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097e145
NotesESS HLTopic 2.3The Nitrogen Cycle (HL only)
Back to ESS HL Topics
2.3.31 min read

The Nitrogen Cycle (HL only) (ESS HL)

IB Environmental Systems and Societies • Unit 2

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Contents

  • The Nitrogen Cycle — Stores and Flows
  • Biological Nitrogen Fixation
  • The Haber Process
  • Nitrogen and Planetary Boundaries
  • Exam-style question (step by step)
Big picture: Nitrogen is essential for all living organisms (found in amino acids, proteins, DNA). Although 78% of the atmosphere is N2, most organisms cannot use it directly — it must first be fixed into reactive forms.
Nitrogen fixation
Conversion of atmospheric N2 into ammonia (NH3) or ammonium (NH4+) by nitrogen-fixing bacteria or lightning. This makes nitrogen available to plants.
Nitrification
Conversion of ammonium (NH4+) to nitrite (NO2-) and then nitrate (NO3-) by nitrifying bacteria (Nitrosomonas and Nitrobacter). Occurs in aerobic conditions.
Assimilation
The uptake of nitrate (NO3-) or ammonium (NH4+) by plants through their roots, incorporating nitrogen into organic molecules.
Ammonification
The decomposition of organic nitrogen (dead organisms, waste) back into ammonium (NH4+) by decomposing bacteria and fungi.
Denitrification
Conversion of nitrate (NO3-) back to N2 or N2O gas by denitrifying bacteria in anaerobic (waterlogged) conditions. Returns nitrogen to the atmosphere.

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Types of nitrogen-fixing organisms

  • Rhizobium bacteria — live in root nodules of leguminous plants (mutualistic symbiosis)
  • Cyanobacteria (blue-green algae) — fix nitrogen in aquatic environments and soil crusts
  • Free-living soil bacteria (e.g., Azotobacter) — fix nitrogen independently
  • Lightning — converts small amounts of N₂ to NO₃⁻ in the atmosphere
Key concept: Biological nitrogen fixation is the largest natural source of reactive nitrogen. Legume-Rhizobium symbiosis is a classic example of mutualism: the bacteria receive sugars from the plant, and the plant receives usable nitrogen.
IB exam tip: Draw and label the nitrogen cycle showing all five processes: fixation, nitrification, assimilation, ammonification, and denitrification. Include the bacteria responsible for each step.

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Key concept: The Haber process (developed 1909) industrially converts atmospheric N2 into ammonia (NH3) using high temperature and pressure. It has doubled the amount of reactive nitrogen entering ecosystems globally.

The Haber process

  • Reaction: N2 + 3H2 → 2NH3 (requires ~450°C, ~200 atm, iron catalyst)
  • Uses natural gas (methane) as hydrogen source — energy-intensive
  • Produces ammonia for fertilisers, explosives, and industrial chemicals
  • Currently produces ~150 million tonnes of ammonia per year

Consequences of the Haber process

  • Enabled the Green Revolution — feeding billions through synthetic fertilisers
  • More than doubled global food production
  • Massively increased reactive nitrogen in the environment
  • Accounts for ~1–2% of global energy consumption
  • Human nitrogen fixation now exceeds natural fixation
Key concept: The planetary boundary for nitrogen has been exceeded. Human activities have more than doubled the amount of reactive nitrogen entering the biosphere, with severe consequences for ecosystems.

Consequences of excess reactive nitrogen

  • Eutrophication of freshwater and marine ecosystems
  • Dead zones in coastal waters (e.g., Gulf of Mexico)
  • Nitrous oxide (N2O) emissions — a potent greenhouse gas
  • Acid deposition from nitrogen oxides
  • Loss of biodiversity in nitrogen-sensitive ecosystems
  • Groundwater contamination with nitrates

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IB-style question — Carbon fluxes: sources vs sinks

Outline four transfers of carbon that affect the amount of carbon dioxide held in the atmosphere. Include transfers that both increase and decrease the atmospheric store. [4]

How to answer it, step by step

  1. Transfers that LOWER atmospheric CO₂

    • Photosynthesis: producers absorb CO₂ → organic molecules (atmosphere → biotic store).

    • Ocean dissolution: CO₂ dissolves in seawater, fixed by marine producers (atmosphere → ocean store).
  2. Transfers that RAISE atmospheric CO₂

    • Respiration: organisms release CO₂ (biotic store → atmosphere).

    • Combustion of fossil fuels: releases ancient locked carbon (lithospheric store → atmosphere).

Final answer

Every answer must state direction — 'from X to atmosphere' or 'atmosphere to X'. Naming a process without direction earns 0. Include at least one that lowers AND one that raises the atmospheric store.

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one reason why most organisms cannot use atmospheric nitrogen directly. [2 marks]

Related ESS HL Topics

Continue learning with these related topics from the same unit:

2.1.1Organisms and species
2.1.2 Identification of Organisms
2.1.3Populations
2.1.4Communities & ecosystems
View all ESS HL topics

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Human Impacts on the Nitrogen Cycle (HL only)2.3.4

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