Carbon Cycle Flashcards
What is the carbon cycle?
The natural C Cycle is the movement (fluxes) and storage of C between the land, ocean and the atmosphere
What is inorganic Carbon?
Inorganic carbon refers to carbon found in non-living forms
Found as carbon dioxide (CO₂) in the atmosphere carbonates in rocks and minerals, and bicarbonates in water.
It plays a key role in the carbon cycle, moving between the atmosphere, oceans, and Earth’s surface.
What is organic carbon?
Organic carbon is carbon found in living organisms or derived from them, such as in plants, animals, and decaying matter.
It plays a key role in the carbon cycle, moving between organisms, the atmosphere, soil, and oceans.
What is Gaseous carbon and where is it found?
Gaseous carbon is carbon in the form of carbon dioxide (CO₂) in the atmosphere, which plays a role in photosynthesis, respiration, and the greenhouse effect.
Found in C02 and CH4
What is carbon sequestration?
It is the capturing, storage and transfer of C from the atmosphere to other stores and can be natural and artificial (e.g. Carbon Capture and Storage).
A plant sequesters C when it photosynthesises and stores the C in its mass.
Where is carbon stored, and which is the highest store and which is the lowest store?
Highest:
Lithosphere = as carbonates in limestone and fossil fuels (e.g. coal, oil and gas)
Hydrosphere = as dissolved carbon dioxide
Pedosphere
Cryosphere = biological carbon is stored in permafrost, which prevents bacterial decay
Atmosphere = as carbon dioxide and compounds such as methane
Biosphere = in living and dead organisms
Lowest:
Large
Hamster
Pigs
Cry
At
Butchers
What are the lithosphere stores?
- Marine sediments (ocean floor) and sedimentary rocks (biggest store). Long-term (up to millions of years).
- Fossil fuel deposits (e.g. coal) – originally long-term, but dynamic due to human exploitation
- Soil organic matter – mid-term (deforestation, agriculture and land-use change are affecting this store)
What are the hydrosphere stores?
Oceans – dynamic.
The second biggest store, but only a tiny fraction of that stored in the lithosphere.
The C is constantly being utilised by marine organisms, lost as an output (diffusion) to the lithosphere (sedimentation on the ocean floor), or gains from inputs from rivers and coastal weathering and erosion
What are Atmosphere stores?
Stores Co2
A dynamic store
Human activity has caused CO2 levels to increase by 40% since 1750 and is accelerating in the 21st Century.
What are Biosphere stores?
Terrestrial plants (mid-term, but very dynamic). Vulnerable to Climate Change deforestation.
What are Cryosphere stores?
Methyl clathrates are molecules of methane that are frozen into ice crystals. If the temperature rises or pressure changes, the ice that imprisons the methane will break apart, and the methane will escape.
Organic matter frozen in permafrost. Permafrost is permanently frozen ground, and it contains a lot of frozen organic matter. This organic matter is made of dead plants and animals that have been frozen deep in permafrost for thousands of years. The carbon in this organic matter is locked up because it is frozen. With global warming, if this permafrost melts the organic matter will decay, and this will release carbon dioxide or methane into the atmosphere.
What are fluxes between carbon stores?
The transfers in the C Cycle cause changes/movement of C in stores over varying degree of time.
They can be categorised as either fast flows or slow flows.
Why is photosynthesis a fast flow?
Plants sequester C by converting CO2 from the atmosphere and water from the soil into O2 and glucose using light energy. This helps to maintain the balance between O2 and CO2 in the atmosphere.
Why is respiration a fast flow?
Respiration occurs when plants and animals convert O2 and glucose into energy, which is opposite of photosynthesis. Plants photosynthesise by day and respire at night. Plants are net oxygen producers because they absorb more than they emit.
Why is combustion a fast flow?
When fossil fuels and organic matter e.g. trees are burnt they emit CO2 into the atmosphere. This is obviously a human influence on the C Cycle (indirectly for some wildfires due to CC).
Why is decomposition a fast flow?
When living organisms die they are broken down by decomposers (e.g. bacteria and fungi) which respire returning CO2 in to the atmosphere. Some organic matter is returned to the soil where it is stored.
During the water cycle, why is diffusion a fast flow?
The oceans can absorb CO2 from the atmosphere which has increased ocean acidity by 30% in the last 250 years, which is harming aquatic life by causing coral bleaching. At the surface, where air meets water, carbon dioxide gas dissolves in and ventilates out of the ocean in a steady exchange with the atmosphere.
Why is sedimentation a slow flow?
Can happen on land or sea floor.
When shelled marine organisms die, their shell fragments sink to the ocean floor and become lithified over time to form limestone.
Organic matter from vegetation can be compacted over time to form fossil fuel deposits.
Why is weathering and erosion a slow flow?
(Long Answer)
Inorganic C is released slowly through weathering e.g. solution of alkaline rocks (e.g. chalk) by carbonic acid in rain/river/sea water. The C is moved through the water cycle and enters the oceans. Marine organisms use the C to build their shells – eventually die and sedimentation occurs on the sea floor. Increasing CO2 levels in the atmosphere are accelerating this process.
Why is volcanic outgassing a slow flow?
Pockets of carbon dioxide exist in the Earth’s crust. Volcanic eruptions and earthquakes can release these gas pockets.
Outgassing is the release of gas, previously dissolved, trapped, frozen or absorbed in some material (e.g. rock). It occurs mainly along mid-ocean ridges, subduction zones and at magma hotspots.
How long can carbon remain in different stores? (Residence time)
Lithosphere – from 10,000 – 300,000,000 years (sedimentary rocks)
Hydrosphere – ocean surface – up to 25 years; deep oceans – up to 1250 years
Cryosphere – up to millions of years
Atmosphere – up to 6 years
Biosphere – average is 13 years (but can be much shorter)
How does chemical weathering impact the carbon cycle?
(Long answer)
- Rainwater reacts with atmospheric CO2 to form a weak carbonic acid. The rain reaches the surface and reacts with some surface minerals slowly dissolving them into their component ions.
- Calcium ions are transported by rivers to the ocean. These combine with bicarbonate ions to form CaCO3 and precipitate out as minerals such as calcite.
- Deposition and burial turns the calcite into limestone.
- The ocean floor is eventually subducted under continental plates.
- Some of the C rises up within magma and degassed as CO2 back into the atmosphere.
How does volcanic outgassing impact the carbon cycle?
The Earth’s crust contains pockets of carbon dioxide which can be disturbed by volcanic eruptions or seismic activity
This release of gas that has been dissolved, trapped, frozen or absorbed in rock is called outgassing
- Outgassing occurs at subduction zones and spreading ridges; hot springs and geysers and as direct emissions from fractures in the Earth’s crust
- Volcanoes currently emit 0.15-0.26 Gt CO2 annually. In comparison, humans emit about 35 Gt, mainly from fossil fuel use, so volcanic degassing is relatively insignificant
- The CO2 emitted by both active volcanoes and at constructive plate margins is roughly the same
What is oceanic sequestration?
Oceanic sequestration refers to the process by which the ocean absorbs and stores carbon dioxide (CO2) from the atmosphere.
93% of carbon dioxide is stored in undersea algae, plants, coral and dissolved form, making oceans the largest carbon store on Earth
The CO2 gas exchange flux between the oceans and atmosphere operates on a timescale of over several hundred years. There is also a significant input of both organic C and carbonate ions from rivers. Only a small proportion of this will end up buried in sediments, but these are important long-term stores operating over millennia, unlike most terrestrial systems.
The exchange of CO2 between the oceans and atmosphere takes place over hundreds of years. Rivers also contribute organic carbon and carbonate ions, with only a small portion getting buried in sediments. These buried materials act as important long-term carbon stores, lasting thousands of years, unlike most land-based systems. (SIMPLIFIED)