The carbon cycle and energy security Flashcards
Petagram
A trillion kg
PgC = Petagram of carbon
Anthropogenic
Human influenced
The carbon cycle
Bio-chemical cycle by which carbon fluxes from one sphere to another. It’s a closed system so the total amount of carbon is constant.
Residency time
How long carbon stays in one sphere
Biggest carbon stores (PgC)
Sedimentary rock - 83m
Intermediate & deep ocean - 37,000
Soil - 2,000
Ocean floor ooze - 1,750
Permafrost - 1,700
Biggest carbon fluxes
(PgC)
Photosynthesis - 123
Respiration & fire - 120
Atmosphere to ocean - 80
Ocean to atmosphere - 78
Fossil fuels and cement - 8
The four spheres
Hydrosphere
Atmosphere
Lithosphere
Biosphere
Oil and natural gas formation
Phytoplankton and sea plants die and are covered by silt and sand. If organic content >= 2%, then over millions of years, heat, pressure and anaerobic processes creates oil/gas.
Formation of sedimentary rocks
Made of calcium carbonate, formed from shells/skeletons and coral.
How do volcanoes release CO2
CO2 is released from sedimentary rocks and water through subduction
What happens to sedimentary rocks like limestone
Buried
Melted
Pushed up into terrestrial sphere
Biological pump
-Phytoplankton photosynthesise
-Passed through food chain and respired
-Carbon moves through the ocean via feeding, waste and decomposition
Carbonate pump
-Organisms use calcium carbonate to build their shells and create marine snow when they die
-Many shells dissolve, releasing carbon into ocean currents
-Shells that don’t dissolve build up on the sea floor and turn into limestone via high heat and pressure
Thermohaline conveyor
-Primary mechanism for distributing heat globally
-Water heats and rises at equator, releasing CO2
-Travels to poles, where it cools and sinks
-Travels back to equator through deep ocean, CO2 stays here for hundreds of years
Why are warming oceans an issue
-Water absorbs less CO2, enhancing GW
-Marine heatwaves that disrupt carbon cycle and marine life
Why is the thermohaline conveyor failing and why’s it bad
-Water doesn’t sink at the poles as much, so less circulation
-Less oxygen reaches deep sea, marine life at risk
-Less CO2 absorption via biological/carbonate pumps
-Since 1990, circulation has slowed by a third
Net Primary Productivity
The balance between energy captured by photosynthesis and released by respiration