OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Earth’s Life Support Systems
Natural sequestration in oceans, vegetation, sediments and rock
- 3 things to know
- Component 01
Overview
Recall questions on carbon sequestration, the solubility, biological and carbonate pumps, the formation of limestone, net carbon uptake by the oceans and land biosphere, soil carbon, carbon in sedimentary rock and silicate weathering, and blue carbon.
What you need to know
Answer each one before you reveal it.
Why does warm tropical seawater hold less dissolved carbon dioxide than cold polar water?
How does limestone form from marine organisms?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is carbon sequestration?
Model answer
Carbon sequestration is the long-term capture and storage of carbon in a store that holds it out of the atmosphere.
- 2
How does the solubility pump carry carbon into the deep ocean?
Model answer
Cold, dense water at high latitudes dissolves carbon dioxide readily and then sinks as part of the thermohaline circulation, carrying that dissolved carbon to depths where it stays for centuries.
- 3
Why does warm tropical seawater hold less dissolved carbon dioxide than cold polar water?
Model answer
The solubility of a gas falls as temperature rises, so warm water can hold less carbon dioxide and tends to release it back to the atmosphere.
- 4
Describe the biological pump.
Model answer
Phytoplankton fix carbon dioxide in the sunlit surface ocean, and when they and the animals that eat them die the organic carbon sinks as detritus into the deep ocean and onto the sea floor.
- 5
What is the carbonate pump?
Model answer
The carbonate pump is the process by which marine organisms build shells and skeletons of calcium carbonate that sink when they die and accumulate as carbonate sediment on the sea bed.
- 6
How does limestone form from marine organisms?
Model answer
Calcium carbonate shells and skeletons settle on the sea floor, build up as sediment and are compacted and cemented over millions of years into limestone.
Other ways to work this
The same content, four other ways.
What is inside Levo
Six ways to work the same material.
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