Geography
Carbon and water feedbacks
- 1.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Distinguish a carbon store from a carbon flux using this case.
[2 marks] · no calculatorAnswer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- A store is an amount, whereas a flux is a transfer per unit time. The annual figures cannot alone tell us the peatland's total existing carbon stock.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- Peat carbon accumulated at a time is a store.
- Annual uptake or respiration is a flux into or out of a store.
Examiner tip: Include a time basis when describing a flux.
- 2.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Calculate the annual change in carbon storage from the listed flows and state one limitation of interpreting it as a climate benefit.
[2 marks]Answer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- Treat uptake as input and the other listed transfers as outputs. The residual is stored carbon under the stated accounting assumptions; unmeasured methane prevents a complete climate balance.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- Storage change = 12 - 7 - 2 - 0 = +3 tonnes C/year.
- The listed carbon balance is a net gain, not a full greenhouse-gas assessment.
Examiner tip: Do not relabel tonnes C as tonnes CO2-equivalent.
- 3.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Explain why drainage can accelerate peat carbon loss.
[3 marks] · no calculatorAnswer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- Waterlogging restricts oxygen availability. Drainage removes that constraint and may also change fire susceptibility, linking the water system to carbon storage.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- Lower water tables expose more peat to air.
- Aerobic decomposition can increase carbon release through respiration.
- Drier peat can become more susceptible to combustion.
Examiner tip: Explain oxygen availability rather than saying water 'contains carbon'.
- 4.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Describe a positive feedback involving warming, peat drying and carbon release.
[3 marks] · no calculatorAnswer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- A feedback must return to its starting variable. Positive means amplification, not environmental benefit; the chain is conditional because rainfall and water management also matter.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- Warming can increase drying under suitable water-balance conditions.
- Drying can increase decomposition or fire emissions.
- Added greenhouse gases can reinforce warming, closing the feedback loop.
Examiner tip: A one-way list of impacts is not a complete feedback loop.
- 5.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Evaluate the claim that the +3 tonnes C balance proves restoration cools the climate.
[4 marks] · no calculatorAnswer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- Carbon storage is one component of mitigation evidence. Compare all relevant gases over an explicit time horizon and against what would have happened without restoration before making a net climate claim.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- A gain in stored carbon supports a sink within the listed accounting boundary.
- Unmeasured methane may affect net warming impact.
- A counterfactual drained-site balance and restoration emissions are needed.
- Makes a qualified judgement separating carbon mass from climate forcing.
Examiner tip: A carbon sink and a net cooling effect are related but not interchangeable claims.
- 6.
Fictional annual carbon accounting for a restored peatland: carbon uptake 12 tonnes C; respiration 7 tonnes C; exported organic carbon 2 tonnes C; fire loss 0. Use storage change = uptake minus listed losses. Methane emissions are not measured. A nearby drained peatland is drier. All quantities are invented; tonnes C are not tonnes CO2-equivalent. Assess a restoration plan that raises water levels but restricts nearby farming drainage.
[4 marks] · no calculatorAnswer explanation
Draft walkthroughs are based on marking guidance, not independently verified derivations.
- Restoration benefits can extend beyond the site while costs fall on particular neighbours. A credible plan combines hydrological monitoring with agreement on water levels and distribution of costs.
- Award each point once. Accept other well-supported interpretations addressing the task.
Marking points
- Higher water levels can protect peat from oxidation and fire.
- Farming access or productivity may be affected by wetter ground.
- Shared hydrological boundaries require coordination with neighbouring land users.
- Proposes a justified negotiated approach with monitoring and compensation or adapted land use.
Examiner tip: Name a stakeholder and a concrete trade-off before judging sustainability.
Marking points are indicative, not an official mark scheme. Accept equivalent valid methods and supported interpretations that address the task; award each mark once without requiring the model wording.