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Earth’s Life Support Systems

Fossil fuel combustion, carbon sequestration and feedback loops

  • 2 things to know
  • Component 01

Overview

Recall questions on the rise in atmospheric carbon dioxide since the industrial era, how much human carbon stays airborne, carbon capture and storage at Sleipner and its limits, the permafrost carbon, ice-albedo and water vapour feedbacks, negative feedbacks, and why methane matters.

What you need to know

Answer each one before you reveal it.

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Key term

What fraction of the carbon released by human activity stays in the atmosphere?

Key term

What is carbon capture and storage?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    By how much has atmospheric carbon dioxide risen since the start of the industrial era?

    Model answer

    It has risen from about 280 ppm before 1800 to over 420 ppm today, an increase of roughly 50%.

  2. 2

    How does fossil fuel combustion break the natural carbon balance?

    Model answer

    It transfers carbon from the slow geological store into the atmosphere far faster than weathering and sequestration can remove it, so the atmospheric store grows year on year.

  3. 3

    What fraction of the carbon released by human activity stays in the atmosphere?

    Model answer

    Roughly half of it remains airborne, while the oceans take up about a quarter and the land biosphere about a quarter.

  4. 4

    What is carbon capture and storage?

    Model answer

    Carbon capture and storage is the capture of carbon dioxide from a power station or industrial plant before it is emitted, followed by its transport and injection into deep geological formations for permanent storage.

  5. 5

    Name the kinds of geological formation used to store captured carbon dioxide.

    Model answer

    Depleted oil and gas reservoirs and deep saline aquifers, each sealed beneath an impermeable cap rock.

  6. 6

    Give an operating example of offshore carbon storage.

    Model answer

    The Sleipner field in the Norwegian North Sea, where around a million tonnes of carbon dioxide a year has been injected into a deep saline sandstone since 1996.

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Earth’s Life Support Systems

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Hotter magma is .
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AThe lower quartile is the 2nd value, 11 cm.
BThe upper quartile is the 6th value, 16 cm.
CThe interquartile range is 16 − 11 = 5 cm.

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The sunspot cycle lasts about 11 years.
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