphere dissolves in sea water. The coral animals use the dissolved carbon to build skeletons of calcium carbonate. When the animals die their skeletons are buried and compressed into limestone, so the carbon is locked away in rock for millions of years instead of returning to the atmosphere.

Explanation

This is the same process that formed limestone from the early atmosphere's carbon dioxide. The carbon moves from the air, into the sea, into calcium carbonate skeletons and finally into sedimentary rock.

Mark scheme
  1. 1 mark

    carbon dioxide from the atmosphere dissolves in sea water

    max 3

  2. 1 mark

    the coral animals use the dissolved carbon dioxide / carbonate to make calcium carbonate skeletons

  3. 1 mark

    when they die the skeletons are buried and compressed to form limestone / sedimentary rock, so the carbon is stored for millions of years

    allow carbon locked up in rock

  4. 1 mark

    more carbon dioxide then dissolves from the atmosphere to replace what was used

Question 4

4 marks

The graph shows one estimate of how the percentage of carbon dioxide in the Earth's atmosphere changed after the Earth formed.

Describe how the percentage of carbon dioxide changed over the time shown and give two reasons for this change.

Line graph of carbon dioxide in atmosphere in % (y-axis, 0 to 100) against time since the Earth formed in billion years (x-axis, 0 to 4.5). The line is a smooth curve through (0.5, 95), (1, 88), (1.5, 70), (2, 40), (2.5, 18), (3, 7), (3.5, 3), (4, 1), (4.5, 0).

Model answer

The percentage of carbon dioxide decreased from about 95% to almost 0%. It fell slowly at first, then fastest between about 1.5 and 2.5 billion years after the Earth formed, and then levelled off close to zero. It decreased because carbon dioxide dissolved in the oceans and was precipitated as carbonates, and because algae and plants removed it by photosynthesis.

Explanation

When describing a graph, give the overall trend with values and say how the rate changed. The reasons are the processes that removed carbon dioxide: dissolving in oceans, carbonate sediments, photosynthesis and fossil fuel formation.

Mark scheme
  1. 1 mark

    decreased overall from about 95% to almost 0%

    must quote data; allow start value 90-95%

  2. 1 mark

    decreased slowly at first, fastest between about 1.5 and 2.5 billion years, then levelled off

    any correct description of how the rate of decrease changed

  3. 1 mark

    photosynthesis by algae and plants

    max 2 marks for reasons

  4. 1 mark

    carbon dioxide dissolved in the oceans

  5. 1 mark

    carbonates precipitated / formation of sedimentary rocks such as limestone

  6. 1 mark

    carbon locked up in fossil fuels

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