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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Learning objective

2.3.12 (HL)—Lithosphere carbon stores

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• The lithosphere contains carbon stores in fossil fuels and in rocks, such as limestone, that contain calcium carbonate • The residence time for carbon in these stores can be hundreds of millions of years

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Learning objective

2.3.13 (HL)—Carbonate fossilization

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• Reef-building corals and molluscs have hard parts that contain calcium carbonate that can become fossilized in limestone • Limestone is the largest store of carbon in Earth systems • Not all limestone is formed by fossilization of animal remains; it can also be formed by both biological and non-biological processes • Details of these processes are not required

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Learning objective

2.3.14 (HL)—Fossil fuel formation

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• In past geological eras, organic matter from partially decomposed plants became fossilized in coal, and partially decomposed marine organisms became fossilized in oil • Formation of coal, oil and gas was greatest in specific geological eras when conditions were most suitable

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Learning objective

2.3.15 (HL)—Methane production

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• Methane is produced from dead organic matter in anaerobic conditions by methanogenic bacteria

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Learning objective

2.3.16 (HL)—Methane cycle

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• Residence time: ~10 years in atmosphere • Oxidized to CO₂ • Potent greenhouse gas

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Learning objective

2.3.17 (HL)—Nitrogen cycle stores

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• Organic: proteins in organisms and dead matter • Inorganic: atmospheric N₂, ammonia, nitrites, nitrates

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Learning objective

2.3.18 (HL)—Bacterial roles in nitrogen cycle

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• Nitrogen fixation: N₂ → ammonia • Nitrification: ammonia → nitrates • Denitrification: nitrates → N₂ • Decomposition: amino acids → ammonium

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Learning objective

2.3.19 (HL)—Denitrification conditions

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• Only in anaerobic conditions (waterlogged soils) • Insectivorous plants use insects as nitrogen source

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Learning objective

2.3.20 (HL)—Plant nitrogen fixation

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• Plants cannot fix nitrogen • Require mutualistic associations with nitrogen-fixing bacteria

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Learning objective

2.3.21 (HL)—Nitrogen cycle flows

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• Mineral uptake, photosynthesis, consumption, excretion, death, decomposition, ammonification

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Learning objective

2.3.22 (HL)—Human impacts on nitrogen cycle

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• Deforestation, agriculture, aquaculture, urbanization

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Learning objective

2.3.23 (HL)—Haber process

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• Industrial production of ammonia for fertilizer • From nitrogen and hydrogen

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Learning objective

2.3.24 (HL)—Nitrogen planetary boundary

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• Exceeded due to human activities • Nitrate increases in biosphere • Major cause: inorganic fertilizers for crops

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Learning objective

2.3.25 (HL)—Global collaboration needed

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• Address uncontrolled nitrogen use • Bring nitrogen cycle within planetary boundaries

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