ga-alevel-wc-geography-matters-carbon-cycle-bundle
GA Post-16 and HE Phase Committee
The Carbon Cycle articles compiled for the Geography Matters newsletter to assist teachers in A-level planning (2016).
Full content available at: www.geography.org.uk/cpdevents/curriculum/geographymatters
Contents Overview
Starting to teach the carbon cycle – Helen Hore (2015)
Climate change and development in the Tonlé Sap Region, Cambodia – Emma Rawlings Smith (2015)
Iceland – innovations in green energy production – Emma Rawlings Smith (2014)
Global climate change and water supplies: the winners and losers – Emma Rawlings Smith (2010)
Starting to Teach the Carbon Cycle (Helen Hore, 2015)
Importance: An essential topic in Geography A Level linked to the water cycle.
Key Content:
Distribution and size of major carbon stores: Land, oceans, and atmosphere.
Driving factors changing the magnitude and cycling processes within carbon stores.
Climate context exploring links between carbon and water cycles.
Significance for Students:
Understanding these cycles aids in evaluating conflicting media views on climate change and carbon manipulation.
Relevant current topics include Japan's drilling for offshore methane hydrates, linking geography and environmental issues.
Global Stores and Transfers of Carbon
Starting Point for Discussion:
Introduce carbon stores (reservoirs) and transfers (fluxes), utilizing prior science knowledge.
Figures:
Major carbon stores (in Gtons) include:
Atmosphere: 720 (CO2, CH4)
Ocean Surface: 620 (dissolved CO2)
Ocean Deep: 36,730 (dissolved CO2, CaCO3)
Lithosphere: >60,000,000 (CaCO3 in limestone)
Biosphere (living): 600-1,000 (sugars, starches)
Dead Organic Matter: 1,200 (soil humus)
Fossil Fuels: 4,000 (hydrocarbons)
Volume of Transfers:
Photosynthesis: 120 Gt/year
Respiration: 120 Gt/year
Emissions from human activities: 9 Gt/year
Increases (red numbers) in CO2 due to human activity highlighted.
Natural Processes in the Carbon Cycle
Variability in Carbon Stores:
Residence time varies: Fast carbon cycles (minutes/hours) vs. slow cycles (millennia).
Rapid Cycles:
Carbon recycled quickly through atmospheric exchanges and photosynthesis; biomass stores carbon.
Slower Cycles:
Decomposition processes recycle carbon into soil; natural wildfires can release carbon quickly.
Very Slow Cycles:
Burial and weathering processes release CO2 from sediments over millions of years:
Fossil fuels result from anaerobic conditions; formation involves woody material and planktonic matter.
Carbon Sources:
Volcanoes also contribute CO2 emissions, albeit much less than fossil fuel combustion.
Methane hydrates as a significant and stable reservoir.
Human Processes Impacting Carbon Cycle
Deforestation:
Alters global carbon biomass; the difficulty in estimating CO2 release post-regrowth.
Energy Use:
Fossil fuel combustion remains the primary contributor to increased atmospheric carbon.
Historical data on CO2 emissions illustrates growth from 5.5 billion tons in the 1980s to 8.7 billion in 2008.
Inquiry Starting Point:
Consider in teaching: "What part do people play in the carbon cycle?"
Teaching Tools
Explore relational maps between carbon stores and flows.
Discuss overlapping roles of hydrosphere, biosphere and lithosphere using time scale comparisons.
Use scenario questions to generate discourse about human activity and climatic impacts.
References
Several resources listed for further exploration on the carbon cycle and associated research.