1 - The Carbon Cycle Flashcards
What is the carbon cycle?
Carbons route on Earth, within which carbon is transformed from organic carbon (in living organisms) to inorganic carbon (ores and minerals) and back again.
Name the 7 carbon stores (FALSBOS)
- Fossil fuels
- Atmosphere
- Lithosphere
- Soils
- Biosphere/vegetation
- Oceans
- Sediments on the ocean floor
Name the 7 carbon flows.
- Photosynthesis
- Combustion
- Ocean uptake and loss
- Sequestration
- Respiration
- Decomposition
- Weathering
Describe the 3 main carbon forms.
Carbon Dioxide (CO2) - gas found in the atmosphere, soils and oceans.
Methane (CH4) - gas found in the atmosphere, soil, oceans and sedimentary rock.
Calcium Carbonate (CaCO3) - a solid compound found in calcareous rocks, oceans and in skeletons and shells of ocean features.
Give an example of positive feedback in the carbon cycle.
Increase in global temp. > Oceanic temp. increases > Dissolved CO2 released by oceans > More CO2 in atmosphere > Increase in global temp. …
Give an example of negative feedback in the carbon cycle.
More fossil fuels burnt > Increase of CO2 in the atmosphere > Increased global temp. > More vegetation grows > More CO2 taken in by plants > Reduced CO2 in atmosphere > Global temp. ‘dampens’ due to less atmospheric CO2
Describe the different time scales that carbon flows happen over.
The fastest carbon flows (minutes-days) include photosynthesis, respiration, combustion and decomposition.
The slowest carbon flow (millions of years!) is sequestration.
Describe the different spatial scales that carbon flows happen over.
Plant scale = photosynthesis and respiration
Ecosystem scale = Combustion and decomposition
Continental scale = all flows!!
Explain photosynthesis as a carbon flow.
Transfers carbon from the atmosphere to the biosphere.
Energy from sun + CO2 + H2O -> Glucose + O2
Tiny marine plants (phytoplankton) in the sunlit waters of the oceans, as well as all terrestrial plants, photosynthetic algae, and bacteria turn carbon into organic matter by photosynthesis.
Explain decomposition as a carbon flow.
Transfers carbon from the biosphere to the atmosphere and soil.
This is when the majority of the remainder of carbon left in living things when they die is released by decomposers that break down the cells and tissues in dead organisms.
Explain respiration as a carbon flow.
Transfers carbon from the biosphere to the atmosphere.
Glucose + O2 -> CO2 +H2O + Energy
By the process of respiration, plants use some stored carbohydrates as an energy source to carry out their life-functions.
Explain combustion as a carbon flow.
Transfers carbon from the biosphere to the atmosphere.
Combustion is the burning of living and dead things e.g. wildfires which are naturally caused by lightning strikes but can also be due to humans.
Explain carbon sequestration as a carbon flow.
Transfers carbon from an environment (the atmosphere or the hydrosphere) and to new store (the biosphere, lithosphere, sediments on the ocean floor, or an artificial store)
Sequestration is the trapping of carbon and its isolation in a natural or artificial store.
Example:
Atmospheric CO2 is removed and dissolved in water = CaCO3, reaches Earth as rain and dissolves minerals on Earth’s surface through chemical weathering, releasing ions that are carried by surface waters into the oceans and settle out as minerals that marine organisms use in shells and coral. These creatures die and their skeletons sink to the bottom of ocean, are buried for millions of years and become sedimentary rock. Through subduction, CO2 can be released back into the atmosphere from this rock.
Carbon sequestration can also happen in plants but is released much quicker when plants combust or decompose.
Explain weathering as a carbon flow.
Transfers carbon from the lithosphere to the hydrosphere.
Weathering is the breakdown or decay of rocks by mildly acidic carbonic acid when rainwater absorbs CO2. The carbon in rocks is held in a solution as the rock dissolves and is transported by the water cycle to the oceans.
What are the 2 types of changes in the carbon cycle?
Natural variations
Human impacts