Carbon Cycle Eq1 Flashcards
What is the carbon cycle
The exchange of carbon between it’s stores: terrestrial, ocean and atmosphere
What is a carbon flux/flow
Process of transferring carbon between stores
Why are movements in terrestrial, atmospheric and ocean stores more important to us
They are quicker and affect us more
What is the flux with the shortest timescale
Plants absorb carbon from the atmosphere through photosynthesis, then release it again through respiration
What is the longest flux
Organic matter that is buried in sediments slowly transforms into fossil fuels which we release back into the atmosphere when we burn them
What two ways are sedimentary rocks formed
• dead organic matter falls to the bottom of oceans and lakes, where it is buried under silt and mud, lots of layers build up on top and compress it, turning it into shale
• sea creatures use calcium carbonate to form shells, they die and fall to the bottom of the ocean, they form layers and are lithified into rock
What is the slow carbon cycle
• CO2 reacts with water to form carbonic acid
• silicate weathering occurs and forms bicarbonate ions
• bicarbonate ions are used by animals for shells - turns into rock
• when rock subducts as part of earths crust , rocks go through metamorphism and release carbon dioxide - or is released through volcanic outgassing
What is silicate weathering
Carbonic acid reacts with silicate rock to form soluble bicarbonate ions
What is carbon sequestration
The capture of carbon from the atmosphere by the ocean, vegetation or sedimentary rocks where it is stored
Whatnare the three ocean pumps
Biological
Physical
Carbonate
What is the biological pump
Carbon dioxide from the atmosphere is absorbed by the phytoplankton through photosynthesis - carbon is either released through respiration or when animals die and fall to the bottom of the ocean
What is the carbonate pump
Carbon is transferred from silicate rock into carbon rich sediment (other flashcard on how sedimentary rock is formed)
What is the physical pump
Thermohaline circulation moved warm water from surface of the ocean to cooler areas of world
Cool water absorbs more carbon
Cool water then sinks as it is denser (down welling)
In other areas, thermohaline circulation moves cool water to the surface where carbon is released back into the atmosphere