Carbon cycle Flashcards

(16 cards)

1
Q

Where is carbon found:

A
  • All organic molecules
  • Fats, carbohydrates and proteins
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2
Q

Carbon cycle definition:

A

Demonstrates the continuous movement of carbon between biotic (living) and abiotic (non-living) components of the environment

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3
Q

Carbon sink:

A
  • Absorb more CO2 than the emit
    Ocean + peat bogs
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4
Q

Photosynthesis:

A
  • Producers, like plants, absorb CO2 from the atmosphere and convert it into organic molecules
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5
Q

What does the carbon cycle demonstrate?

A
  • Continuous movement of carbon between the biotic (living) and abiotic (non-living) components of the environment.
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6
Q

Consumption:

A

Carbon is passed through food chains as organisms consume other organisms

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7
Q

Respiration:

A

Organisms use oxygen and carbohydrates to release energy, releasing CO2 back into the atmosphere

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8
Q

Decomposition:

A

Dead organic matter is broken down by microorganisms, which releases CO2 into the environment

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9
Q

Formation of fossil fuels:

A

Carbon, stored in dead organic matter that does not decompose due to high temperature and pressure, is transformed over millions of years into fossil fuels, including coal and oil.

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10
Q

Combusion:

A

The burning of fossil fuels reacts stored carbon with oxygen, releasing CO2 into the atmosphere

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11
Q

Weathering:

A

Carbon stored in sedimentary rocks is released back into the environment through weathering processes

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12
Q

Volcanic activity:

A

Tectonic plate movements can lead to the release of CO2 from volcanic eruptions

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13
Q

Fluctuations in atmospheric CO2

A

Fluctuate daily, seasonal, annual basis mainly due to variations in photosynthesis and respiration rates

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14
Q

Daily fluctuations in atmospheric CO2:

A
  • Respiration occurs continuously throughout the day and night, releasing CO2 into the atmosphere
  • Photosynthesis only occurs during daylight, removing CO2 from the atmosphere and reducing local atmospheric CO2 levels during the daylight hours
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15
Q

Seasonal fluctuations in atmospheric CO2:

A
  • During the summer, long daylight hours and warm temperatures increase photosynthesis rates, absorbing more CO2 and reducing local atmospheric CO2 levels
  • During winter, reduced daylight hours and colder temperatures decrease photosynthesis rates and resulting higher local atmospheric CO2 levels
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16
Q

Annual fluctuations in atmospheric CO2:

A
  • Annually, greenhouse gas emissions, including those of CO2, have been increasing
  • Increased deforestation removes photosynthesising biomass, lowering the capacity to remove CO2 from the atmosphere
  • The rising concentration of CO2 in the atmosphere accelerates global warming
  • Global warming decreases the solubility of CO2 in oceans as less gas can dissolve in warmer water, leading to more CO2 being released into atmosphere