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Understanding the Carbon Cycle and Energy Security

May 4, 2025

Edexcel Geography A-level

The Carbon Cycle and Energy Security

Geological Carbon Cycle

  • Movement and storage of carbon between land, ocean, and atmosphere.
  • Three forms of carbon:
    • Inorganic: Rocks as bicarbonates and carbonates.
    • Organic: Plant material and living organisms.
    • Gaseous: CO₂ and CH₄ (methane).
  • Balance between production and absorption (sources and sinks).

Stores of Carbon

  • Terrestrial, Oceanic, Atmospheric stores.
  • Carbon sink: Stores more carbon than it emits (e.g., intact tropical rainforest).
  • Carbon source: Emits more carbon than it stores (e.g., damaged rainforest).

Main Carbon Stores:

  • Marine Sediments & Sedimentary Rocks: Largest store, 66,000-100,000 million billion metric tons.
  • Oceans: 38,000 billion metric tons.
  • Fossil Fuel Deposits: 4000 billion metric tons.
  • Soil Organic Matter: 1500 billion metric tons.
  • Atmosphere: 750 billion metric tons.
  • Terrestrial Plants: 560 billion metric tons.

Fluxes of Carbon Cycle

  • Photosynthesis: Converts CO₂ and water into oxygen and glucose.
  • Respiration: Converts oxygen and glucose into energy, water, and CO₂.
  • Combustion: Fossil fuels and organic matter burn, releasing CO₂.
  • Decomposition: Decomposers break down organisms, releasing CO₂.
  • Diffusion: Oceans absorb CO₂, increasing acidity.
  • Sedimentation: Formation of limestone from shell fragments.
  • Weathering & Erosion: Releases inorganic carbon slowly.
  • Metamorphosis & Volcanic Outgassing: Releases CO₂ from Earth's crust.

Variations in Carbon Fluxes

  • Quick cycle: Photosynthesis and respiration.
  • Long-term storage: Dead organic material turns into sedimentary rocks or hydrocarbons.

Complex Carbon Processes

  • Ocean as Carbon Sink: Stores 50x more carbon than the atmosphere.
  • Biological Carbon Pump: Phytoplankton photosynthesise, base of marine food web.
  • Physical Pump: CO₂ saturation in ocean surface layer, thermohaline circulation.

Terrestrial Sequestration

  • Primary producers (plants) sequester carbon via photosynthesis.
  • Decomposition in tropical climates quickly recycles carbon.
  • Diurnal and seasonal variations in carbon flux.

Soil's Capacity to Store Carbon

  • Climate, soil type, and land use affect carbon storage.

The Natural Greenhouse Effect

  • CO₂ levels maintain global temperatures.

Anthropogenic Interference

Enhanced Greenhouse Effect

  • Increase in greenhouse gases since the 1750s.
  • Major contributors: Fossil fuels, deforestation, urbanization.

Implications

  • Temperature, climate, and precipitation changes.
  • Severe weather, ecosystem shifts, hydrological cycle impacts.

Energy Security

Key Concepts

  • Maximum energy security: Uninterrupted energy at affordable prices.
  • Four aspects: Availability, Accessibility, Affordability, Reliability.
  • Energy security evaluated at national level.

Energy Mix

  • Non-renewable: Fossil fuels like coal, oil, natural gas.
  • Renewable: Solar, wind, geothermal.
  • Recyclable: Nuclear energy.

Primary Energy Sources

  • Coal, oil, natural gas, uranium, biomass, hydroelectric power.

Energy Players

  • TNCs play a major role in energy exploration, exploitation, distribution.
  • OPEC: Controls majority of world oil reserves.
  • National governments and consumers influence energy security.

Alternative Energy Sources

  • Unconventional fossil fuels: Shale gas, deep-water oil, tar sands.
  • Renewable energy: Solar, wind, wave, tidal, geothermal.

Reducing Carbon Emissions

Strategies

  • Carbon Capture and Storage (CCS).
  • Hydrogen fuel cells as alternative to oil.

Threats to Water and Carbon Cycle

Deforestation

  • Reduces carbon storage, increases flooding risk.

Grassland Conversion

  • Converts carbon sinks into carbon sources.

Ocean Health

  • Overfishing and acidification impact economy and biodiversity.

Climate Change Impacts

  • Severe weather, rising sea levels, ecosystem changes.

Tipping Points

  • Forest die-back, thermohaline circulation disruption.