EQ1- How does the carbon cycle operate to maintain planetary health Flashcards

1
Q

What is the importance of the carbon cycle on earth

A

Provides a major building block for all life on earth. A balanced carbon cycle is important in regulating our climate and maintaining the health of our planet.

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2
Q

Explain the composition of carbon

A

Is a common element in the composition of the earth
Exists in gas, solid and liquid forms , in organic and inorganic forms. Carbon moves between these forms (carbon pathway) through natural (biogeochemical) processes over time

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3
Q

Define Sequestering

A

Is the natural storage of carbon by physical or biological processes such as photosynthesis

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4
Q

Explain the carbon cycle as a system

A

The carbon cycle is a closed system . It does not have any external inputs or outputs , so the total amount of carbon is constant and finite

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5
Q

Define stores

A

Reservoirs where carbon is held

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6
Q

Define Fluxes

A

Are the movement of carbon between stores

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7
Q

Define processes

A

Are the physical mechanisms which drive the fluxes between stores

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8
Q

Define and explain the form of the four carbon stores

A

The atmosphere - gases such as carbon dioxide and methane

The hydrosphere - dissolved carbon dioxide in oceans and lakes

The lithosphere - carbonates in limestone and fossil fuels

The biosphere - living and dead organisms

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9
Q

State the largest Carbon store and the largest carbon flux

A

Carbon store - sedimentary rock store (83 million pgc)

Carbon flux - photosynthesis (123 pgc/year)

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10
Q

Explain the geological carbon cycle

What is its importance

A

Is a natural cycle that moves carbon between land, oceans and the atmosphere. This movement involves chemical reactions which creates stores to trap carbon, leading to a natural balance between carbon production and absorption within the cycle, allowing a equilibrium.

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11
Q

Explain the factors in the geological carbon cycle

A

Carbon held within the mantle is released as co2 when volcanoes erupt

Co2 in the atmosphere combines with rainfall to produce acid rain

Carbonic acid reacts with rocks to form calcium carbonate

When plants and animals die their shells form limestone with carbon stored in it

Carbon rich rocks are sub ducted along plate boundaries

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12
Q

Explain the biogeochemical carbon cycle

What is its importance

A

The cycles processes determine how much of the carbon available on earth is stored or released. Living organisms help control the balance between storage, release, transfer and absorption. Allows an equilibrium to be maintained

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13
Q

Explain the factors of the biogeochemical carbon cycle

A

Photosynthesis occurs where plants remove co2 from the atmosphere

Respiration occurs where animals consume plants and release co2 into the atmosphere and water

Decomposition occurs in dead plants and animals releasing co2 into soils and deposits carbon in the sea

Combustion occurs where fossil fuels are burnt releasing co2

All contribute towards co2 in the atmosphere

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14
Q

Define system feedback

A

Occurs when the earth’s system operate by negative feedback , maintaining an equilibrium by preventing too much release of co2 into the atmosphere

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15
Q

Explain the impact of human carbon emissions

A

Are only small compared to natural emissions. However when more carbon is released into the atmosphere , through human activities, it adds up because the land and ocean cannot absorb all the extra carbon. Human emissions disrupt the natural balance of the carbon cycle

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16
Q

Explain which areas of the world absorb the most co2

A

Mid and high latitudes absorb the most carbon dioxide. In the northern hemisphere levels of CO2 a higher due to the high amount of vegetation, allowing photogenic activity to occur. In the northern hemisphere large fluctuations in co2 occur during summer and winter due to the large differences in plant photosynthesis

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17
Q

State the three forms of carbon and where they are found

A

Inorganic - found in rocks as carbonates
Organic- found in plant material
Gaseous- found as C02, methane and carbon monoxide

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18
Q

Explain how limestone rock is a store for carbon

A

Contains a high concentration of calcium carbonate, formed from shell building organisms (coral) that extracted carbon from the seawater, and also from marine phytoplankton that absorbs carbon through photosynthesis

Their remains accumulate on the ocean floor, and after a long period of time are cemented and lithified into limestone

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19
Q

Explain how biologically derived carbon in rocks is a store for carbon

A

An example is shale

Formed when carbon from organisms is embedded into layers of mud. Heat and pressure over millions of years compress the mud and carbon to form shale rock

20
Q

Explain how carbon fossil fuels is a store for carbon

A

Made up 300 million years ago from dead organic material

Dead organisms sank to the bottom of rivers and seas, covered in silt and mud, then decayed anaerobically

The organic matter built up faster than it decayed , forming fossil fuels like coal instead of shale

21
Q

State the two main geological processes that release carbon into the atmosphere

A

Chemical weathering in rocks

Volcanic degassing at ocean ridges and subduction zones

22
Q

Explain how chemical weathering in rocks is a process that releases carbon into the atmosphere

A

Occurs where the geological part of the carbon cycle reacts with the rock cycle, causing the weathering of carbon rich rocks, like limestone

Water reacts with atmospheric carbon, forming carbonic acid.

Only weakly acidic , but dissolves rock minerals (when it reaches the surface as rain) to form new minerals such as calcium carbonate. Only occurs when calcium ions are transported to the sea, where it reacts with bicarbonate to form calcium carbonate.

These minerals are Deposited and buried , then cemented and liquefied after a long period of time to form limestone

Tectonic spreading occurs, causing the seduction of the sea floor and bringing carbon rich sedimentary rocks into contact with extreme heat, in the form of magma. This causes chemical changes and rock to be degassed , releasing CO2 into the atmosphere.

This is seen in contemporary society , in geothermal areas like Iceland and New Zealand

23
Q

Explain how volcanic degassing at ocean ridges and subduction zones is a process that releases carbon into the atmosphere

A

Is relatively insignificant in comparison to human activity , however it does release approximately 300 million tons of carbon into the atmosphere, due to it being the least soluble and his degassed earlier in the eruption process.

Outguessing takes place in subduction zones and ocean ridges seen in Hawaii and Cicely. Degassing occurs in the vent of a of a volcano, where carbon is recycled at subduction zones and carbonate rocks are dragged into the mantle. In the volcano erupts magma, containing carbon , is released into the atmosphere

24
Q

Explain the oceans role in the carbon cycle

A

The ocean is one of the earth’s largest carbon stores, 50x greater than the atmosphere

25
Q

Define carbon sequestration

A

Is the removal and storage of carbon from the atmosphere. Usually occurs in oceans, forests and soil through photosynthesis.

26
Q

Describe the co2 gas exchange between the ocean and the atmosphere

A

Operates over several hundreds of years. Only a small proportion of the carbon in oceans is eventually buried in the ocean sediments.

27
Q

Define carbon cycle pumps

A

Are the processes operating in oceans to circulate and store carbon. There are three types: biological, carbonate and physical.

28
Q

Define and explain the biological pump in oceans

A

Is the organic sequestration of CO2 to oceans by phytoplankton.

Phytoplankton float up to the ocean surface to photosynthesise, they are the base of the food web.
Carbon is then passed up the food chain by fish and zoo plankton, which releases CO2 back into the water and the atmosphere.
Most carbon is recycled in surface water, only 0.1% reaches the sea floor after the dead plankton sink and decompose.

29
Q

Define and explain the carbonate pump in the ocean

A

Is the formation of sediments from dead organisms.

Marine organisms (like plankton, oysters and lobsters) may utilise calcium carbonate to make hard outer shells.
When organisms die and sink, their shells dissolve before reaching the sea floor. The carbon becomes part of the deep ocean current.
Shells that don’t dissolve build up slowly on the sea floor, forming limestone sediments like the white cliffs of dover
30
Q

Define and explain the physical pump in the ocean

A

Is the ocean circulation of water including upwelling, downwelling and the thermohaline current.

Co2 concentration is different in different parts of the ocean, the colder the water the more potential for co2 to be absorbed whilst warm waters release co2 into the atmosphere.
Major ocean currents, like the gulf stream, moves water from the tropics to the poles, the water cools and absorbs more atmospheric carbon.

31
Q

Define and explain thermohaline circulation in the ocean

A

Is the global system of surface and deep ocean currents driven by temperature (thermo) and salinity (haline) differences between areas of the ocean.

  1. Main current begins in polar oceans with low temperatures and high levels of salinity
  2. Division of the main current sees a current in the Indian ocean and the Pacific ocean
  3. The two currents warm and rise, circulating around the world until they reach the poles
32
Q

Explain and define the role of primary producers (plants) in the carbon cycle

A

Sequester carbon through photosynthesis. Store a significant amount of carbon.

Producers are green plants that use solar energy to produce biomass, accounting for 95% of a trees biomass. As they grow they release co2 into the atmosphere through respiration

33
Q

Explain the role of consumers in the carbon cycle

A

Depend on producers to feed, plants and leaves dropped from trees, and return carbon to the atmosphere through respiration.

These consumers store carbon as part of their fats and proteins.

Dead animals and plants Start to decompose fastest in tropical climates, where there are high temperatures and high rainfall, and biological decomposes feed on the dead organisms. When decomposition occurs the nutrients and carbon are taken in by the soil, acting as a store and contributing towards the growth of biomass

34
Q

Explain the significance of soil in the carbon cycle

A

Soil stores 20 to 30% of global carbon, sequestering two times the quantity of carbon as the atmosphere.

After the death of organisms thousands of compounds are decomposed before being broken down by soil microbes and released back into the atmosphere.

Carbon cycling is most active in the top of the soil, and perms first region 60% of carbon is stored in 30 cm.

Mangrove forests sequester 1.5 metric tons of carbon a year, with thick layers of peat which absorbs carbon and decompose it slowly. Carbon from mangrove soil is only released if it is drained.

35
Q

Define biological carbon

A

Is stored in soils in the form of dead organic matter, or returned back to get atmosphere as a result of decomposition

36
Q

Explain the factors affecting social capacity to store carbon (3)

A

Climate- dictates plant growth and microbial activity, rapid decomposition occurs in hot climates with high rainfall

Soil type- Clee rich soils have a higher carbon content than sandy soil,protecting carbon from decomposition.

Management and use of soil- cultivation and disturbance has caused a 40- 90 billion tonne loss of carbon since 1850.

37
Q

Define systems

A

Is how the carbon cycle sustains other earth systems

38
Q

Define equilibrium of carbon

A

Describes how the carbon cycle is balanced and how that balance is disturbed by human activities

39
Q

Explain the greenhouse effect

A

Is the warming of the atmosphere as gases such as carbon dioxide, methane and water vapour absorb heat energy radiated from the earth. These greenhouse gases absorb and reflect back some of the radiated heat from the earth’s surface , helping to retain a temperature to support human life.

40
Q

Explained the enhanced greenhouse effect

A

Describes the increase of greenhouse gases in the atmosphere as a result of increased human activity. The burning of fossil fuels and deforestation release natural stores of carbon to form co2 and nitrous oxide , leading to increased water temperatures and the trapping of heat in the atmosphere.

41
Q

Describe the effect of greenhouse gases on temperature.

A

The amount of solar energy reaching the earth’s surface varies at different locations, which influences temperature.

The angle of the sun’s rays makes solar insolation intense at the equator, but dispersed over the poles. How light or dark an area is on the earth’s surface determines the albedo, snow reflects and dark forests absorbs.

Heat is redistributed around the world by wind, ocean currents and pressure differences

42
Q

Describe the effect of greenhouse gases on precipitation

A

The heating of the earth’s atmosphere and surface controls the temperature, pressure, movement and moisture content of the air.
Where solar insolation is most intense, over the equator, precipitation is more intense due to the rising, cooling and condensing of cool air

43
Q

Explain and list the role of photosynthesis in regulating the composition of the atmosphere

A

Phytoplankton in the ocean sequester co2 through photosynthesis, the biological carbon pump

Terrestrial photosynthesis enables plants to sequester, the released back into the atmosphere through respiration and decomposition.

Tropical rainforests and coral reefs sequester large amounts of carbon

44
Q

What is the importance of carbon for soil (4)

A

Supports micro-organisms that maintain the nutrient cycle
Breakdown organic matter
Provide pore spaces for infiltration and storage of water
Enhance plant growth

45
Q

What are the characteristics of healthy soil (6)

A
Dark , crumbly and porous
Contain many organisms 
Provide air, water and nutrients for micro-organisms 
Contains and sequesters carbon
Enable infiltration and percolation
Retains moisture