The carbon cycle and energy security Flashcards
(115 cards)
What is the full name of the carbon cycle?
The biogeochemical carbon cycle
How much carbon is stored in the oceans?
38,000 PgC
How much carbon is stored in the atmosphere?
750 PgC
How much carbon stored in soils?
1950 PgC
How much carbon stored in vegitation?
550 PgC
How much Carbon stored in sedimentary rocks?
83,000,000 PgC
How much carbon stored in fosil fuels?
1471 PgC, though this is constantly falling due to human activity
How much carbon is stored in perma frost?
1700 PgC
How big is the flux from photosynthesis?
123 PgC
How big is the flux from respiration?
60PgC
How big is the flux from Ocean to atmosphere?
78 PgC
How big is the flux from the atmosphere to the oceans?
80 PgC
How big is the flux derived through the burning of fossil fuels?
8-10 PgC
Explain the geological carbon cycle
Rainwater becomes a weak carbonic acid when it absorbs
carbon dioxide from the atmosphere that then reacts with silicate minerals. This chemical weathering process releases ions such as calcium, which are transported by rivers to the oceans, where organisms combine calcium with dissolved
carbon to create calcium carbonate which they use for shells. Carbonate rock forms via sedimentation of dead organisms, which creates strata of sedimentary rock. carbon is released back into the atmosphere by volcanism and the metamorphism of sedimentary rocks.
What are the three pumps of carbon in the ocean?
The biological pump, the carbonate pump and the physical pump
Explain the biologicl pump of carbon within the ocean?
Phytoplankton are tiny, single celled microorganisms.They make up less than 1% of the worlds biomass, but half of it’s primary production. They move close to the oceans surface to photosynthesise, as they have chlorophyl. As the basis of the ocean food chain, they sequester carbon from the atmosphere and pass it up the foodchain to form organic matter. They can decay, releasing carbon back into the ocean.
Explain the carbonte pump of carbon in the oceans
marine organisms such as mollusks, crabs and plankton use the bicarbonate ions (HCO₃⁻) to form calcium carbonate (CaCO₃), which they use to build their shells and skeletons.
When these organisms die, most of their calcium carbonate shells disolve, releasing carbon into ocean currents which can be transfered back into the atmosphere. Some sink to the ocean floor, carrying carbon to the deep ocean, where they become compacted and form sedimentary rocks, storing carbon for long periods.
Explain the Phyical pump of carbon within the ocean
The physical pump refers to the ocean’s role in moving carbon through deep ocean currents. This process is driven by the thermohaline circulation
Carbon dioxide in the atmosphere enters the ocean through diffusion, thoAt higher latitudes (near the poles), the water cools down and becomes denser (saltier water from evaporation also adds to this). This cold, dense water sinks to the deep ocean, carrying dissolved carbon with it as cold water can store more carbon than warm waters. As this cold water sinks, it triggers a global pattern of deep-ocean currents. These currents transport carbon to the deeper parts of the ocean, where it can be stored for centuries or longer.
This deep-water carbon can eventually upwell (move back toward the surface) in other parts of the ocean, releasing the carbon back into the atmosphere as it warms near the tropics (as warm water stores less carbon). But for a time, this carbon is sequestered deep in the ocean.
Explain the role of terrestial vegitation in the carbon cycle
Terresterial vegitation sequesters carbon during photosynthesis. In a process of carbon fixation, it turns gaseous carbon into organic matter in the cells of autotrophs and is stored there. Carbon can be released back into the atmosphere through respiration, meaning there is a continuning balance between oxygen and carbon in the atmosphere and eventually decompisition. However, deforestation is reducing the effectiveness of this store by accelerating the process by which the carbon sequested in the vegitation is returned to the atmosphere.
How is biological carbon stored and released through soils?
Carbon can be stored in soil in the form of dead organic matter, or be released back into the atmosphere through decomposition.
Why are mangrove forests especially effective at storing carbon in their soils?
Mangrove soil contains a rich layer of carbon rich materials such as humus and peat (over 10% carbon). Submerged by tides twice a day, their soil is anaerobic. Bacteria cannot live without oxygen, so decomposition tends to be very slow.
How much mangrove has been lost due to human activity?
50%
Why are tundra soils effective at storing carbon?
Frozen all year at the bottom, microbes cannot decompose the organic matter so ancient carbon is stored.
explain the natural greenhouse effect
When solar energy enters the atmosphere, clouds reflect about 31% of it back into space. The rest of it can pass through the atmospheric gasses due to the energys short wave length. About 50% of the energy is absorbed by the surface. Some of this energy is reflected back ooutwards, hhowever is now a longer wavelength in the form of infrared radiation. This means that it struggles to move through the greenhouse gasses, and is absorbed by them. These greenhouse gasses then remmit this energy in all directions, moving some into space and some back towards the surface.