2.1.6: The global carbon cycle Flashcards

1
Q

Stores

A

The amount of carbon held in the global system eg: the atmosphere, oceans and biosphere

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2
Q

Flows

A

Are movements or transfers of carbon between stores eg: volcanic activity adds 0.1 gigatonnes of carbon to the atmosphere annually

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3
Q

Inputs

A

Flows into stores

eg: CO2 added to the atmosphere by human activities

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4
Q

Outputs

A

Flows leaving stores

eg: dissolved carbon carried from the land in solution by rivers

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5
Q

1 gigatonne

A

1 billion tonnes

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6
Q

GtC

A

1 gigatonne of carbon dioxide

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7
Q

Carbon sequestration

A

Capture and storage of CO2

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8
Q

Processes between the land and atmosphere
(fast carbon cycle)
4

A

photosynthesis
respiration
decomposition
fossil fuel combustion

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9
Q

Carbon pathway from land to ocean
slow carbon cycle
process overview

A
Rainwater containing weak carbonic acid
reacts with limestone rock to produce
soluble calcium bicarbonate - moves thru water cycle
marine organisms use ^ to create shells
shells deposited as carbon-rich sediment
lithified
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10
Q

Lithification

A

Process by which sediment is slowly turned into rock

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11
Q

Weathering

A

In situ breakdown of rocks at or near the Earth’s surface by physical, chemical and biological processes.

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12
Q

Difference between weathering and erosion?

A

Weathering happens where the material is and erosion is the removal of the material

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13
Q

Carbonation

A

Rainwater combines with dissolved CO2 to forms weak carbonic acid and reacts with minerals in the rock form soluble bicarbonates.

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14
Q

Carbonation

type of weathering

A

chemical weathering

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15
Q

Chemical weathering transfers …. from rocks to the atmosphere and oceans every year

A

0.3 billion tonnes of carbon

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16
Q

Examples of limestone landscapes in the UK

2

A

Limestone cliffs at Llandudno

Exposed rocks at Malham, Yorkshire

17
Q

Example of chalk landscapes in the UK

A

England’s South Downs

18
Q

Methods by which oceans take up CO2

2

A

biological pump and physical pump

19
Q

Physical pump

A

CO2 dissolved in oceans can be transferred to the deep oceans in areas where cold, dense surface water sink.
Process of downwelling

20
Q

Downwelling

A

Carries carbon molecules to great depths where they remain for centuries

21
Q

What determines ocean acidity

A

CO2 diffusion

22
Q

Biological pump

A

Organisms such as phyloplankton absorb CO2 via photosynthesis and then are consumed by other organisms in the marine food web.