Carbon cycle theory Flashcards

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1
Q

what is the biosphere

A

the regions of the surface and atmosphere of the earth or another planet occupied by living organisms

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2
Q

what are carbon stores also known as

A

carbon sinks

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3
Q

what is 99.9% of all carbon storage

A

99.9% of all carbon storage is in carbonate-based sedimentary rocks

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4
Q

what are the two strands to the carbon cycle

A

a slow cycle and a fast cycle

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5
Q

what is the slow carbon cycle

A

carbon stored in rocks, sea-floor sediments + fossil fuels which is locked away for millions of years

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6
Q

what is the total amount of carbon circulated by this slow cycle and how does it work?

A
  • total amount of carbon circulated by this slow cycle is 10-100 million tonnes/year
  • CO2 diffuses from the atmosphere into the oceans where marine organisms make their shells + skeletons by fixing dissolved carbon together w calcium carbonate.
  • on death, remains of these organisms sink to the ocean floor.
  • they accumulate over millions of years, heat and pressure convert them to carbon-rich sedimentary rocks through lithification
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7
Q

what is the typical residence time for carbon held in rocks

A

150 million years

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8
Q

what is the fast carbon cycle

A

carbon circulates most rapidly between the atmosphere, the oceans, living organisms (biosphere) + soils

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9
Q

what are the key components of the fast carbon cycle and how does it work

A
  • land plants + microscopic phytoplankton in the oceans are key components
  • through photosynthesis, they absorb CO2 from the atmosphere + combine it w water + sunlight to make carbohydrates
  • carbon exchange also occurs between the atmosphere + the oceans. through this exchange, individual carbon atoms are stored in the oceans for around 350 years
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10
Q

what are the carbon cycle processes

A

photosynthesis, respiration, precipitation, weathering, decomposition + combustion

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11
Q

photosynthesis as a process in the carbon cycle

A
  • the flux of carbon from atmosphere to land plants + phytoplankton via photosynthesis is around 120GT/year
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12
Q

what is respiration

A
  • respiration is the process by which carbohydrates fixed in photosynthesis are converted to CO2 + water (reverse of photosynthesis)
  • plants + animals absorb oxygen, which ‘burns’ these carbohydrates + provides the energy needed for metabolism + growth
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13
Q

what is the word equation for photosynthesis and respiration

A

carbon dioxide + water glucose + oxygen

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14
Q

why is precipitation considered a process of the carbon cycle

A

atmospheric CO2 dissolves in rainwater to form weak carbonic acid. this is a natural process, however, rising concentrations of CO2 in the atmosphere, due to anthropogenic emissions, have increased the acidity of rainfall. increased acidity in oceans

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15
Q

what is weathering

A

weathering is the in situ breakdown of rocks at/near Earth’s surface by chemical, physical + biological processes

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16
Q

why is weathering considered a process of the carbon cycle

A

rainwater is a weak carbonic acid, which slowly dissolves limestone + chalk in a process known as carbonation. this releases carbon from limestones to streams, rivers, oceans + the atmosphere

17
Q

how much carbon does chemical weathering transfer to the atmosphere + oceans every year

A

it is estimated that chemical weathering alone transfers 0.3 billion tonnes of carbon to the atmosphere + the ocean/year

18
Q

how does rate of decomposition depend on climatic conditions

A

rates of decomposition depend on climatic conditions. the fastest rates occur in warm, humid environments, with slow decomposition occurring in cold environments such as Arctic Tundra

19
Q

when does combustion occur

A

combustion occurs when organic material reacts or burns in the presence of oxygen - combustion process releases CO2 as well as other gases

20
Q

what combustion occurs in ecosystems?

A
  • wildfires caused by lightning strikes are essential to the health of some ecosystems, as long, cold winters slow the decomposition of forest litter which builds up on the forest floor. Fire shifts this log jam, freeing carbon + nutrients previously inaccessible to forest trees.
  • it also opens up the forest canopy, creating new habitats + increasing biodiversity.
  • combustion also results from human activities, such as the deliberate firing of forest + grassland in order to clear land for cultivation or improve the quality of grazing
21
Q

explain the combustion of fossil fuels occurring (stats)

A
  • oil, coal + natural gas power the global economy
  • currently, the burning of fossil fuels transfers nearly 10GT of CO2/year from geological store to the atmosphere, oceans + biosphere
22
Q

what is carbon sequestration

A

a natural or artificial process by which carbon dioxide is removed from the atmosphere + held in solid or liquid form

23
Q

explain the role of the physical pump of carbon dioxide in ocean-atmosphere interactions (carbon sequestration)

A
  • CO2 enters the oceans from the atmosphere by diffusion.
  • the physical carbon pump involves the mixing of surface + deep ocean waters by vertical currents creating even more distribution of carbon in oceans
  • the surface currents then transport this dissolved CO2 polewards where the water cools, becomes more dense + sinks
  • this downwelling takes the dissolved carbon to the ocean depths where individual carbon molecules may remain for centuries
  • eventually, deep ocean currents transport the carbon to areas of upwelling + the CO2 is brought to the surface + diffuses back into the atmosphere
24
Q

what is upwelling

A

Upwelling is a process in which deep, cold water rises toward the surface

25
Q

what is downwelling

A

Downwelling is the process of accumulation and sinking of higher density material beneath lower density material, such as cold or saline water beneath warmer or fresher water or cold air beneath warm air

26
Q

explain the role of the biological pump of carbon dioxide in ocean-atmosphere interactions (carbon sequestration)

A
  • this is carbon exchanged between oceans + the atmosphere by marine organisms
  • phytoplankton drive this biological pump by absorbing carbon as CO2 + combining it with sunlight + water to produce organic material
  • the carbon locked in these phytoplankton is released into the oceans as CO2 once the phytoplankton die or after they are consumed in the food chain
  • most carbon-rich ocean material ends up into ocean sediments is then lithified to form chalk + limestone
27
Q

what is lithification

A

Lithification is the process in which sediments compact under pressure, expel connate fluids, and gradually become solid rock

28
Q

what is vegetation’s role in carbon sequestration

A
  • land plants, especially trees in the rainforests, contain huge stores of carbon
  • most of this carbon has been extracted from atmospheric CO2 through photosynthesis + is now locked away for decades
29
Q

how does farming (human activity) affect the carbon cycle

A
  • clearance of forest for farming reduces carbon storage in both above + below ground biomass
  • soil carbon storage is reduced by ploughing + exposure of soil organic matter to oxidation
  • significant soil erosion occurs during the arable farming process
  • often the NPP of crops can exceed the NPP of the previous grassland
  • however, photosynthesis generally falls, fundamentally down to the lack of biodiversity
30
Q

what is arable farming

A

An arable farmer is a farmer who grows ‘cereal crops’

31
Q

how much of global energy consumption have fossil fuels accounted for + how much CO2 is released into the atmosphere annually

A

fossil fuels account for 87% of global energy consumption, releasing 10 billion tonnes of CO2 into the atmosphere annually

32
Q

what is carbon capture and storage and how does it work

A

CCS or carbon capture and storage is capture/storage of CO2 released by power plants + industry

  • firstly, the CO2 is separated from the power station emissions
  • then, CO2 is compressed + transported by pipeline to storage areas
  • finally, CO2 is injected into porous rocks deep underground
33
Q

what economic/geographical factors limit carbon capture and storage’s (CCS) effectiveness

A
  • Big capital costs
  • Uses large amounts of energy - typically 20% of a power plant’s output is needed to separate + compress CO2
  • requires storage reservoirs w specific geological conditions (porous rock overlain by impermeable strata)
34
Q

what state of equilibrium is the global carbon cycle in currently and why

A

the global carbon cycle is currently in a state of disequilibrium:
- the concentration of CO2 in the atmosphere, the acidity of oceans + the flux of carbon between the major stores have all been distorted by human activity (primarily burning of fossil fuels)

35
Q

what is the carbon fertilisation effect (CFE) and is there evidence for this theory

A
  • the larger the amount of carbon dioxide in the atmosphere that has resulted from rising anthropogenic emissions should help the growth of plants, which use carbon dioxide during photosynthesis
  • Despite the correlation between the increase in primary production + the increase in atmospheric CO2, there is yet to be enough evidence to support this theory
36
Q

what is NPP

A

Net primary productivity (NPP) is defined as the net flux of carbon from the atmosphere into green plants per unit time - the amount of carbon uptake after subtracting ‘plant repiration’ from GPP

37
Q

what is GPP

A

the total rate at which the ecosystem captures + stores carbon as plant biomass per unit time