How do carbon and nitrogen cycle between organisms, the atmosphere, the oceans and the rocks?
The processes that move carbon and nitrogen through the biosphere, atmosphere, hydrosphere and lithosphere, including photosynthesis, respiration, nitrogen fixation, nitrification, denitrification and decomposition.
A focused answer to AQA A-Level Environmental Science 3.1.3, covering the carbon cycle and nitrogen cycle, the key biological and physical processes that drive them, and how human activity disrupts each cycle.
Reviewed by: AI editorial process; not yet individually human-reviewed
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What this dot point is asking
AQA wants you to describe the carbon cycle and the nitrogen cycle, name and explain the key processes (photosynthesis, respiration, combustion, nitrogen fixation, nitrification, denitrification and decomposition), and explain how human activity disturbs each cycle. The most-rewarded skill is stating the direction of each conversion correctly, since this is where most marks are lost.
The carbon cycle
Carbon moves between several stores through clearly defined fluxes:
- Photosynthesis removes carbon dioxide from the atmosphere and fixes it into organic compounds (glucose, then biomass) in plants and algae.
- Respiration by all organisms (plants, animals, decomposers) breaks down organic compounds and returns carbon dioxide to the atmosphere.
- Decomposition of dead matter releases carbon dioxide as decomposers respire.
- Combustion of fossil fuels, wood and other biomass releases carbon dioxide.
- Ocean exchange: carbon dioxide dissolves in seawater and is used by marine organisms; some forms carbonate shells.
- Long-term stores include fossil fuels, carbonate rocks such as limestone, and the deep oceans, which hold carbon for millions of years.
The nitrogen cycle
Atmospheric nitrogen gas () makes up about 78 percent of the air but is very unreactive because of its strong triple bond, so it must be converted into usable forms before organisms can use it to build proteins and DNA.
Decomposition (ammonification) by decomposers releases nitrogen from dead organisms and waste as ammonium, recycling it back into the soil. Plants absorb nitrate (and some ammonium) through their roots, build it into amino acids and proteins, and pass it along food chains. The cycle therefore links the atmosphere, soil, microbes, plants and animals, and depends heavily on bacteria at almost every step.
Human disruption of the cycles
- Burning fossil fuels and clearing forests raise atmospheric carbon dioxide, enhancing the greenhouse effect and driving climate change; deforestation also removes a carbon sink.
- Heavy use of nitrogen fertilisers adds large amounts of reactive nitrogen to soils; runoff into rivers and lakes causes eutrophication, algal blooms and oxygen depletion.
- The Haber process and combustion engines add reactive nitrogen compounds (including nitrogen oxides) to the environment, contributing to acid rain and smog.
- Drainage and ploughing can speed decomposition of soil organic matter, releasing stored carbon.
Try this
Q1. Name the process that converts atmospheric nitrogen into ammonium and give two ways it occurs. [3 marks]
- Cue. Nitrogen fixation, by nitrogen-fixing bacteria (free-living or in legume nodules), lightning, or the Haber process (any two).
Q2. Explain how burning fossil fuels disrupts the carbon cycle and why this raises atmospheric carbon dioxide. [3 marks]
- Cue. It moves carbon from long-term geological stores to the atmosphere faster than photosynthesis and ocean uptake remove it, so the input exceeds removal and concentration rises.
Q3. Explain why growing a legume crop in a rotation can reduce the need for nitrogen fertiliser. [2 marks]
- Cue. Legumes host nitrogen-fixing Rhizobium in root nodules, adding fixed nitrogen to the soil and replenishing fertility naturally.
Exam-style practice questions
Practice questions written in the style of AQA exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
AQA 20196 marksDescribe the roles of nitrogen fixation, nitrification and denitrification in the nitrogen cycle, and explain why crop rotation with legumes can improve soil fertility.Show worked answer →
A 6-mark answer needs the three named processes plus the applied legume reasoning.
- Nitrogen fixation
- Atmospheric nitrogen gas is very unreactive (a strong triple bond), so it must be converted to usable forms. Nitrogen-fixing bacteria (free-living in soil, or Rhizobium in the root nodules of legumes) and lightning convert nitrogen gas to ammonia or ammonium; the Haber process does it industrially for fertiliser.
- Nitrification
- Nitrifying bacteria in well-aerated soil oxidise ammonium first to nitrite and then to nitrate. Nitrate is the main form plants absorb through their roots.
- Denitrification
- In waterlogged, anaerobic soils, denitrifying bacteria reduce nitrate back to nitrogen gas, returning it to the atmosphere and lowering soil fertility.
- Legume rotation
- Legumes (peas, beans, clover) host nitrogen-fixing Rhizobium in root nodules, adding fixed nitrogen to the soil. Rotating a legume crop with other crops replenishes soil nitrogen naturally, reducing the need for artificial fertiliser and maintaining fertility.
Markers reward correct direction of each conversion (fixation: gas to ammonium; nitrification: ammonium to nitrate; denitrification: nitrate to gas), the role of bacteria, and the legume nodule link.
AQA 20214 marksExplain how burning fossil fuels and clearing forests both disrupt the carbon cycle, and explain why this raises atmospheric carbon dioxide.Show worked answer →
A 4-mark answer needs both human activities linked to the carbon balance.
- Burning fossil fuels
- Fossil fuels are a long-term geological carbon store. Combustion transfers this carbon to the atmosphere as carbon dioxide, adding carbon that was locked away for millions of years much faster than natural processes can remove it.
- Clearing forests
- Forests are a large carbon store and remove carbon dioxide by photosynthesis. Cutting and burning trees releases their stored carbon and removes the future photosynthetic uptake (the carbon sink), so less carbon dioxide is taken out of the air.
- Why carbon dioxide rises
- Both activities increase inputs to the atmosphere and (for deforestation) reduce removal, so the flux of carbon dioxide into the atmosphere exceeds the flux out by photosynthesis and ocean uptake, and concentration rises, enhancing the greenhouse effect.
Markers reward (1) fossil fuels as a long-term store released by combustion, (2) forests as both a store and a sink, and (3) the imbalance between input and removal raising concentration.
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Sources & how we know this
- AQA A-level Environmental Science (7447) specification — AQA (2017)