The carbon cycle Flashcards

1
Q

What is the carbon cycle ?

A

The cycle by which carbon moves from one Earth sphere to another.
A closed system.

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2
Q

What are the major stores of carbon ?

A

-Lithosphere
-Cryosphere
-Atmosphere
-Hydrosphere
-Biosphere

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3
Q

Explain the lithosphere as a store of carbon

A

The crust and upper mantle.
Inorganic forms of carbon in the lithosphere: Ca, Mg
Organic forms : Coal, oil, organic matter, natural gas
-Distributed between marine sediments, sedimentary rock, soil organic matter, fossil fuel deposits, peat.
-Sedimentary rock is the largest store containing 99.9% of carbon
-In total stored around 100 million Gt of carbon

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4
Q

Explain the Cryosphere as a store of carbon

A

-Methyl clathrates are molecules of methane that are frozen into ice crystals (form under high pressure and low temperature)
-Organic matter frozen in permafrost (global warming melts permafrost releasing CO2/methane)
-Permafrost is in the Northen Hemisphere

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5
Q

Explain how the atmosphere is a store of carbon ?

A

Atmosphere used to composed of mainly CO2.
-Carbon makes up 0.04% of the atmosphere
-Due to human activities CO2 conc is higher than is has been for at least 800,000 years (possibly 200 million)

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6
Q

Explain the hydrosphere as a store of carbon

A

-Oceanic store between 37,000 GtC and 40,000 GtC
-Euphotic zone (surface) 900 GtC
-Twighlight zone (intermediate) 37,100 GtC
-Living organic matter amounts 30 GtC and dissolved organic matter 700 GtC
-Carbon stored by sedimentation

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7
Q

Explain how the biosphere is a store of carbon

A

The total sum of all living matter.
-living vegetation
plants constantly exchange carbon with the atmosphere
-Plant litter
Fresh, undecomposed plant debris
-Soil humus
Litter decomposition, gets dispersed throughout the soil
-Peat
Accumulation of partially decayed vegetation in wetland conditions, anaerobic conditions which slows down decomposition
-Animals
Decomposition

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8
Q

What is a Lithosere ?

A

A community that forms on rocks

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9
Q

What is a Psammosere ?

A

A community that forms on sand

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10
Q

What is a Xerosere ?

A

A community that forms on a dry and arid area

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11
Q

What is a Halosere ?

A

A community that forms on a marshy and saline area

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12
Q

What is the fast carbon cycle ?

A

Relatively rapid transfers of carbon compounds over years, decades and centuries

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13
Q

What is the slow carbon cycle ?

A

Transfers of carbon compounds over extensive timescales (up to millions of years)

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14
Q

What processes are apart of the slow carbon cycle ?

A

-Weathering
-Oceanic carbon pump
-Burial of sediment
-Carbon sequestration
-Tectonic/volcanic activity

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15
Q

What processes are apart of the fast carbon cycle ?

A

-Photosynthesis
-Respiration
-Decomposition
-Combustion

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16
Q

Explain decomposition

A

-Returns carbon from the biosphere to atmosphere. (can end up in pedosphere - soils or lithosphere)
-Decomposers (e.g. fungi, bacteria, earthworms) break down dead organisms and return carbons in their bodies to the atmosphere as CO2 by respiration.
-Dead organisms are broken down into substances that plants need for growth.
-Decomposition can be blocked if organic matter is frozen or buried in anaerobic environments (peat)

17
Q

Explain combustion

A

-When organic material is burned in the presence of oxygen and gives off CO2 , water and energy
-Oil, coal, fossil fuel, wood, plastic
-If any other elements are present they combine with oxygen to form pollutant molecules (e.g. nitrogen oxides)
-Could be deliberate and man-made or natural wildfires

18
Q

Explain sediment burial

A

-Tiny marine organisms from skeletons and shells of calcium carbonate
-When they die they sink
-Over years they’re buried by layers of sediment, as the pressure builds they turn into sedimentary rock
-Carbon is then stored as rocks beneath the ocean

19
Q

Explain weathering

A

-CO2 is removed from the atmosphere when it dissolves in the ocean and forms carbonic acid
-This forms acid rain which reacts with minerals dissolving them into ions
-The ions then reach rivers and eventually ocean where they eventually form calcium carbonate

20
Q

Explain tectonic and volcanic process

A

-Circulation of magma drags plates which causes oceanic and continental crust to meet
-The oceanic plate subducts, heats, rises back to the surface through eruptions, vents and CO2 rich hot springs.
-This allows CO2 to return to the atmosphere

21
Q

Explain the physical ocean pump

A

-CO2 dissolves in the sea (in colder water-poles)
-The cold water sinks to the bottom (vertical deep mixing)
-Once the cold water reaches the equator, the water warms and rises which releases CO2 back to the atmosphere
-Water then moves back to the poles at surface to repeat process

22
Q

Explain the biological carbon pump

A

-CO2 dissolves in the oceans
-This carbon is used to create shells and skeletons for marine organisms as calcium carbonate
-As they die they sink, the decay releases CO2 in the deep water
-Some material sinks and forms sedimentary rocks

23
Q

Explain geologic carbon sequestration

A

-Carbon is captured at its source (factory) and injected in liquid form into stores underground
-Injected into depleted oil, gas reservoirs, coal seams, salt formations or the deep sea
-This is still at the experimental stage and is very expensive

24
Q

Explain terrestrial carbon sequestration

A

-CO2 is absorbed by plants
-Therefore enrichment of plant ecosystems is a positive environmental action
-However forests may lose carbon to a fire or disease
-It’s slow growing and requires active management
-Carbon is never permanently removed from the atmosphere

25
What are natural changes to the carbon cycle ?
-Volcanic activity Transmits carbon from the lithosphere to atmosphere but has an overall cooling effect -Wildfires Increasing in intensity, duration and frequency. They occur where plant litter builds and if it’s dry enough.
26
How are humans influencing the carbon cycle ?
-Fuel extraction and burning The rate of fossil fuels is increasing as is extraction and burning, adding carbon to the atmosphere -Farming practices Ploughing, pastoral, clearing biomass to crops, peat bogs, rice paddies increase the rate carbon is released -Urbanisation A higher demand of energy and resources releasing more carbon -Deforestation Replaces biomass with inferior stores of carbon and releases CO2 into atmosphere, even more if burnt
27
Define the carbon budget
How much carbon is emitted by various processes compared to what can be absorbed
28
What is the natural greenhouse effect ?
Causes the natural warming of the earth, caused by the absorption of infrared radiation by greenhouse gasses in the atmosphere. Life could not be supported on earth without it.
29
What is the enhanced greenhouse effect ?
The additional warming of the atmosphere due to the increased amount of CO2 and other greenhouse gasses that humans release into the atmosphere.
30
What is carbon fertilisation ?
Increased CO2 concentration means more carbon is readily available to be converted into plant matter via photosynthesis. The extra growth in plants is carbon fertilisation. However warmer temps due to more CO2 dry them out making them more susceptible to burning, release CO2 when burnt. Warning is also melting permafrost which gives off CO2 and methane.
31
What is ocean acidification?
More CO2 is dissolving into the oceans which forms carbonic acid and H+. H+ increases the acidity. Sea life with calcium carbonate shells then find it harder to build and maintain shells. It also causes coral bleaching. These consequences are decreasing populations and may cause food webs to collapse.
32
What is ocean warming ?
The ocean is warming unevenly. Makes extreme weather events more common and impacting sea level rise. Warmer oceans can’t absorb as much CO2. Marine life suffers due to coral bleaching, marine heatwaves and even migration patterns.
33
How is melting sea ice having an impact ?
The reflective ice is replaced by more heat absorbent water. This amplifies warming as more sun is absorbed. Sea ice is a unique habitat for algae and other animals (polar bears) which rely on ice for their main source of food.
34
How is changing ocean salinity having an impact ?
Salinity levels decrease due to higher precipitation levels and higher temps. Higher temps cause ice caps to melt and glaciers causing an input of freshwater. Precipitation leads to more run-off that ends up in the sea.
35
How is sea-level rise having an impact ?
Rising at 3.1mm a year since 90’s. Melting of terrestrial ice as increased summer melting and less winter snowfall, Antarctica and greenland ice sheets are moving towards the ocean due to increased water lubricating bases. Water expands when it warms leading to thermal expansion. 1/2 of the past centuries rise has been due to water having more volume. 0.6-2.5m by 2100.