Course review

2.3 Biogeochemical cycles

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Learning objective

2.3.1—Biogeochemical cycles purpose

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• Ensure chemical elements remain available to living organisms • Human impact affects ecosystem sustainability

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Learning objective

2.3.2—Cycle components

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• Stores: equilibrium with environment • Sinks: net accumulation • Sources: net release

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Learning objective

2.3.3—Carbon stores

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• Organic: organisms, crude oil, natural gas • Inorganic: atmosphere, soils, oceans

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Learning objective

2.3.4—Carbon flows

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• Photosynthesis, feeding, defecation, respiration, death, decomposition

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Learning objective

2.3.5—Carbon sequestration

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• Capturing atmospheric CO₂ and storing as solid/liquid • Natural: trees absorb CO₂ → biomass • Fossilization into coal, oil, natural gas

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Learning objective

2.3.6—Ecosystems as carbon stores/sinks/sources

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• Sink: photosynthesis > respiration (e.g., young forest) • Store: balanced (e.g., mature forest) • Source: respiration > photosynthesis (e.g., forest fire)

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Learning objective

2.3.7—Fossil fuels as carbon stores

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• Fossil fuels are stores of carbon with unlimited residence times • They were formed when ecosystems acted as carbon sinks in past eras and become carbon sources when burned • Consider: the concept of fossil fuels but not the detail of how and when coal, oil and natural gas were formed

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Learning objective

2.3.8—Agriculture as carbon store/source/sink

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• Agricultural systems can act as carbon stores, sources and sinks, depending on the techniques used • Regenerative agricultural methods, such as crop rotation, cover crops and no till, will promote the role of soil as a carbon sink whereas drainage of wetland, monoculture • Cropping over a longer timescale (e.g., timber production) and the subsequent use of harvested products will also affect these roles

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Learning objective

2.3.9—Ocean carbon exchange

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• Carbon dioxide is absorbed into the oceans by dissolving and is released as a gas when it comes out of a solution • While oceans act as a carbon sink, the human use of fossil fuels releases inorganic carbon at a faster rate than oceans can absorb it

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Learning objective

2.3.10—Ocean acidification

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• Increases in concentrations of dissolved carbon dioxide cause ocean acidification, harming marine animals • Small decreases in pH can interfere with calcium carbonate deposition in mollusc shells and coral skeletons

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Learning objective

2.3.11—Alleviating carbon cycle impacts

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• Measures are required to alleviate the effects of human activities on the carbon cycle • Consider at least three required measures • These include low-carbon technologies, reduction in fossil-fuel burning/soil disruption/deforestation, carbon capture through reforestation and artificial sequestration

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