AQA GCSE Chemistry coverage

Chemistry of the atmosphere

Section 4.9
10 spec leafs

Notes and three levels of exam-style practice for each registered specification leaf in this section.

Open the printable pack
4.9.1.1

The proportions of different gases in the atmosphere

  • For about 200 million years, air has contained approximately 80% nitrogen and 20% oxygen, with much smaller proportions of carbon dioxide, noble gases and water vapour.
  • Use a percentage as a fraction of 100: volume of a gas =(percentage/100)×total volume=(\text{percentage}/100)\times\text{total volume}.
  • For example, a 350cm3350\,\text{cm}^3 air sample contains about 0.20×350=70cm30.20\times350=70\,\text{cm}^3 of oxygen.
  • The 80:20 split is an approximation: nitrogen and oxygen do not make exactly 100%, and the proportion of water vapour varies.

Tier 1 · Easy

1 mark
ORIGINAL

Estimate the volume of oxygen in a 240cm3240\,\text{cm}^3 sample of air.

Tier 2 · Standard

2 marks
ORIGINAL

A weather balloon contains 2.5dm32.5\,\text{dm}^3 of air. Estimate the volumes of nitrogen and oxygen in the balloon.

Tier 3 · Hard

4 marks
ORIGINAL

A student passes an air sample over a substance that removes oxygen. Its volume falls from 480480 to 386cm3386\,\text{cm}^3. Calculate the percentage of the original sample that was oxygen and compare it with the accepted approximate value.

4.9.1.2

The Earth's early atmosphere

  • Theories of the early atmosphere have changed and developed as evidence has been interpreted; one theory proposes that intense volcanic activity released the gases that formed it.
  • The atmosphere may initially have resembled those of Mars and Venus today: mainly carbon dioxide, with little or no oxygen; volcanic nitrogen accumulated, and small proportions of methane and ammonia may also have been present.
  • As the Earth cooled, volcanic water vapour condensed to form oceans; carbon dioxide then dissolved and carbonates precipitated as sediments, lowering its atmospheric proportion.
  • Evidence from 4.6 billion years ago is limited, so this is a supported theory rather than a certain, directly observed account; detailed knowledge of other theories is not required.

Tier 1 · Easy

1 mark
ORIGINAL

Name the gas thought to have made up most of the Earth's early atmosphere.

Tier 2 · Standard

3 marks
ORIGINAL

Explain how volcanic activity and cooling could produce an early atmosphere and then oceans.

Tier 3 · Hard

4 marks
ORIGINAL

A report claims that the exact composition of the atmosphere 4.6 billion years ago is known because modern volcanoes release carbon dioxide and water vapour. Evaluate this claim.

4.9.1.3

How oxygen increased

  • Algae and plants released oxygen by photosynthesis: carbon dioxide and water form glucose and oxygen using light energy.
  • Link the biological timeline: algae began producing oxygen about 2.7 billion years ago, oxygen then appeared in the atmosphere, and later plants increased its proportion further.
  • Photosynthesis simultaneously removes carbon dioxide and supplies oxygen, so a growth in photosynthetic organisms changes both gases in opposite directions.
  • Do not attribute the oxygen rise to volcanoes: in this model the sustained increase came from algae and plants, eventually allowing animals to evolve.

Tier 1 · Easy

1 mark
ORIGINAL

Name the process by which algae first increased atmospheric oxygen.

Tier 2 · Standard

3 marks
ORIGINAL

Explain why a large increase in photosynthetic organisms changes the proportions of both oxygen and carbon dioxide in the atmosphere.

Tier 3 · Hard

4 marks
ORIGINAL

A model shows atmospheric oxygen rising from 0.20% to 8.6%0.20\%\text{ to }8.6\% during a period when algae spread widely. Calculate how many times greater the final percentage is and explain why the data are consistent with the accepted account of atmospheric change.

4.9.1.4

How carbon dioxide decreased

  • Atmospheric carbon dioxide decreased because algae and plants used it in photosynthesis and because it dissolved in the oceans.
  • Trace where the carbon went: dissolved carbon dioxide contributed to carbonate sediments and limestone, while carbon in organisms was eventually locked into fossil fuels.
  • Coal formed mainly from buried plant material; crude oil and natural gas formed mainly from buried remains of marine organisms over millions of years.
  • A common error is to say carbon disappeared: it was transferred into biomass, sedimentary rocks and fossil fuels rather than destroyed.

Tier 1 · Easy

1 mark
ORIGINAL

State one process carried out by plants that lowered atmospheric carbon dioxide.

Tier 2 · Standard

4 marks
ORIGINAL

Explain two routes by which carbon from the early atmosphere became stored for long periods.

Tier 3 · Hard

5 marks
ORIGINAL

Compare the formation of limestone, coal, and crude oil or natural gas, and explain how each contributed to a lower proportion of atmospheric carbon dioxide.

4.9.2.1

Greenhouse gases

  • Water vapour, carbon dioxide and methane are greenhouse gases that maintain a temperature on Earth high enough to support life.
  • Describe the greenhouse effect by wavelength: short-wavelength radiation from the Sun reaches and warms the surface, which emits longer-wavelength infrared radiation.
  • Greenhouse-gas molecules absorb some outgoing long-wavelength radiation and re-emit it in all directions, reducing the rate at which energy escapes to space.
  • Do not confuse the greenhouse effect with ozone depletion, and do not claim that greenhouse gases stop all radiation from leaving Earth.

Tier 1 · Easy

2 marks
ORIGINAL

Name two greenhouse gases present in the Earth's atmosphere.

Tier 2 · Standard

3 marks
ORIGINAL

Describe how short-wavelength and long-wavelength radiation are involved in the greenhouse effect.

Tier 3 · Hard

4 marks
ORIGINAL

Explain why increasing the concentration of carbon dioxide can raise the Earth's average surface temperature even though sunlight can still enter the atmosphere.

4.9.2.2

Human activities which contribute to an increase in greenhouse gases in the atmosphere

  • Burning fossil fuels and deforestation increase atmospheric carbon dioxide; livestock farming, rice cultivation, landfill and decay of organic waste can increase methane.
  • For a recall question, give two distinct human activities for carbon dioxide and two for methane, linking each activity to the correct gas.
  • A strong climate-evidence evaluation checks sample size and duration, uncertainty, peer review, agreement with other data and whether the source communicates the full evidence.
  • A single weather event or a short local record cannot by itself establish a global climate trend; correlation also needs a scientifically plausible explanation.

Tier 1 · Easy

2 marks
ORIGINAL

Give one human activity that increases carbon dioxide and one that increases methane in the atmosphere.

Tier 2 · Standard

4 marks
ORIGINAL

State two human activities that increase atmospheric carbon dioxide and two that increase atmospheric methane.

Tier 3 · Hard

5 marks
ORIGINAL

An online article uses six years of temperatures from one town to claim that human activity cannot affect global climate. The article was written by an energy company, gives no uncertainty, and has not been peer reviewed. Evaluate the quality of this evidence.

4.9.2.3

Global climate change

  • An increase in average global temperature is a major cause of climate change, but the consequences differ between regions.
  • Use a cause-and-effect chain: warming can melt land ice and expand seawater, raise sea level, alter rainfall and extreme-weather patterns, and change habitats or species distributions.
  • For example, sea-level rise may increase coastal flooding, while changed rainfall may produce drought in one region and greater flood risk in another.
  • Do not present every projected effect as certain: discuss its scale, likelihood, risk and environmental implication using the evidence supplied.

Tier 1 · Easy

1 mark
ORIGINAL

State one potential effect of global climate change.

Tier 2 · Standard

3 marks
ORIGINAL

Explain how an increase in average global temperature can increase the risk of coastal flooding.

Tier 3 · Hard

5 marks
ORIGINAL

A coastal wetland supports rare birds and protects a nearby town from storm waves. Discuss the scale, risk and environmental implications if climate change raises sea level in this region.

4.9.2.4

The carbon footprint and its reduction

  • A carbon footprint is the total carbon dioxide and other greenhouse gases emitted across the full life cycle of a product, service or event.
  • Include raw materials, manufacture, transport, use and end-of-life when comparing footprints; omitting a stage can reverse a decision.
  • Footprints can be reduced through lower energy use, renewable energy, less travel, reduced waste, recycling, methane capture and changes in farming or diet.
  • Reductions may be limited by cost, available technology, infrastructure, public acceptance, convenience and incomplete or uncertain life-cycle data.

Tier 1 · Easy

2 marks
ORIGINAL

Define the carbon footprint of a product.

Tier 2 · Standard

4 marks
ORIGINAL

A music festival wants to reduce its carbon footprint. Describe two suitable actions and give one reason why each action may be limited.

Tier 3 · Hard

5 marks
ORIGINAL

A reusable product has life-cycle contributions of 18, 4, 30 and 2kg18,\ 4,\ 30\text{ and }2\,\text{kg} from manufacture, transport, use and disposal, respectively. A redesign adds 3kg3\,\text{kg} in manufacture but cuts transport emissions by 25%25\% and use emissions by 40%40\%. Calculate the new footprint and the percentage reduction.

4.9.3.1

Atmospheric pollutants from fuels

  • Burning carbon- and hydrogen-containing fuels can release carbon dioxide and water vapour; limited oxygen can also produce carbon monoxide, soot and unburned hydrocarbons.
  • Identify sulfur dioxide from sulfur impurities in a fuel, and oxides of nitrogen from nitrogen and oxygen reacting at the high temperatures inside engines.
  • Given a fuel's composition and conditions, first list its elements, then use oxygen supply and combustion temperature to predict the possible gaseous and particulate products.
  • Carbon monoxide and carbon dioxide are different products: carbon monoxide and soot indicate incomplete combustion, whereas complete combustion of carbon produces carbon dioxide.

Tier 1 · Easy

1 mark
ORIGINAL

Name the toxic gas formed when a carbon-containing fuel burns with too little oxygen.

Tier 2 · Standard

3 marks
ORIGINAL

A fuel contains carbon, hydrogen and a small amount of sulfur. It burns in excess oxygen. Predict three products released by combustion and identify the element responsible for each.

Tier 3 · Hard

5 marks
ORIGINAL

A 2.0kg2.0\,\text{kg} fuel sample contains 0.80% sulfur by mass. Assume every sulfur atom forms sulfur dioxide when the fuel burns. Calculate the mass of sulfur dioxide produced. Use Ar(S)=32A_r(\text{S})=32 and Ar(O)=16A_r(\text{O})=16.

4.9.3.2

Properties and effects of atmospheric pollutants

  • Carbon monoxide is toxic, colourless and odourless, so a dangerous concentration is not easily detected by human senses.
  • Sulfur dioxide and oxides of nitrogen cause respiratory problems and acid rain; connect each pollutant to both human-health and environmental effects when asked.
  • Particulates damage health and cause global dimming by reducing the amount of sunlight reaching the Earth's surface.
  • Do not assign global dimming to carbon dioxide or acid rain to soot: name the pollutant before explaining its specific effect.

Tier 1 · Easy

2 marks
ORIGINAL

Give two properties that make a carbon monoxide leak difficult for a person to detect.

Tier 2 · Standard

3 marks
ORIGINAL

Describe one effect of sulfur dioxide or oxides of nitrogen on humans, one effect on the environment, and one effect of particulates.

Tier 3 · Hard

5 marks
ORIGINAL

Near an industrial area, residents report breathing problems, a lake becomes more acidic, and less sunlight reaches the ground. Identify the likely pollutant groups and explain how the observations support your choices.