Unit 4: The Global Carbon Cycle Flashcards
(45 cards)
Define the carbon cycle
The carbon cycle is a biochemical cycle by which carbon moves from one part of the planet to another
What % of the planets biomass is made of carbon?
50%
How many metric tonnes of carbon is stored in the biosphere?
560 billion
What % of all the planets carbon is stored in the biosphere?
0.0012%
How many metric tonnes of carbon is stored in the atmosphere?
750 billion
What % of all the planets carbon is stored in the atmosphere?
0.0017%
What % of all the planets carbon is stored in the pedosphere?
0.0031%
What % of all the planets carbon is stored as fossil fuels?
0.004%
What % of all the planets carbon is stored in the hydrosphere?
0.0038%
How many metric tonnes of carbon is stored in the hydrosphere?
38,000 billion
As part of the lithosphere where is over 99.9% of the worlds carbon stored?
Marine sediment and sedimentary rocks such as limestone.
What time period does the slow carbon cycle operate over?
Between 100 and 200 million years
A type of chemical weathering known as carbonation weathering requires carbonic acid. How and where does carbonic acids form?
Atmosphere contains CO2 which combines with water vapour to make carbonic acid
The carbon in the ocean is used by what organisms and for what purpose?
Shells and skeletons of marine creatures as calcium carbonate.
What happens to carbon in these organisms?
They die, fall to bottom of sea, over millions of years they will compact down to create sedimentary rocks like limestone under heat and pressure, carbon from organic matter trapped in the sediment is converted into fossil fuels.
What is the name of the process in which atmospheric carbon is stored in a liquid or solid form in the lithosphere?
Sequestration
What happens to the carbon stored on the ocean floor at convergent plate boundaries when subduction occurs?
Under extreme heat and pressure the carbon contained in the rocks is released and rushes back to the surface. Every year volcanoes around the world release about 200 million tonnes of carbon dioxide back into the atmosphere.
Why is rainfall naturally acidic?
Due to CO2 in the air. Industry can make it more acidic.
What happens to rocks containing calcium carbonate, such as limestone, when it comes into contact with acidic solutions?
It bubbles and the rocks/limestone gets cared away.
Summarise the process of chemical weathering in the carbon cycle
- Atmospheric carbon dioxide is dissolved in water vapour and forms carbonic acid, Precipitation is naturally acidic (carbonic acid)
- Carbonic acid reacts with rocks containing calcium carbonate e.g. limestone through carbonation weathering and creates calcium bicarbonate
- Calcium bicarbonate is soluble in water and is carried away in solution by runoff and percolating water
- Soluble calcium bicarbonate is transferred to the ocean by river runoff
Whats a Karst landscape?
Areas where limestone dominates the surface rock type will over millions of years’ experience extensive carbonation weathering, which overtime can lead to distinctive landscapes known as karst landscapes - a limestone pavement is an example. Location example = Malham Cove, Yorkshire, England
What happens to the calcium bicarbonate?
- rivers, throughflow and groundwater transport calcium bicarbonate to the oceans
- at the bottom of the oceans large amounts of dissolved inorganic carbon accumulate (carbon sequestration) to form carbonate sediments Some of this sediment will be from the bicarbonate created by carbonation weathering.
- In the oceans carbonate is used by marine organism such as plankton and shellfish to make their shells.
What happens to the carbon stored on the ocean floor?
In subduction zones at convergent plate boundaries some of the carbon sediments are converted into magma which may result in volcanic eruptions, emitting CO2 back into the atmosphere. Each year about 200 million tons of CO2 are released into the atmosphere by volcanoes.
What are other effects of Plate tectonics on the carbon cycle?
Fold mountains which form at convergent boundaries will force carbonate-rich sediments and rocks, such as limestone, upwards. An example of this is the Himalayas. Once exposed to precipitation carbonation weathering will occur - back to the starting point.