Flux table carbon cycle Flashcards

1
Q

What is the process of diffusion?

A

Carbon dioxide diffuses from the atmosphere to water into plants

Carbon dioxide also diffuses from the atmosphere to the ocean.

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2
Q

What are the oceans 2 carbon cycle ‘pump’ mechanisms referred to as?

A

Physical pump and Biological pump

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3
Q

Describe the physical pump

A
  • CO2 from atmosphere to ocean by diffusion
  • Carbon dioxide dissolved in the surface of the ocean can be transferred to the deep ocean in areas where cold dense surface waters sink.
  • This ‘downwelling’ carries carbon molecules to great depths where they may remain for centuries.
  • When cold water returns to the surface and warms up again it loses carbon dioxide to the atmosphere.
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4
Q

Describe the biological pump

A
  • These move carbon dioxide from the ocean surface to marine plants called phytoplankton through photosynthesis
  • This effectively converts carbon dioxide into food for zooplantic (microscopic animals) and their predators.
  • Most of the carbon dioxide taken up by phytoplankton is recycled near the surface. About 30% sinks into deeper waters before being converted back into carbon dioxide by marine bacteria.
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5
Q

How long does diffusion take?

A

Seconds

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6
Q

What is photosynthesis

A

Plants use energy from sunlight to combine CO2 from the atmosphere with water from the soil to create carbohydrates.
In this way CO2 is removed from the atmosphere and stored in the structure of plants.

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7
Q

Photosynthesis equation

A

Carbon Dioxide + Water → Light Energy → Oxygen + Glucose

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8
Q

Explain photosynthesis in marine plants

A

Higher amounts of carbon dioxide are removed from the atmosphere into the oceanic biological pump.
Removing greenhouse gas molecules from the atmosphere mitigates the warming effect of CO2 fossil fuel emissions

Higher amounts of carbon drawn into the biological pump eventually move down into deep ocean currents and sediments.
Carbon stored in deep ocean currents is there for time scales of hundreds to thousands of years.

The carbon that makes its way to sea floor sediments is stored for time scales of millions to billions of years.

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9
Q

How much of atmospheric carbon dioxide do global forest cycles make up for?

A

Photosynthesis in global forest cycles account for approximately one-twelfth of atmospheric carbon dioxide every year, accounting for about 50% of terrestrial (land based) photosynthesis.

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10
Q

How long does photosynthesis take?

A

Seconds

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11
Q

What is respiration?

A
  • happens in all cells - common in plants and animals
  • takes oxygen from the atmosphere and replaces it with carbon dioxide
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12
Q

How long does respiration take?

A

Seconds

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13
Q

Explain consumption in animals as a carbon flux

A

Animals feed on plants and other animals. Carbon is passed along the food chain.

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14
Q

Explain consumption in marine animals as a carbon flux

A

Phytoplankton in the ocean is consumed by other marine organisms and carbon is passed long the food chain by fish and larger sea animals as they consume one another.

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15
Q

How long does consumption take

A

Minutes hours

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16
Q

Decomposition as a carbon flux

A

When organisms die they are consumed by decomposers such as bacteria, fungi and earthworms. This process of decomposition results in carbon from their bodies being returned to the atmosphere as carbon dioxide. Some carbon is also returned to the soil.

17
Q

Decomposition as a carbon flux - water

A

In oceans when organisms die, their dead cells and shells sink into deep water. Decay releases carbon dioxide into this deep water.

18
Q

How long does decomposition take?

A

Hours/days

19
Q

Shell and coral formation as a carbon flux

A

In oceans some carbon gets incorporated into marine organisms as structural calcium carbonate shells and coral skeletons.
When oceanic organism die shells and sinks to the bottom, where it forms a layer of carbon rich sediment. They are eventually lithified (turned into rock). This can lock up carbon for millions of years.

20
Q

How long does shell and coral formation last?

A

Millennia

21
Q

Fossilisation as a carbon flux - ocean

A

Over millions of years chemical and physical processes may turn the carbon rich sediment at the bottom of the ocean into sedimentary rocks (chalk and limestone) This is known as lithification. This can lock up carbon for millions of years.

22
Q

Fossilisation as a carbon flux - land

A

Partial decomposed organic matter from past geological eras converted into coal, oil and gas

23
Q

How long does fossilisation take?

A

Millennia

24
Q

Explain combustion

A

When organic material is burned in the presence of oxygen it gives off carbon dioxide, energy and water. The carbon dioxide is released into the atmosphere, returning carbon that might have been stored in rocks for millions of years.

25
Q

Industrial revolution affect on carbon emissions

A

Since the start of the industrial revolution carbon dioxide has been released at an increasing rate by the burning of fossil fuels and biomass (naturally occurring wildfires as well as human induced burning). These fossil fuels contain carbon that was captured by living organisms over periods of millions of years and have been stored within the Earth‘s crust.

26
Q

How much carbon do fires release per year?

A

Every year fires release more than a billion tonnes of carbon into the atmosphere as carbon dioxide.

27
Q

How long does combustion take?

A

Seconds

28
Q

Explain volcanic activity as a carbon flux

A

Huge volumes of stored carbon in sedimentary rocks are on the move constantly (albeit at extremely slow rates) through the geological process of tectonic plate movement.
Some carbon is eventually released into the atmosphere by volcanic eruptions, as CO2 is released form melted rocks when subduction occurs at plate boundaries.

29
Q

How long does volcanic activity take?

A

Hours / days

30
Q

Explain methane formation as a carbon flux

A

Organic matter held under water is metabolised by methane producing bacteria
Methane accumulates in the ground in porous rocks or underwater, but may diffuse into the atmosphere
In air and light methane is oxidised to CO2 and water.

31
Q

How long does methane formation take?

A

Minutes

32
Q

Explain how weathering is a carbon flux

A

Weathering involves the breakdown of rocks in situ (their original place). Water is the key medium for chemical weathering. When carbon dioxide is absorbed by rainwater it forms a mild carbonic acid. This reacts with calcium carbonate in chalk and limestone, forming calcium bicarbonate which is soluble and removed by percolating water.

33
Q

How much carbon is transferred to the atmosphere by weathering per year?

A

Globally, some 0.3 billion tonnes of carbon are transferred from rocks to the atmosphere and oceans each year by chemical weathering.

34
Q

Weathering - water - carbon flux explanation

A

Calcium bicarbonate can be transferred by overland flow, throughflow or groundwater flow into river where it becomes part of the solute load

35
Q

How long does chemical weathering take?

A

Years

36
Q

Carbon sequestration explanation

A

This is an umbrella term used to describe the transfer of carbon from the atmosphere to other stores for long term storage. Sequestration is both a natural process and a human process;

37
Q

Natural carbon sequestration explained

A

The natural capture and storage of carbon dioxide from the atmosphere by physical or biological processes such as photosynthesis (see diagram below). This occurs naturally but can be enhanced through land management practices that maximise the amount of carbon that remains stored in soil and in plants for the long term.

38
Q

Human carbon sequestration explained

A

CO2 captured at source e.g. power plants and then injected in liquid form into underground stores such as coal beds or depleted gas and oil reserves. This is experimental at the moment.

39
Q

How long does natural carbon sequestration take?

A

Seconds